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Sinosphere Blog: Wealthy Chinese Travelers Lining Up to Blast Off

Written By Unknown on Rabu, 10 September 2014 | 15.49

Photo Sheng Tianxing, a tea trader, bought a $100,000 ticket for a trip on a commercially operated flight to go 64 miles above Earth.Credit Qilai Shen for The New York Times

One night in June, Sheng Tianxing made good on his name, which translated literally means "sky travel." With a single click online, he paid $100,000, about a third of his annual income, for a seat on a rocket that will carry him into space.

Come 2016, if all goes as planned, Mr. Sheng, 41, a tea trader from the southeastern Chinese province of Zhejiang, will spend up to six minutes floating 64 miles above the Earth as one of the first civilians aboard a commercially operated flight beyond the planet's atmosphere.

"I've always wanted to go into space," he said recently, recalling that he got hooked on space films and science fiction as a boy growing up in a mountain village. "I've always wondered if Armstrong did actually walk on the moon. I'd like to have a look myself."

A half-century ago, bemoaning his nation's backwardness, Mao Zedong said that China could not launch a potato into space. Now, well-to-do Chinese business people are lining up for one-hour voyages to the cosmos, and tour operators say China is set to become the world's largest market for the incipient space tourism industry.

Already, more than 30 mainland Chinese have purchased or made down payments of 50 percent on tickets for journeys offered by XCOR Aerospace, a company based in Mojave, Calif., that plans to begin operating suborbital flights late next year. The tours went on sale in China in December, two years after the company began selling them elsewhere, and one in 10 of all bookings have been by Chinese citizens, according to Dexo Travel, the Beijing-based sales agent in China for the trips.

The sales reflect late-blooming interest in space travel in China, which celebrated the successful landing of a lunar rover in December, four decades after the United States accomplished the same feat. The notion of traveling amid the stars has captivated a segment of the Chinese public just as it once fascinated Americans who were riveted by Neil Armstrong's first steps on the moon. But unlike that earlier generation, the Chinese have the option of booking a trip themselves — and many have the money to pay for it.

"There are wealthy people everywhere in the world, but there are not so many wealthy people who also dream of going into space," said Alex Tang, chief executive of XCOR Aerospace's Asia operation. China, he said, had both. In a survey this year of more than 200 Chinese luxury travelers by the Shanghai-based research firm Hurun, about 7 percent said they hoped to visit space within the next three years.

Mr. Tang attributed the Chinese passion for space travel to the recent successes of the nation's space program. "Many want to go to space like Yang Liwei," he said, referring to the astronaut who circled the Earth in 2003 and came home a national hero for bringing China into the ranks of space-faring nations.

Zhang Yong, chief executive of Dexo Travel, described the people booking seats as business executives and entrepreneurs who already have luxury homes and cars and are turning their sights beyond earthly objects. Two-thirds are male, he said. Influenced by books and films like "Gravity," a hit in China, they long for the transcendent experience of gazing upon Earth from space, Mr. Zhang said.

Interest in the spaceflights is high even among those without the means to go. Some would-be space tourists have become minor celebrities long before the first liftoff.

After Tong Jingling, a 40-year-old banker, booked a ticket in April, she started getting invitations from businesses to be their spokeswoman, she said. One company asked her to conduct medical experiments while in space.

Ms. Tong, a graduate of Beihang University, formerly known as the Beijing Institute of Aeronautics, has capitalized on the attention by trying to launch several crowd-funded ventures. One would arrange weddings in space. Another would produce a reality television show in which contestants compete for a ticket for space travel. An investment of 100 renminbi, or $16, gets you a T-shirt that says, wo yao shang taikong (我要上太空), or "I want to go up into space."

The Chinese are coming a bit late to space tourism. The first civilian space tour was in 2001, when the American billionaire Dennis Tito joined a Russian space mission and flew to the International Space Station. He spent $20 million and underwent months of training. Since then, six other civilians have made the same trip.

But companies are now selling suborbital trips to altitudes just beyond the Earth's atmosphere, at prices that put the dream of space travel within the reach of wealthy Chinese. After long delays caused by technical and safety issues, XCOR Aerospace and Virgin Galactic, founded by the British entrepreneur Richard Branson, say they are planning flights next year.

Because Virgin Galactic spacecraft are powered by rocket engines manufactured in the United States that use technology considered to have potential military applications, citizens from 22 countries, including China, are barred from traveling on them, the company has said. Virgin Galactic said it hoped that future United States government rulings would enable it to offer spaceflights to an expanded roster of nations.

XCOR Aerospace's Lynx shuttle uses different engines that do not appear to raise the same concerns. A $95,000 ticket with XCOR buys a flight late next year to an altitude of about 38 miles — what the company calls "the edge of space" — while a $100,000 ticket will take a passenger beyond the atmosphere in 2016. Each flight carries one passenger, who must undergo medical screening and training.

Mr. Zhang said he expects Chinese interest in space tourism to increase further once the first civilian flights are underway. "Many from business circles and celebrities have told me that they'll buy tickets once the test flights succeed or the first tourists return safely," he said.

Several Chinese who have booked seats said they had confidence in the safety of the shuttle technology, though some had not told their families of their plans.

Zhang Xiaoyu, 29, an entrepreneur in Beijing, said he told his parents only that he planned to fly at a "relatively high altitude." He did not tell them how much the ticket cost, either. But Mr. Zhang said traveling to space meant more to him than putting a down payment on an apartment or buying a car in the congested Chinese capital.

"You will be able to look back at the planet where you were born and experience complete solitude," he said. "You wouldn't be able to experience this anywhere else."


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Well: The Problem With Reclining Airplane Seat Design

Written By Unknown on Selasa, 09 September 2014 | 15.49

The Well Column

Tara Parker-Pope on living well.

To recline or not to recline? That is the question now being hotly debated among air travelers after three flights were forced to land after passengers on board began fighting about reclining seats.

But are passengers really the problem? The real issue may be that most airline seats are not designed to fully accommodate the human body in its various shapes and sizes.

"We are fighting each other, but the seats are not designed right," said Kathleen M. Robinette, professor and head of the department of design, housing and merchandising at Oklahoma State University. "The seats don't fit us."

Dr. Robinette would know. She is the lead author of a landmark anthropometric survey conducted by the Air Force with a consortium of 35 organizations and published in 2002. It is widely used by seat makers and other designers.

The survey, called the Civilian American and European Surface Anthropometry Resource project, measured the bodies of 4,431 people in North America, the Netherlands and Italy. The survey collected a voluminous amount of data about its subjects, ranging from height and weight to shoe and bra size. Dr. Robinette and her colleagues made 3D scans of their subjects, allowing for detailed measurements in sitting and standing positions.

For seat designers, the most relevant data came from measurements of people sitting, which included distances from the buttock to the knee, the breadth of the hips and the height of the knees.

The data gave an accurate view of the variations in the human form, Dr. Robinette said, but the measurements have not been used correctly.

Seat designers often make the assumption that nearly everyone will be accommodated if they design a seat for a man in the 95th percentile of measurements, meaning that they are larger than all but 5 percent of other men — and, theoretically, all women. But even in that group, there are big differences.

Take the buttock-to-knee measurement of the largest men in the study: In the North American group, the average measurement was 26.5 inches, but the Dutch men were larger, measuring 27.6 inches. Factor in the fact that nobody on an airplane sits upright with the knees bent at a 90 degree angle, plus variations in calf length and thigh length.

The result is that the measurements don't really account for different body shapes and variations in the way people sit.In addition, choosing the 95th percentile of men as a cutoff means at least 5 percent, as many as 1 in 20 men, on the plane will be using seats that are too small for them. "That's about 10 people on every plane who are dis-accommodated, as well as all the people sitting next to them," Dr. Robinette said.

A big flaw in seat design, however, is that men in the 95th percentile are not necessarily larger than women, particularly in the parts of the body that are resting on the seat.

In terms of hip width, women are bigger than men. In the study, North American women in the 95th percentile had hip breadth measurements of 19.72 inches, compared to 17.15 inches for North American men.

According to SeatGuru.com, which collects data on seat sizes from dozens of airlines, the typical economy class airline seat ranges from 17 to 18 inches across. This means that seats will be snug on many bodies; for about 1 in 4 women, the seat will be too small at the hips, causing them to spill over into the adjacent seat.

Further, the widest part of the body is actually the shoulders, which is why so many of us end up knocking elbows and shoulders with the passengers next to us, or leaning into the window or aisle to avoid pressing against our seat neighbor.

The issue goes beyond passenger comfort. Dr. Robinette notes that travelers who are squeezed together and touching continually are more likely to spread cold viruses or other illnesses to a fellow passenger. People who are confined to tight seats and who can't move comfortably are at risk for painful "hot spots" — precursors to the bed sores that occur in nursing home patients who aren't moved frequently.

Of greater concern is the risk of blood clots, including a potentially deadly condition called deep vein thrombosis.

"When sitting in a way so you can't move, you start to get spots that are compression spots after maybe a half-hour or so," Dr. Robinette said. "Pain and discomfort is your body telling you something is wrong, and on an airplane there is a risk of blood clots. It's a serious problem that we are all discounting."

When it comes to reclining a seat, the most important measure of comfort is seat pitch, which is the distance from any point on one seat to the exact same point on the seat in front or behind it.

According to SeatGuru, seat pitch is a good approximation of how much seat and leg room a passenger can expect. The measurement on short-haul flights averages about 31 inches on most flights, ranging from a tight 28 inches on some airlines to a roomy 38 to 39 inches on a few.

"Seat pitch is what most fliers are concerned about," said Jami Counter, senior director of SeatGuru and TripAdvisor. "When you are talking about 31 inches as the standard, that's pretty tight; 28 inches is incredibly tight. Airlines are feeling really crowded and really cramped."

Officials at Recaro Aircraft Seating, a German seat manufacturer, said that seat design had to take into account safety requirements, weight, passenger comfort and airplane space needs, and have enough flexibility that seats can be used in various aircraft layouts.

Recaro has introduced a new seat with a slimmer back rest, giving the passenger behind the seat more space for knees and shins. The designers also moved the seat pocket above the tray table to allow for more knee room.

Recaro has received orders for more than 200,000 of the seats since introducing the model in late 2010.

"Of course, it is possible to install seats in an aircraft at a more comfortable distance from each other, so that everybody has sufficient knee and leg space," Rene Dankwerth, the vice president of research and development at Recaro, said in a written response. "However, the ticket price would definitely rise."

At 6 feet 6 inches, Chicago economics professor Devin Pope knows the risk of sitting behind someone who chooses to recline the seat. Dr. Pope likened it to a classic economics experiment called the Dictator game, in which a person is given $10 and allowed to keep it all, or share it with another person. Surprisingly, the dictator often chooses to share the money.

"It suggests that people really do care about other people sometimes," said Dr. Pope, associate professor of behavioral science at the University of Chicago's Booth School of Business. "I think it suggests why a lot of people don't lean the seat back."

 

A version of this article appears in print on 09/09/2014, on page D1 of the NewYork edition with the headline: Taking a Position on Plane Comfort.


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Sinosphere Blog: Wealthy Chinese Travelers Lining Up to Blast Off

Written By Unknown on Senin, 08 September 2014 | 15.49

Photo Sheng Tianxing, a tea trader, bought a $100,000 ticket for a trip on a commercially operated flight to go 64 miles above Earth.Credit Qilai Shen for The New York Times

One night in June, Sheng Tianxing made good on his name, which translated literally means "sky travel." With a single click online, he paid $100,000, about a third of his annual income, for a seat on a rocket that will carry him into space.

Come 2016, if all goes as planned, Mr. Sheng, 41, a tea trader from the southeastern Chinese province of Zhejiang, will spend up to six minutes floating 64 miles above the Earth as one of the first civilians aboard a commercially operated flight beyond the planet's atmosphere.

"I've always wanted to go into space," he said recently, recalling that he got hooked on space films and science fiction as a boy growing up in a mountain village. "I've always wondered if Armstrong did actually walk on the moon. I'd like to have a look myself."

A half-century ago, bemoaning his nation's backwardness, Mao Zedong said that China could not launch a potato into space. Now, well-to-do Chinese business people are lining up for one-hour voyages to the cosmos, and tour operators say China is set to become the world's largest market for the incipient space tourism industry.

Already, more than 30 mainland Chinese have purchased or made down payments of 50 percent on tickets for journeys offered by XCOR Aerospace, a company based in Mojave, Calif., that plans to begin operating suborbital flights late next year. The tours went on sale in China in December, two years after the company began selling them elsewhere, and one in 10 of all bookings have been by Chinese citizens, according to Dexo Travel, the Beijing-based sales agent in China for the trips.

The sales reflect late-blooming interest in space travel in China, which celebrated the successful landing of a lunar rover in December, four decades after the United States accomplished the same feat. The notion of traveling amid the stars has captivated a segment of the Chinese public just as it once fascinated Americans who were riveted by Neil Armstrong's first steps on the moon. But unlike that earlier generation, the Chinese have the option of booking a trip themselves — and many have the money to pay for it.

"There are wealthy people everywhere in the world, but there are not so many wealthy people who also dream of going into space," said Alex Tang, chief executive of XCOR Aerospace's Asia operation. China, he said, had both. In a survey this year of more than 200 Chinese luxury travelers by the Shanghai-based research firm Hurun, about 7 percent said they hoped to visit space within the next three years.

Mr. Tang attributed the Chinese passion for space travel to the recent successes of the nation's space program. "Many want to go to space like Yang Liwei," he said, referring to the astronaut who circled the Earth in 2003 and came home a national hero for bringing China into the ranks of space-faring nations.

Zhang Yong, chief executive of Dexo Travel, described the people booking seats as business executives and entrepreneurs who already have luxury homes and cars and are turning their sights beyond earthly objects. Two-thirds are male, he said. Influenced by books and films like "Gravity," a hit in China, they long for the transcendent experience of gazing upon Earth from space, Mr. Zhang said.

Interest in the spaceflights is high even among those without the means to go. Some would-be space tourists have become minor celebrities long before the first liftoff.

After Tong Jingling, a 40-year-old banker, booked a ticket in April, she started getting invitations from businesses to be their spokeswoman, she said. One company asked her to conduct medical experiments while in space.

Ms. Tong, a graduate of Beihang University, formerly known as the Beijing Institute of Aeronautics, has capitalized on the attention by trying to launch several crowd-funded ventures. One would arrange weddings in space. Another would produce a reality television show in which contestants compete for a ticket for space travel. An investment of 100 renminbi, or $16, gets you a T-shirt that says, wo yao shang taikong (我要上太空), or "I want to go up into space."

The Chinese are coming a bit late to space tourism. The first civilian space tour was in 2001, when the American billionaire Dennis Tito joined a Russian space mission and flew to the International Space Station. He spent $20 million and underwent months of training. Since then, six other civilians have made the same trip.

But companies are now selling suborbital trips to altitudes just beyond the Earth's atmosphere, at prices that put the dream of space travel within the reach of wealthy Chinese. After long delays caused by technical and safety issues, XCOR Aerospace and Virgin Galactic, founded by the British entrepreneur Richard Branson, say they are planning flights next year.

Because Virgin Galactic spacecraft are powered by rocket engines manufactured in the United States that use technology considered to have potential military applications, citizens from 22 countries, including China, are barred from traveling on them, the company has said. Virgin Galactic said it hoped that future United States government rulings would enable it to offer spaceflights to an expanded roster of nations.

XCOR Aerospace's Lynx shuttle uses different engines that do not appear to raise the same concerns. A $95,000 ticket with XCOR buys a flight late next year to an altitude of about 38 miles — what the company calls "the edge of space" — while a $100,000 ticket will take a passenger beyond the atmosphere in 2016. Each flight carries one passenger, who must undergo medical screening and training.

Mr. Zhang said he expects Chinese interest in space tourism to increase further once the first civilian flights are underway. "Many from business circles and celebrities have told me that they'll buy tickets once the test flights succeed or the first tourists return safely," he said.

Several Chinese who have booked seats said they had confidence in the safety of the shuttle technology, though some had not told their families of their plans.

Zhang Xiaoyu, 29, an entrepreneur in Beijing, said he told his parents only that he planned to fly at a "relatively high altitude." He did not tell them how much the ticket cost, either. But Mr. Zhang said traveling to space meant more to him than putting a down payment on an apartment or buying a car in the congested Chinese capital.

"You will be able to look back at the planet where you were born and experience complete solitude," he said. "You wouldn't be able to experience this anywhere else."


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Sinosphere Blog: Wealthy Chinese Travelers Lining Up to Blast Off

Written By Unknown on Minggu, 07 September 2014 | 15.49

Photo Sheng Tianxing, a tea trader, bought a $100,000 ticket for a trip on a commercially operated flight to go 64 miles above Earth.Credit Qilai Shen for The New York Times

BEIJING — One night in June, Sheng Tianxing made good on his name, which translated literally means "sky travel." With a single click online, he paid $100,000, about a third of his annual income, for a seat on a rocket that will carry him into space.

Come 2016, if all goes as planned, Mr. Sheng, 41, a tea trader from the southeastern Chinese province of Zhejiang, will spend up to six minutes floating 64 miles above the Earth as one of the first civilians aboard a commercially operated flight beyond the planet's atmosphere.

"I've always wanted to go into space," he said recently, recalling that he got hooked on space films and science fiction as a boy growing up in a mountain village. "I've always wondered if Armstrong did actually walk on the moon. I'd like to have a look myself."

A half-century ago, bemoaning his nation's backwardness, Mao Zedong said that China could not launch a potato into space. Now, well-to-do Chinese business people are lining up for one-hour voyages to the cosmos, and tour operators say China is set to become the world's largest market for the incipient space tourism industry.

Already, more than 30 mainland Chinese have purchased or made down payments of 50 percent on tickets for journeys offered by XCOR Aerospace, a company based in Mojave, Calif., that plans to begin operating suborbital flights late next year. The tours went on sale in China in December, two years after the company began selling them elsewhere, and one in 10 of all bookings have been by Chinese citizens, according to Dexo Travel, the Beijing-based sales agent in China for the trips.

The sales reflect late-blooming interest in space travel in China, which celebrated the successful landing of a lunar rover in December, four decades after the United States accomplished the same feat. The notion of traveling amid the stars has captivated a segment of the Chinese public just as it once fascinated Americans who were riveted by Neil Armstrong's first steps on the moon. But unlike that earlier generation, the Chinese have the option of booking a trip themselves — and many have the money to pay for it.

"There are wealthy people everywhere in the world, but there are not so many wealthy people who also dream of going into space," said Alex Tang, chief executive of XCOR Aerospace's Asia operation. China, he said, had both. In a survey this year of more than 200 Chinese luxury travelers by the Shanghai-based research firm Hurun, about 7 percent said they hoped to visit space within the next three years.

Mr. Tang attributed the Chinese passion for space travel to the recent successes of the nation's space program. "Many want to go to space like Yang Liwei," he said, referring to the astronaut who circled the Earth in 2003 and came home a national hero for bringing China into the ranks of space-faring nations.

Zhang Yong, chief executive of Dexo Travel, described the people booking seats as business executives and entrepreneurs who already have luxury homes and cars and are turning their sights beyond earthly objects. Two-thirds are male, he said. Influenced by books and films like "Gravity," a hit in China, they long for the transcendent experience of gazing upon Earth from space, Mr. Zhang said.

Interest in the spaceflights is high even among those without the means to go. Some would-be space tourists have become minor celebrities long before the first liftoff.

After Tong Jingling, a 40-year-old banker, booked a ticket in April, she started getting invitations from businesses to be their spokeswoman, she said. One company asked her to conduct medical experiments while in space.

Ms. Tong, a graduate of Beihang University, formerly known as the Beijing Institute of Aeronautics, has capitalized on the attention by trying to launch several crowd-funded ventures. One would arrange weddings in space. Another would produce a reality television show in which contestants compete for a ticket for space travel. An investment of 100 renminbi, or $16, gets you a T-shirt that says, "I want to go up into space" in Chinese.

The Chinese are coming a bit late to space tourism. The first civilian space tour was in 2001, when the American billionaire Dennis Tito joined a Russian space mission and flew to the International Space Station. He spent $20 million and underwent months of training. Since then, six other civilians have made the same trip.

But companies are now selling suborbital trips to altitudes just beyond the Earth's atmosphere, at prices that put the dream of space travel within the reach of wealthy Chinese. After long delays caused by technical and safety issues, XCOR Aerospace and Virgin Galactic, founded by the British entrepreneur Richard Branson, say they are planning flights next year.

Because Virgin Galactic spacecraft are powered by rocket engines manufactured in the United States that use technology considered to have potential military applications, citizens from 22 countries, including China, are barred from traveling on them, the company has said. Virgin Galactic said it hoped that future United States government rulings would enable it to offer spaceflights to an expanded roster of nations.

XCOR Aerospace's Lynx shuttle uses different engines that do not appear to raise the same concerns. A $95,000 ticket with XCOR buys a flight late next year to an altitude of about 38 miles — what the company calls "the edge of space" — while a $100,000 ticket will take a passenger beyond the atmosphere in 2016. Each flight carries one passenger, who must undergo medical screening and training.

Mr. Zhang said he expects Chinese interest in space tourism to increase further once the first civilian flights are underway. "Many from business circles and celebrities have told me that they'll buy tickets once the test flights succeed or the first tourists return safely," he said.

Several Chinese who have booked seats said they had confidence in the safety of the shuttle technology, though some had not told their families of their plans.

Zhang Xiaoyu, 29, an entrepreneur in Beijing, said he told his parents only that he planned to fly at a "relatively high altitude." He did not tell them how much the ticket cost, either. But Mr. Zhang said traveling to space meant more to him than putting a down payment on an apartment or buying a car in the congested Chinese capital.

"You will be able to look back at the planet where you were born and experience complete solitude," he said. "You wouldn't be able to experience this anywhere else."


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Dot Earth Blog: Dynamic Planet: Under the Volcano in Papua New Guinea

Written By Unknown on Jumat, 05 September 2014 | 15.49

Photo A family in Rabaul, Papua New Guinea, copes with the ash falling from the nearby volcano. This is one of many photographs taken in the threatened town by the French photographer Eric Lafforgue.Credit

A caldera is the cauldron-like depression formed when a volcanic eruption empties a shallow chamber of magma and the cone collapses. If the volcano is at sea level, the result, after the passage of time, can be a fine harbor.

A fine harbor, and fertile soil from all that ash, attracts people. At the east end of New Britain Island in Papua New Guinea, the result was the port and one-time district capital, Rabaul. The capital shifted after two of the three smaller cones around the caldera, Tavurvur and Vulcan, explosively erupted in 1994. But plenty of people still live in Rabaul, and they live in harm's way.

Amid the news about an eruption in Iceland last week, you may also have heard about the latest explosive eruption of Tavurvur. After seeing an extraordinary Facebook post of a photo of the eruption, shot from the sailing vessel Obelisk, I dug in a bit.

Photo Jesse Smith, the skipper of the circumnavigating sailboat Obelisk, made for safer waters on August 29 as the Tavurvur Volcano erupted near Rabaul, Papua New Guinea. Aboard was the underwater photographer Christopher Hamilton, who took this photograph.Credit Christopher Hamilton

One result, which you can read below, is a remarkable firsthand account from the underwater photographer Christopher Hamilton and his partner, Leah Sindel, who were aboard the boat when the harbor began rumbling. They were sailing in the region photographing World War II shipwrecks and a cave full of skulls. The boat's owner and skipper, pictured above in one of Hamilton's photos (and the Facebook shot), is Jesse Smith.

But first I want to draw your attention to two other views of Rabaul and the eruption.

First, another fine photographer, Eric Lafforgue, was on the ground in Rabaul after the eruption and captured some absolutely stunning pictures of daily life there, reflecting the realities facing millions of people in developing countries who live in places deeply vulnerable to geological hazards. At the top of this post is one of his images. There are many more here.

Second, there's the geological context. On The Conversation, a fast-expanding website in which scientists and scholars fill the gap left as conventional news operations shrink, there's a superb look at the Tavurvur eruption by Robin Wylie, a doctoral student in volcanology at University College London (@rwylie9 on Twitter). Here's just a snippet of his piece, but I encourage you to read the rest:

Don't be concerned if you don't know much about Rabaul. Until recently, not even volcanologists did. The eruptive history of Tavurvur and its volcanic entourage was largely a mystery until the 1970s, when an increase in seismicity beneath the region prompted the first extensive volcanological survey.

It revealed that, over the past 7,000 years, a number of huge, highly explosive eruptions had occurred. These cataclysms hollowed out Rabaul caldera. The largest of them occurred in the late 6th century, and is believed to have generated pyroclastic flows – that of hot gas, ash and rocks blown out of a volcano – reaching at least 50 kilometers from Rabaul. This massive eruption probably had a volcanic explosivity index of six, which is equivalent to that of the 1883 eruption of Krakatoa. And yet, while the former lives in infamy, relatively few people have even heard of Rabaul.

…While small eruptions are fairly common, experts also believe that a big one may be brewing. Devastating eruptions like the ones which carved out the caldera take place on average every few thousand years. And as the last one struck 1,400 years ago, the clock is well and truly ticking. The rebuilt Rabaul town now has only around 4,000 inhabitants, but tens of thousand more live within touching distance of a large blast. This far-flung island is worth watching.

I'll be helping run a blogging workshop for communicative scientists this fall at Stony Brook University and Wylie (and The Conversation) will be a prime example of what's possible.

Finally, please read Hamilton's note (written with Sindel's help) describing the scene on Aug. 29 when the bay started reverberating and ash and flaming boulders started falling (I inserted links to relevant photographs from their Flickr feed):

I have been on a sailing journey from New Zealand to Indonesia, passing through Vanuatu, the Solomon Islands, & Papua New Guinea. My time in these countries has been principally spent diving (mostly on wrecks from the second World War) and exploring.

We arrived in Rabaul on August 26th, and soon met local wreck hunting legend Rod Pearce, who was kind enough to show us around and take us to dive some of the most fascinating war wrecks in the harbor.

At 3.30 am on the morning of the 29th, we felt a light rain, and sleepily closed the hatches above our heads, but were faintly aware of an odd sound, somewhere in the background. Finally one of my sailing companions called out in a puzzled voice, "It's rainy but I am not getting wet." At this point we rose to investigate further, and were sharply jolted awake when we realized that it was ash and small pebbles of pumice raining down on us, not water.

We were at first bemused, thinking that the volcano not far from where we were anchored was sending out a small benign shower. The locals had told us that sometimes dust showers could occur. But soon the hatches above out heads become black with a thick layer of debris, and the volcanic rain seemed to be getting heavier. Shortly after this we were awakened by Rod Pearce, tied up to the dock next to us, who sharply informed us that everyone was getting out — now.

The crew sprang into action, and in two minutes we were making our way out of the harbor. By this point, sizable chunks of pumice and other debris were bombarding us as we coiled the lines and tried to find a path ahead of us.

I ducked down to the chart table to turn on our navigation software, and suddenly heard from above several great cries in unison. I came back up immediately and was greeted with one of the most extraordinary spectacles I have ever seen. The mountain — far from issuing a benign puff of ash — was spewing out a fountain of lava, flinging enormous molten rock fragments miles into the sky. The sound was deafening, and preceding every rumble, the shock waves that were sent out reverberated through your chest. At this point we were beside ourselves with elation, and fumbled through the drawers for a zip-lock bag containing the camera.

Photo The Tavurvur volcano near Rabaul, Papua New Guinea, erupted on Aug. 29.Credit Christopher Hamilton

Dawn soon came upon us, and the spectacle of the eruption was crowned by deep golden light rays filtering down what we could now clearly see to be a colossal pillar of smoke, ash and sulfur billowing above the bay.

As the light grew stronger we were also confronted with the heavy layer of ash and debris covering the sailboat, and the enormous task that lay ahead of us. Our departure date, it was obvious, had been pushed back awhile. We spent all of that day in a harbor along the other side of the bay (upwind of the volcano), scrubbing and hosing and prying and scraping the muddy, crunching mess from the decks and from every conceivable crevice on the boat. All the while we had a perfect view of the eruptions' death throes. Every so often a flash of light like a perfect sphere was perceptible for a split second above the caldera, and a shock wave would ripple up the cloud column.

Photo The photographer Christopher Hamilton captured this image from a sailboat as the Tavurvur Volcano near Rabaul, Papua New Guinea, eruped on Aug. 29.Credit Christopher Hamilton

Seconds later this would be accompanied by a stupendous crash. The lava was less abundant and certainly less visible now in daylight, but the mountain continued to throw out enormous chunks of debris, some of which were flung so far that they landed in the sea at the foot of the volcano with an explosive splash and a mist of steam.

By later afternoon the activity had significantly subsided, and we spent the evening with a cold beer in hand, peering out into the darkness of the bay to catch the final flickers of light above the peak.

There are more images on Flickr, as well as video shot by Hamilton.

Postscript | Capital Weather Gang has yet another vantage point on the eruption — before and after imagery from NASA showing the extent of the ash fall.


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Dot Earth Blog: Accounting for the Expanding Carbon Shadow from Coal-Burning Plants

Written By Unknown on Jumat, 29 Agustus 2014 | 15.50

Steven Davis of the University of California, Irvine, and Robert Socolow of Princeton (best known for his work dividing the climate challenge into carbon "wedges") have written "Commitment accounting of CO2 emissions," a valuable new paper in Environmental Research Letters showing the value of shifting from tracking annual emissions of carbon dioxide from power plants to weighing the full amount of carbon dioxide that such plants, burning coal or gas, could emit during their time in service.

This makes sense because of the long lifetime of these plants once built — typically 40 years or so — and the long lifetime of carbon dioxide once released. (I'd love to see some data visualization experiments on this idea from Adam Nieman, building on his work showing the volume of daily CO2 emissions from cities and the like.)

Here's Davis's "video abstract" (the transcript is appended at the end of this post, along with a rich discussion of the paper's findings and implications):

The opening section of the paper is remarkably clear and is worth posting here (minus footnotes and the like):

Each year, governments and firms estimate and report CO2 emissions from the burning of fossil fuels, and their efforts to slow climate change are measured against these annual emissions. Ultimately, though, the magnitude of warming we experience will not be determined by emissions in any one year, but by cumulative CO2 emissions. Thus, climate scientists and energy-economic modelers have developed hundreds of plausible scenarios of future emissions and used them to identify emissions pathways that might achieve climate policy goals. Such scenarios are powerful tools for connecting emissions and warming to trajectories of population growth, economic development, and energy use. However, these trajectories are constrained by tremendous socio-economic inertia (e.g., existing energy, transport and built infrastructures) that limits the rate at which CO2 emissions can be reduced and climate change avoided.

In 2010, Davis et al [background] quantified an important component of socio-economic inertia by estimating the future emissions expected from all existing fossil fuel-burning infrastructure worldwide, naming these 'committed' emissions. That paper provided a single data point (commitments as of 2009), but lacked the context perhaps most important to policymakers: how these committed emissions have changed over time. Here we provide that context. We show that, despite international efforts to reduce CO2 emissions, total remaining commitments in the global power sector have not declined in a single year since 1950 and are in fact growing rapidly (by an average of 4% per year 2000–2012).

The annual 'commitment accounting' that we demonstrate here offers policymakers an opportunity to evaluate historical trends and to quantify the long-term consequences of current actions in a new way.

Environmental Research Web has posted "Why our carbon-dioxide emissions are like credit-card debt," which explains how it grew out of earlier work by Davis and others (Davis, Caldeira and Matthews, Science, 2010). This quote from Davis is particularly helpful:

"One of the things that makes climate change such a difficult problem is that it lacks immediacy," Steven Davis of the University of California, Irvine, told environmentalresearchweb. "It's going to have huge impacts in the long run, but its effects on our day-to-day lives seem small. The way we've been tracking carbon-dioxide emissions reinforces this remoteness: the annual emissions we monitor are small relative to the cumulative emissions that will cause large temperature increases. The alternative we present, what we call commitment accounting, helps by quantifying the long-run emissions related to investment decisions made today."

I sought reactions from a host of energy and climate analysts, kicking things off with this query and thought (some email shorthand is cleaned up):

You are probably aware of "Commitment Accounting of CO2 Emissions," a valuable new Socolow/Davis paper (building on Davis, Caldeira, Matthews, 2010).

Given the near-term and enduring benefits of electric power expansion in developing countries, the other long-term effect of expanded coal-powered generation is accrued wealth and economic growth (along with health costs if they are dirty plants, of course). You could call it a gigawatt-hours commitment.

It'd be interesting to visualize all of this side by side with the emissions commitment in some way.

I think this emerging form of emissions accounting provides a valuable way to show how the growing coal (and natural gas) greenhouse-gas emissions commitment will play out, but — because of the competing social and economic values embedded in that extracted energy, along with the equity argument poor countries use against established fossil-powered industrial giants — I'm not sure it leads to a more effective strategy for cutting those emissions.

I'd love to include your thoughts on this, including links to relevant background that bolsters your points…. On complex issues the best way to pinpoint "reality" is through discourse. As in celestial navigation, the more "lines of position," the tighter the resulting area on the chart.

(Please excuse the acronyms below. For now, please use Google to find definitions. I don't have time at the moment to include explanatory links.)

Christopher Green, an energy-focused economist at McGill, was first to reply:

Without taking anything away from the importance of the Davis-Socolow contribution, your suggestion that we should also look at the benefits of the electricity generated is, in my opinion, dead on. The world as a whole (especially the emerging/developing country component) is going to require increased energy consumption for the foreseeable (and likely more distant) future. That that energy, however produced, provides enormous benefits cannot be denied

The important question is how the world's huge and growing energy requirements are going to be met. Hoffert et al (1998) [the paper is here] provided what still is the clearest framework for establishing the huge magnitude of the energy technology challenge to meeting a growing energy commitment—a challenge measured in terawatts not gigawatts. That challenge has been largely ignored, with the policy focus placed on emissions and emissions reduction and the political will to reduce them, without due regard to the current limits on alternative low carbon energy technologies. The failure to address the Hoffert et al energy technology question is reflected in the fact that since 2000 (and including 2013) the share of global energy consumption accounted for by fossil fuels has remained essentially constant at 86.5-87.0%. (Here I use BP Energy Statistics.) globally, the "progress" made with non-hydro renewables is offset by a decline in energy from nuclear power plants. Not surprisingly, the carbon content of energy is the same in 2013 as it was in the early 1990s and actually rose a little since 2000.

While Davis and Socolow are clearly right that the climate has not benefited from the lack of progress on the energy technology front, billions of people, particularly in the emerging country/developing world, have benefited substantially from the energy generated. As far as I can see the standoff will continue until there is recognition that climate change is first and foremost an energy technology problem, one that cannot be solved/resolved without a great deal more than emission reduction pledges.

David Hawkins of the Natural Resources Defense Council was concerned that I was using too wide a brush:

You say— "Given the near-term and enduring benefits of electric power expansion in developing countries, the other long-term effect of expanded coal-powered generation is accrued wealth and economic growth…"

This statement conflates three things: electrification services, electric generating capacity, and coal-fired generating capacity.  The implication is that there is a serious tradeoff between constraining cumulative global CO2 emissions and meeting the needs of developing countries for increased electrification services.  Truth is, the CO2 commitment from new generating capacity in the poorest countries will be small, even if they build mostly coal.  But building mostly coal is not the only path they or other countries need to follow to expand electrification services.  When the world's wealthiest countries begin to take climate protection seriously, there are ways in which any incremental costs of pursuing a low-carbon electrification path in poorer countries can be shared based on all countries' strategic interests in avoiding a disrupted climate.

Steve Davis, one of the paper authors, added this:

Dave is right to point out that the largest commitments we've quantified are only distantly related to meeting the energy needs of the underserved. The big commitments reflect coal-based industrialization and energy-intensive development whose value is more questionable given the climate and health impacts entailed and availability of cleaner and more energy-efficient options.

I responded with this question:

But given urbanization trends, particularly, centralized power production and the jobs and output that come with industrialization are certainly a big factor for many governments, right?

Davis replied:

Perhaps, but that's the distant relation. We point out that the world built 89 GW [gigawatts, or billion watts] of coal-fired capacity per year 2010-2012. That's roughly equal to the entire generating capacity of sub-Saharan Africa being added every year. These plants are supporting large-scale industrialization that is a world apart from providing basic energy services, even if one dreams of the other. They're related just as the merits of different graduate schools are in the minds of parent teaching their toddlers to read.

Chris Green responded to Davis and Hawkins:

Yes, Dave is talking about the underserved in the sense of the poorest many of whom are not even hooked up to the grid. But my comment addresses the huge energy demands as people move beyond the very poorest. Think here of the many countries, especially the populous ones, that are industrializing and urbanizing. They inevitably will require a lot of energy, if for no other reason than that materials for construction (steel, cement, flat glass, aluminum, copper) are hugely energy intensive — with energy intensities an order of magnitude higher than that for most other manufactured goods. Think too about the demand for appliances including air conditioning as people move into the middle class. These are key factors in the rise in energy demand and the observed increase in fossil fuel generating capacity.

I also take issue with Dave's suggestion of good alternatives to fossil fuel generated energy. With the possible exception of nuclear energy, which to date has faced numerous hurdles, there certainly aren't on anything like the scale required. And little has changed in this respect since Hoffert et al, 1998.

Alex Trembath at the Breakthrough Institute joined the general discussion:

Thanks for the note. As you know, Breakthrough and our colleagues at the Consortium for Science, Policy & Outcomes (and development/energy experts from across the world) addressed this issue in our April report "Our High-Energy Planet." As Professor Green mentioned, the singular focus on emissions is pervasive, and in some cases understandable (for instance, comparing national emissions accounts — measured in MTCO2 — is often much easier than harmonizing and comparing trade-adjusted energy consumption — measured variously in Mtoe, GWhs, bbls, EJs, etc etc). But in the case of energy in emerging economies, the laser focus on emissions is inappropriate.

There has been some movement towards a "gigawatt-hours commitment," as you write. This is the Decade of Sustainable Energy for All, after all. Unfortunately, the dominant frameworks used for understanding the energy access challenge — including those of the UN and IEA — are pretty clearly unacceptable. There are two main problems. The first is an almost exclusive focus on basic household electricity access, often in remote areas, without attendant attention to urbanizing populations, industrializing economies, etc. The second is the scale of ambition. As most on this thread will know, energy access is defined at 250-500kWh/year. This compares to the average German consumption of over 7000kWh/yr. With German levels of consumption, a planet of 9-10 billion in midcentury would require three times as much energy as the world does today.

If we don't start with this very basic, fundamental point, then we're not really having a discussion about energy development or climate change. Again, as Professor Green writes, these realities are commonly ignored, even though folks like Marty Hoffert, Nathan Lewis, Richard Smalley, and John Holdren pointed them out over a decade ago.

Morgan Bazilian and Roger Pielke, Jr. have described what it actually take for sub-Saharan Africa to reach levels of energy consumption enjoyed by South Africans or Americans. China, India, Indonesia, South Africa, and other emerging countries have of course developed largely with coal-fired power. Africa appears poised to mostly leapfrog coal straight towards large hydro and natural gas. No one has yet conceived of a feasible energy development strategy — to power cities, industries, major infrastructure, etc — with renewables or nuclear as the dominant energy sources. Fortunately, a lot of the much-needed work on delivering truly scalable and affordable zero-carbon alternative is being done in the developing world itself. China is pursuing nuclear, solar, and carbon capture at a much greater scale than most Western economies. There are several dozen other countries investing in next-generation nuclear technologies (along with things like renewables, shale gas, coal-to-gas, etc.) to power rapidly growing demand. If decarbonization is to remain a priority — as it should — the energy innovation momentum of the developing world must be captured and accelerated.

I would finally recommend the work of Catherine Wolfram at UC Berkeley, who has both criticized the energy projections methods of the IEA and most recently introduced the very helpful framework of "under-grid" populations, which are very near but unconnected to nascent electricity grids. While some in the West have apparently decided that delivering energy access is a household event best pursued by developed-world charities, NGOs, and entrepreneurs, what we actually see with electricity is similar to what we see with food — good governance and political institutions are essential for equitable and abundant distribution.

Amory Lovins of the Rocky Mountain Institute weighed in:

On the contrary, everything has changed since 1998, making Marty's paper even less relevant today. A few quick highlights, doubtless incomplete:

- Half the new generating capacity the world has added since 2008 has been renewable. (In 2013, 68% of China's new capacity was renewable, the majority of it solar and wind; in Europe, 72%.)

- In each of the past three years, the world invested >$250b investment in non-hydro renewables, adding >80 GW per year. Orders for central thermal plants continue to fade because they have no business case.

- PV power is scaling faster than cellphones worldwide, and in concert with high end-use efficiency (e.g. LED lighting) has extraordinary potential to reach those with no electricity as well as in peri-urban areas.

- China in 2012 increased electricity output more from non-hydro renewables than from all fossil-fueled and nuclear sources, and in 2013, added more PV capacity than the US had added since it invented PVs in 1954. RMI's Reinventing Fire: China collaboration with ERI, EF/C, and LBNL is turning up cost-effective practical potential to raise China's 2050 carbon productivity (GDP per unit of fossil fuel) by ≥15x. The potential in India, where a revolution in efficiency and renewables is also emerging, may be even greater. Both these countries make more electricity from windpower than from nuclear power.

- Unsubsidized US market prices in favorable US sites are ~$0.07/kWh for PV power and ~$0.04/kWh for windpower, with both falling rather rapidly, but already they beat new combined-cycle gas, even neglecting gas's ~$2/GJ price-volatility cost.

- Grid integration of high-renewables mixes, for those paying attention, is now an interesting evolutionary opportunity, not a prohibitive technological or economic challenge. (See http://www.rmi.org/storage_necessity_myth_amory_lovins for a short nontechnical summary of why no breakthrough in bulk electrical storage is needed.) Four EU countries not especially rich in hydropower got about half their 2013 electricity consumption from renewables—Spain 45%, Scotland 46%, Denmark ≥47%, Portugal 58%—with excellent reliability and no additions of bulk storage.

- Micropower—the Economist's term for renewables, less big hydro, plus cogeneration—now produces one-fourth of the world's electricity (>2x nuclear output); see RMI's July 2014 Micropower Database update for details.

- Commonly mentioned renewable issues around land-use turned out to be a canard (http://www.rmi.org/Knowledge-Center/Library/2011-07_RenewableEnergysFootprintMyth).

- Both globally and nationally, renewables excluding big hydro have scaled at least as fast as nuclear power ever did, and without its two-decade "windup" period of building the very demanding capabilities and complex institutions required.

- Properly integrated renewables have emerged as a uniquely profitable and practical pathway to resilient grids that make big cascading blackouts impossible—without adding material cost (see Transform scenario in Reinventing Fire).

- Although U.S. utilities typically pay ~$0.02–0.03/kWh for efficiency, RMI's empirically grounded Reinventing Fire synthesis showed in detail how to quadruple U.S. electric end-use efficiency at an average cost of ~$0.007/kWh (2009 $). The average IRR for 3-4x higher energy productivity in US buildings is 33%; for doubled energy productivity in US industry, 21%. Previous analyses show higher costs and smaller savings because they left so much out, including integrative design, which often turns diminishing into expanding returns to investments in energy efficiency.

- The world is investing >$300b/y in energy efficiency (the electric fraction is unknown but significant), and some major economies like the US and Germany show pretty steady declines in electricity use even as their economies grow. US weather-adjusted electric intensity, for example, fell 3.4% in 2012 alone. It's probably reasonable to estimate that efficiency's annual addition to global electrical services is at least comparable to that of nonhydro renewables.

- It is not essential for developing countries to repeat industrialized countries' historic trajectories: on the contrary, they can leapfrog in energy supply as many did in cellphones. Some are already doing exactly that. Experience teaches that waiting for the wires to reach the villages, bringing unaffordable thermal power, is impractical. The smart solution is to skip the wires, just as in telecomms, and go efficient/renewable/resilient/distributed.

- In general, developing countries have lower end-use efficiency and have more infrastructure yet unbuilt, and they can more easily build right than fix later, so they have far more dynamic and capacious efficiency opportunities than industrialized countries.

- As Ashok Gadgil and I showed ~23 years ago from World Bank data, investing in negawatts wherever they're cheaper than megawatts cuts by ~4 orders of magnitude (3 from intensity, 1 from velocity) the capital needed by the power sector — the most capital-intensive sector, gobbling about ¼ of all development capital. Such least-cost investment could turn that sector into a net exporter of capital to fund other development needs. That's the most powerful macroeconomic lever we know for global development; yet few finance ministers have ever heard of it.

In short, convergent trends in renewable and distributed power, empowered customers, liberalized markets, transparent pricing, and radical end-use efficiency are building an energy future very different from the past. Powerful players are betting on this new horse, coming up fast on the outside. Those who can't see that horse will continue to lose value, because their preferences have more cost and financial risk than investors wish to fund. These market forces will ultimately prove more important than policy, international agreements, or the inertia of those with old ideas and trapped equity.

I haven't time to enter a protracted discussion about these facts and ideas, but was surprised by their absence from the thread, and hope their injection may prove helpful.

Chris Green responded to Lovins's arguments:

It is hard to square the energy facts presented by Amory Lovins with those I have garnered from BP Energy Statistics. While the statistics here (see below) focus on primary energy consumption and those presented by Lovins focus on electricity (a component of final energy) the differences are stark. Here are just a few of the differences:

1. Lovins says renewables (including small hydro and co-generation) account for 47, 58, and 46% of electricity consumption in Denmark, Portugal and Spain, respectively. But non-hydro renewables (NHRs) and all hydro accounted for only 5.7%, 28% and 19%, respectively, of primary energy consumption in 2013 in these three countries. If only NHRs are considered the percentages would be much lower.

2. Globally, NHRs accounted for 2.2% of primary energy consumption in 2013—up from 0.5% in 2000. If all hydro is added in the share in 2013 rises to 8.9%.

3. All of the gain in share of NHRs share since 2000, was offset by the decline in share of nuclear.

4. Lovins claims regarding the contribution of NHRs to electricity consumption in China in 2013 must contend with the fact that the NHRs increased by only 9.4 million million tonnes of oil equivalent (mTOE) between 2012-2013 compared to 100 mTOE for fossil fuels.

As indicated in an earlier intervention, low carbon energy has not made any inroads into the 86.5-87% dominant share of fossil fuels in global energy consumption since 2000. What NHRs have gained has been at the expense of nuclear

I would note that Alex Trembath's useful intervention to this discussion provides insight into why we can expect global energy consumption will continue to grow, and tangentially why so much of that energy will be supplied by fossil fuels without an major breakthroughs in energy technology.

Trembath built on Green's comment:

Indeed, Professor Green, the numbers for even 2013 are not nearly as optimistic as Dr. Lovins suggests. Over 2012, 2013 consumption of different energy sources rose by the following amounts, measured in Mtoe (note these are primary energy, not only electricity):

Oil: 46.1

Gas: 34.1

Coal: 103.0

Nuclear: 3.3

Hydro: 22.2

Wind: 24.0

Solar: 6.9

(Source: BP 2014)

There really ought to be a collegial rule against discussing energy consumption trends without mentioning capacity factor, which explain why 68% of capacity added in 2013 was renewable but a much smaller minority of added generation was renewable. Capacity factor of course also explains why renewables excluding large hydro (and excluding CHP) account for almost twice the installed capacity of global nuclear, yet nuclear in 2013 still generated about 20% more electricity than all those sources combined. These graphs are taken from RMI's Micropower Database; the first is capacity and the second is generation:

Of course we see here also how essential including cogeneration (typically combined heat and power using natural gas) is for drawing such optimistic conclusions about micro generation.

I'm also not sure along what metric Dr. Lovins finds that " globally and nationally, renewables excluding big hydro have scaled at least as fast as nuclear power ever did." As this analysis by my colleagues shows, the best cases of nuclear have outpaced the best cases of nuclear when the metric is added generation divided by national population:

Of course some of the fastest energy, not carbon, transitions have been with natural gas. The UK went from 0% natural gas for electricity in 1990 to 40% in 2000. The US deployed over 250 GW of natural gas generation capacity in the last 20 years, and here's what our own energy transition has looked like:

Certain subsidized and unsubsidized renewables projects can come in at low cost, and we should celebrate these and learn from their successes. But while Dr. Lovins cites 7c/kWh as a best case for solar, the EIA still finds average LCOE of solar at 13c/kWh, higher than advanced nuclear and, of course, higher than natural gas. Wind does appear to have reached an all time low, settling in 4-6c/kWh unsubsidized, as the recent LBNL report showed. However, it must be remembered that these technologies' value to the grid decreases, and integration cost increases, with higher penetration. This is from the work of Lawrence Berkeley National Labs:

This dynamic is evident in Germany, where wholesale power prices are being depressed by must-dispatch, low-marginal cost renewables, but balancing this intermittency is causing retail power prices to rise, both from increasing FIT commitments, and increasingly with costs like capacity payments for baseload power stations and curtailment payments for excess renewables. Here's the results of a review of increasing integration costs from variable renewables:

On the efficiency side of things, we and others have long requested that RMI better incorporate rebound effects into modeling future energy consumption patterns. For instance. In Reinventing Fire (RF), Lovins et al cite 2 studies finding transportation sector rebounds at 3 and 22 percent, but ultimately exclude transportation rebounds from their analysis (Sorrell 2007's survey and the European Commission's review find transpo rebound between 10 and 30 percent; Gavankar and Geyer 2010 identify long-term rebounds between 20 and 65 percent). RF uses 10 and 5 percent rebound for heating and cooling respectively, while Sorrell 2007 finds 10-30 percent for heating and 1-26 percent for cooling. RF rejects the idea of rebounds effects in industrial processes, while Saunders finds rebound in energy intensive industries like primary metals, utilities, manufacturing, and agriculture to be in the range of 20-35 percent. The IPCC and the IEA have recently begun to incorporate rebound effects into their analyses, largely at the behest of organizations like Breakthrough, UKERC, the European Commission, and vocal scholars like Harry Saunders, Steve Sorrell, Joyashree Roy, Dorothy Maxwell, and Karen Turner.

I think it's clear from the above that the world still continues to rely primarily on fossil fuels for development and that even the richest economies are far from achieving significant scaling of renewables (or nuclear) for major decarbonization. Where renewables have scaled, they have brought national electricity prices right up with them. This is especially true for solar PV, where in Germany and Spain FIT payments have caused serious energy policy turmoil, and in the US, where net metering policies have caused public utility backlash against PV deployment in states like Arizona and California (a result of utilities being forced to pay 15-30ckWh for PV electricity instead of purchasing on the wholesale markets for 4-6c/kWh).

To return to the point of Andy's original prompt. Renewables are expanding and their costs are declining, but isolated and contextless success stories don't help us understand the true scale of both the climate and energy development challenges. Drs. Davis and Socolow's intervention with the new paper is extremely helpful because it aims to reveal the scale of the challenge. While renewables continue to develop worldwide — and while countries as varied as US, UK, China, South Korea, Turkey, UAE, Ethiopia, Vietnam, Jordan, etc continue to develop nuclear — fossil still reigns. Now the deployment of fossil and coal generation in regions like sub-Saharan Africa is very likely a net positive for humanity, since a lack of modern electricity systems is largely what makes those locales most vulnerable to climate and other impacts in the first place. But again, if decarbonization of the global economy is the ultimate goal, then I think it's clear we still need answers to the cost and scalability of nuclear and renewables both large and small.

At this point Rob Socolow, one of the paper authors, sought to be sure readers caught the main intent of the paper:

It would be nice to flag what Steve Davis and I have contributed which we think is new.

We are calling attention to a systematic neglect of capital investment decisions in the reporting rules related to climate change, relative to current emissions.

We introduce a concept, "committed emissions," and a methodology to quantify the carbon implications of capital investments.

We show quantitatively that, for the global power sector in any recent year, two quantities are comparable: 1) current emissions that year from all power plants, and 2) "committed emissions" from plants that went on line that year – emissions that can be expected from these plants in the future (when we assume a 40 year lifetime).

We take the concept of remaining committed emissions developed in Steve's 2010 paper with Caldeira and Matthews and work out the trajectory of that value for the global power sector each year over the past 60 years (the earlier paper reported the value for only a single recent year). We find that this index has never fallen, is over 300 GtO2 today and was 200 GtCO2 as recently as Year 2000.

We recommend that "committed emissions" be incorporated prominently into energy analysis, scenario making, and climate policy.

Burt Richter, the physics Nobelist and author of "Beyond Smoke and Mirrors: Climate Change and Energy in the 21st Century," added this comment:

Sorry to jump in late, but I have been away. I think of world energy demand as follows:

Energy = (population) x (per capita income) x (energy/GDP)

We know population is going up (UN mid-level projection is about 9.5 billion by 2050 and 10.5 by 2100), and the poor want to get rich while the rich don't want to get poor, so the only way to work on global energy demand is the last term which is really energy efficiency. If you want to worry about emissions, add another term (emission per unit energy) which is where clean energy comes in. I use "clean" rather than "renewables" because renewables is a term designed to exclude nuclear, big hydro, and large scale efficiency efforts. Taken with most projections for growth energy demand will be up by nearly a factor of 4 by 2100.

What kind of energy is the question? The most recent authoritative numbers for the world that I can find are from the IEA and credit big hydro and combustibles with significant contributions to the total, while wind and solar are quite small. As for Amory's numbers, Denmark is insignificant of the world scale and is connected to the Scandinavian power grid so has lots of back up. Germany is not so connected and so already is having trouble with the stability of its grid. In discussions with Amory in the past I have always found it useful to ask for references for his numbers.

As to the world's poorest countries, they contribute negligibly to emissions and to demand. Let them start up development in any way they can.

Then came input from Nathan Myhrvold, who is best known for his time in research at Microsoft and as an inventor and investor, but has been an author on some relevant energy papers:

Burt's outlook is one that I share.

If you think of energy usage from a "rich world" perspective where there is low growth in demand you can imagine the 21st century challenge to be one where we replace existing fossil fuel energy with clean (in Burt's sense) energy.

But the reality is that the currently poor world is getting richer so by 2100 we need way more primary energy. Today's entire infrastructure will be only ~25% of the picture. The ~4X increase will be in the developing world which will put a huge premium on cost.

As Burt asks, what will that be? At present it is very hard to be optimistic that the new energy will be clean. That isn't the current course.

Amory appears to be far more optimistic than I am, based on numbers that I can't reconcile with the figures available to me.

Daniel Kammen, a professor of energy at the University of California, Berkeley, who happens to edit the journal in which the Davis-Socolow paper is published, offered some overarching thoughts:

As Editor-in-Chief of Environmental Research Letters I am delighted to see this neat paper by Davis and Socolow generating this useful discussion.

Commitment accounting as per Davis and Socolow is useful (I dispute that these facts are not widely known) but it is always useful to be reminded of the implications of our collective decisions today.

The key point that Davis and Socolow make is that when we talk about stranded assets their measure puts this huge looming threat into a form that can easily become something the business community can assess in terms of risks.

When I was at the World Bank my number one goal was to make as many multinational agencies perform life-cycle accounting of emissions on all of their current assets and future potential investments.

This is a step that governments, companies, municipalities and others could commit to at, for example, the September 23Climate Summit in New York.

Even for entities not ready to implement a price on carbon, simply making this accounting a business requirement would dramatically advance the calculation along the lines that Davis and Socolow recommend.

As an example, the University of California system has committed to eliminating fossil fuel use by 2025 — a major task given our transportation footprint.

One way to do this is to start with good, holistic accounting.

We took a step there with a recent national carbon emissions per household map where we show interactively the average footprint for each US zip code. (Yes, a finer-grained map is needed; that paper is next.)

Second, a very simple directive that states, agencies, cities, and the federal government could do to bring the committed emissions into focus is to do that GHG life-cycle analysis along with other project assessments.

In California, for example, we would recommend using the current market price of carbon GHG emissions (around $11/ton in CA), but this could arguably vary to the http://www.epa.gov/climatechange/EPAactivities/economics/scc.html">social cost of carbon or other reasonable values.

From there, agencies, financial officers, CFOs would all know the long-term implications of their decisions.

Kammen appended this thought focused on his years of work in developing countries:

I'd like to add a bit on the developing nation aspects of this conversation.

I have been working in Central America and East Africa for the last 30 years.

I am also just back from far northern Kenya where I was working with the grid planning and the infrastructure for both on-grid wind energy (Africa's largest wind farm is begin built to take advantage of remarkable wind site and the transmission access provided by a new Kenya-Ethiopia linking line). Photo over Lake Turkana with the wind site at upper right (construction begins this fall).

Kenya's grid today is 1.8 GW, and the country's least-cost form of new energy is geothermal (8.5 cents/kWh) for which the economic resource is > 9 GW.

Second, off-grid solar is fastest growing and largest component of new energy access in a country with 29% grid access today. One company with which my lab has an NDA/MOU is the largest user of mobile online money in the country.

Kenya is also on path to replace its hydropower dominated grid of today with one where wind and geothermal are the largest providers of energy (hydropower in the region is increasingly uncertain due to climate change).

Kenya is not unique. Many nations have this clean energy capacity. This message gets lost all the time. 80%+ clean energy paths are not at all hard to find (we are doing assessment for 10 nations right now), and other researchers are doing similar things elsewhere.

On and off-grid are both vital, and public-private partnerships and pure private sector investments are key. We need to find ways to support locally directed efforts that meet these fully decarbonized local visions.

Steve Davis circled back the prime points of the paper:

Regardless of how well renewables are or are not doing, the point Rob and I are trying to make is that fossil infrastructure is still expanding in a big way: the total committed emissions represented by power plants is growing even faster than annual emissions. Whether or not we share Amory's rosy outlook on renewables, these fossil commitments are inconsistent with a decline in emissions any time soon.

Myhrvold reacted:

This is a key point — the fossil infrastructure is still expanding.

Ken Caldiera and I have done a lot of work recently in modeling atmospheric GHG concentration during switchover from fossil fuels to clean energy. A general lesson that comes from this work is that inertia in the climate system means that the "hangover" from emission lasts for decades. Radiative forcing due to greenhouse gases and global average temperature continue to rise for a long time.

So even if you stopped emissions today, we would have climate impact for decades.

But we are not stopping today – the fossil infrastructure is still expanding. The metric of "committed emissions" makes that clear.

Indeed if one combined that metric with modeling results you could call it "committed delta T" – in effect power plant construction commits us to higher global average temperature.

As promised, here's the transcript of Davis's video presentation on the work:

Video Abstract for Commitment Accounting of CO2 Emissions, Davis and Socolow

One of the things that makes climate change an especially difficult problem is that, for the average policymaker, and certainly the average person, it lacks immediacy. As one psychologist puts it, "Climate change may ruin your future, but it won't mess up your evening."

The fact that climate impacts are a threat in the long-run and will materialize slowly over time make it hard for us to get very excited about responding to the threat, no matter how devastating the impacts may turn out to be.

The problem is, our instinct to wait and see is at odds with another characteristic of climate change, which is that it's a problem with huge inertia.

There's a bit of physical inertia—it would take temperatures a few years to catch up with all the CO2 we've been dumping into the atmosphere even if we stopped today.

But more importantly, there is a tremendous amount of social, economic and political inertia. We've spent nearly two centuries and tens of trillions of dollars worldwide building up the largest network of infrastructure that has ever existed to extract, process, and deliver fossil fuels and fossil energy to consumers. All of this long-lived infrastructure represents an enormous investment that won't be easy to walk away from.

The idea behind the new paper my co-author Rob Socolow and I have written is that it's possible to estimate future GHG emissions that are locked-in by all the existing fossil infrastructure, what we call "committed emissions." Our paper demonstrates the concept of this commitment accounting by quantifying the CO2 emissions that are expected to come from now-existing power plants.

Rather than tallying up CO2 emissions from power plants in the year they come out of the plant's smokestacks, we assume a typical plant lifetime of 40 years and allocate the lifetime emissions of each power plant to the year it was built.

What we found is that the currently existing power plants around the world—unless they are retired early or retrofitted so that their emissions are captured–can be anticipated to emit roughly 300 billion tons of CO2 in the future. That's about 10 years worth of current emissions from existing power plants alone, and enough to put a big dent in the remaining budget of emissions we can dump into the atmosphere and still have a reasonable chance of avoiding 2 degrees C of warming relative to the preindustrial era.

But even more daunting than this large amount of committed emissions, we found that total committed emissions grew by an average of 4% between 2000 and 2012 as we built more coal-fired power plants over that period than in any previous 12-year period.

Power plants in the US, EU and India each represent about 10% of the current committed emissions, and the incredible expansion of coal-power in China shows up, as all these Chinese plants represent 42% of global committed emissions. Power plants in Japan, Indonesia, Saudi Arabia and Iran also have substantial and growing share of the world total.

Now to be clear, "committed" doesn't mean "unavoidable." There's nothing to stop us from shuttering a brand new power plant or retrofitting it with carbon capture and storage technology, but of course there'd be costs associated with doing of either of those things. Once something is built and operating, there really is some commitment.

SO, coming back to the issues of immediacy and inertia, our hope is that the sort of commitment accounting described and demonstrated in the paper will be taken up by other analysts and used to evaluate the long-run climate impacts of current capital investments, in turn allowing policymakers to confront these distant implications of their decisions in the present.

Thanks for listening, and feel free to email me with questions about the paper or the concept of commitment accounting of GHG emissions.


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Dot Earth Blog: A Closer Look at Turbulent Oceans and Greenhouse Heating

Written By Unknown on Rabu, 27 Agustus 2014 | 15.49

Photo A sailboat encounters a waterspout along a squall line in the Indian Ocean near the Maldives in 1984 (high resolution).Credit Andrew C. Revkin

Updated, 6:30 p.m. | Earth's climate is shaped by the interplay of two complicated and turbulent systems — the atmosphere and oceans. (The photo above is from the two years I spent at that interface as crew on ocean-roaming sailboats.) The oceans hold the majority of heat in the system, are full of sloshy cycles on time scales from years to decades and, despite an increase in monitoring using sophisticated diving buoys, remain only spottily tracked.

It's no wonder, then, that assessing the mix of forces shaping short-term wiggles in global and regional atmospheric temperature (years to decades) remains a daunting exercise. That's why it's worth stepping back after weeks of news about studies of the role of oceans in retarding, and sometimes accelerating, global warming to reflect a bit on the difference between edge-pushing analysis and firm scientific conclusions.

What's firmly established is that the climate is warming, that the buildup of human-generated heat-trapping greenhouse gases is contributing substantially to the warming and that while the buildup of gases is steady, the rise in temperatures is not.

There's been a burst of worthy research aimed at figuring out what causes the stutter-steps in the process — including the current hiatus/pause/plateau that has generated so much discussion. The oceans are high on the long list of contributors, given their capacity to absorb heat. The recent studies have pointed variously to process in the Pacific and Atlantic and Southern oceans (the latter being the extraordinary band of seas in the Southern Hemisphere where winds circulate around the globe unimpeded by continents).

There's important work to be done on this question but — as the oceanographer Carl Wunsch notes at the end of this post — the paucity of data on ocean heat makes it tough to get beyond "maybe" answers.

Peter Spotts of the Christian Science Monitor wrote a nice piece on the battle of the ocean basins. Here's his description of the Atlantic mechanism:

[I]n the Atlantic, the heat is carried north as part of a powerful current system known as the Atlantic thermohaline circulation. The north-flowing Gulf Stream is the most visible manifestation of this circulation.

By the time it reaches the far North Atlantic, the dense, salty water has cooled and sinks. It plunges toward the seafloor and heads south at depth, retaining some of the heat it accumulated on the surface.

In a news article in the journal Science, which published the latest paper on the Atlantic's role in decades-long global temperature fluctuations, Eli Kintisch described the Pacific argument this way: 

[I]n the 17 August Nature Climate Change study, a team led by [Kevin] Trenberth suggests that natural variability in the Pacific explains more than half of the hiatus. Based on data and climate simulations, they argue that a pattern known as the Pacific Decadal Oscillation, which shifts every 20 to 30 years, is driving the increased upwelling as well as other climate trends, including the rapid warming of the Arctic and recent cold winters in Europe.

The newest paper, in the current issue of Science, "Varying planetary heat sink led to global-warming slowdown and acceleration," argues that the Atlantic not only has shaped the current plateau, but also was responsible for half of the sharp global warming at the end of the 20th century. The paper, by Xianyao Chen of the Ocean University of China and Ka-Kit Tung of the University of Washington, has a remarkably trenchant abstract:

A vacillating global heat sink at intermediate ocean depths is associated with different climate regimes of surface warming under anthropogenic forcing: The latter part of the 20th century saw rapid global warming as more heat stayed near the surface. In the 21st century, surface warming slowed as more heat moved into deeper oceans. In situ and reanalyzed data are used to trace the pathways of ocean heat uptake. In addition to the shallow La Niña–like patterns in the Pacific that were the previous focus, we found that the slowdown is mainly caused by heat transported to deeper layers in the Atlantic and the Southern oceans, initiated by a recurrent salinity anomaly in the subpolar North Atlantic. Cooling periods associated with the latter deeper heat-sequestration mechanism historically lasted 20 to 35 years.

In an e-mail exchange, Ka-Kit Tung noted how this work can help reveal the steady warming in the background that is attributable to human activities:

The underlying anthropogenic warming trend, even with the zero rate of warming during the current hiatus, is 0.08 C per decade.* [That's 0.08 degrees Celsius, or 0.144 degrees Fahrenheit.] However, the flip side of this is that the anthropogenically forced trend is also 0.08 C per decade during the last two decades of the twentieth century when we backed out the positive contribution from the cycle….

This aspect of the work was largely missed in press coverage. I asked a range of climate and ocean scientists to weigh in on the paper. Many focused on details of the Atlantic-Pacific debate. A few took a broader view that's worth sharing:

Joshua K. Willis of NASA's Jet Propulsion Laboratory said this:

In regards to your question, if you mean how robust is the "slowdown" in global surface warming, the answer is it just probably just barely statistically significant. If you are wondering whether is it meaningful in terms of the public discourse about climate change, I would say the answer is no. The basic story of human caused global warming and its coming impacts is still the same: humans are causing it and the future will bring higher sea levels and warmer temperatures, the only questions are: how much and how fast?

As far as the cause of the slowdown, I think there is still some debate, not just about the cause but about the details of what's going on. For example, there have been several studies including this one to suggest that some deeper layer of the oceans are warming faster now than they were 10 or 15 years ago. This suggestion of an accelerated warming in a deep layer of the ocean has been suggested mostly on the basis of results from reanalyses of different types (that is, numerical simulations of the ocean and atmosphere that are forced to fit observations in some manner). But it is not clear to me, actually, that an accelerated warming of some sub-surface layer of the ocean (at least in the globally-averaged sense) is robustly supported by the data itself.

Until we clear up whether there has been some kind of accelerated warming at depth in the real ocean, I think these results serve as interesting hypotheses about why the rate of surface warming has slowed-down, but we still lack a definitive answer on this topic.

Here's Andrew Dessler of Texas A&M University:

There are a few interesting things to note here.

First, the hiatus is example of how science works. When it was first observed a few years ago, there were lots of theories — including things like stratospheric water vapor, solar cycles, stratospheric aerosol forcing. After some intense work by of the community, there is general agreement that the main driver is ocean variability. That's actually quite impressive progress and shows how legitimate uncertainty is handled by the scientific community.

Second, I think it's important to put the hiatus in context. This is not an existential threat to the mainstream theory of climate. We are not going to find out that, lo and behold, carbon dioxide is not a greenhouse gas and is not causing warming. Rather, I expect that the hiatus will help us understand how ocean variability interacts with the long-term warming that humans are causing. In a few years, as we get to understand this more, skeptics will move on (just like they dropped arguments about the hockey stick and about the surface station record) to their next reason not to believe climate science.

As far as this particular paper goes, I think the findings that the heat is going into the Atlantic and Southern Ocean's is probably pretty robust. However, I will defer to people like Josh Willis who know the data better than I do.

What's most exciting to me is that this is really a fascinating conundrum. People like Kevin Trenberth and Kosaka and Xie have published quite convincingly that the action seems to be in the Pacific. So the challenge is to try to resolve that evidence with the ocean heat data that shows that the energy is going into other ocean basins. Ultimately, the challenge come up with the parsimonious theory that fits all of the data.

I do think that ocean variability may have played a role in the lack of warming in the middle of the 20th century, as well as the rapid warming of the 1980s and 1990s. But the argument that the hiatus will last for another decade or two is very weak and I would not put much faith in that. If the cycle has a period of 60-70 years, that means we have one or two cycles of observations. And I don't think you can much about a cycle with just 1-2 cycles: e.g., what the actual period of the variability is, how regular it is, etc. You really need dozen of cycles to determine what the actual underlying variability looks like. In fact, I don't think we even know if it IS a cycle.

And this brings up what to me is the real question: how much of the hiatus is pure internal variability and how much is a forced response (from loading the atmosphere with carbon). This paper seems to implicitly take the position that it's purely internal variability, which I'm not sure is true and might lead to a very different interpretation of the data and estimate of the future.

Thus, their estimate of 1-2 more decades before rapid warming resumes might be right; but, if so, I'd consider them lucky rather than smart.

John Michael Wallace, a professor emeritus of atmospheric sciences at the University of Washington, offered these thoughts:

Back in 2001 I served as a member of the committee that drafted the National Research Council report, "Climate Change Science: An Analysis of Some Key Questions." The prevailing view at that time, to which I subscribed, was that the signal of human-induced global warming first clearly emerged from the background noise of natural variability starting in the 1970s and that the observed rate of increase from 1975 onward could be expected to continue into the 21st century. The Fourth Assessment Report of the IPCC, released in 2007, offered a similar perspective, both in the text and in the figures in its Summary for Policymakers.

By that time, I was beginning to have misgivings about this interpretation. It seemed to me that the hiatus in the warming, which by then was approaching ten years in length, should not be dismissed as a statistical fluke. It was as legitimate a part of the record as the rapid rises in global-mean temperature in the 1980s and 1990s.

In 2009 Zhaohua Wu contacted me about a paper that he, Norden Huang, and other colleagues were in the process of writing in which they attributed the stair-step behavior in the rate of global warming, including the current hiatus, to Atlantic multidecadal variability. I was initially a bit skeptical, but in time I began to appreciate the merits of their arguments and I became personally involved in the project. The paper (Wu et al.) encountered some tough sledding in the review process, but we persisted and the article finally appeared in Climate Dynamics three years ago. [See Judith Curry's helpful discussion.]

The new paper by Tung and Chen goes much farther than we did in making the case that Atlantic multidecadalvariability needs to be considered in the attribution of climate change. I'm glad to see that it is attracting attention in the scientific community, along with recent papers of Kosaka et al. and Meehl et al. emphasizing the role of ENSO-like variability. I hope this will lead to a broader discussion about the contribution of natural variability to local climate trends and to the statistics of extreme events.

Carl Wunsch, a visiting professor at Harvard and professor emeritus of oceanography at the Massachusetts Institute of Technology, offered a valuable cautionary comment on the range of papers finding oceanic drivers of short-term climate variations. He began by noting the challenge just in determining average conditions:

Part of the problem is that anyone can take a few measurements, average them, and declare it to be the global or regional value. It's completely legitimate, but only if you calculate the expected uncertainty and do it in a sensible manner.

The system is noisy. Even if there were no anthropogenic forcing, one expects to see fluctuations including upward and downward trends, plateaus, spikes, etc. It's the nature of turbulent, nonlinear systems. I'm attaching a record of the height of the Nile — 700-1300 CE. Visually it's just what one expects. But imagine some priest in the interval from 900-1000, telling the king that the the Nile was obviously going to vanish…

Photo Variations in the height of the Nile River over the centuries.Credit Carl Wunsch

Or pick your own interval. Or look at the central England temperature record or any other long geophysical one. If the science is done right, the calculated uncertainty takes account of this background variation. But none of these papers, Tung, or Trenberth, does that. Overlain on top of this natural behavior is the small, and often shaky, observing systems, both atmosphere and ocean where the shifting places and times and technologies must also produce a change even if none actually occurred. The "hiatus" is likely real, but so what? The fuss is mainly about normal behavior of the climate system.

The central problem of climate science is to ask what you do and say when your data are, by almost any standard, inadequate? If I spend three years analyzing my data, and the only defensible inference is that "the data are inadequate to answer the question," how do you publish? How do you get your grant renewed? A common answer is to distort the calculation of the uncertainty, or ignore it all together, and proclaim an exciting story that the New York Times will pick up.

A lot of this is somewhat like what goes on in the medical business: Small, poorly controlled studies are used to proclaim the efficacy of some new drug or treatment. How many such stories have been withdrawn years later when enough adequate data became available?

Addendum, 6:30 p.m. | Ka-Kit Tung responded to Wunsch and Dessler in an e-mail.

Here's his reply to Carl Wunsch's reaction:

Carl Wunsch's concern over the sparsity of the ocean data, as expressed in his recent papers, is mostly related to the part of the ocean below 2000 m (the abyssal ocean). He pointed out the signal in the abyssal oceans were mostly at least 500 years old. The signals that we are interested for the current hiatus of the past 15 years came down from above and have not reached the part of the ocean below 2000 m. We used only data above 1500 m and our case was made in Figure 2 of the paper using recent data with better coverage.

And Andrew Dessler's reaction:

We did not predict in our Science paper that the current hiatus will last another decade or two. The statement that it will last another "15 years" was found in the press release by Science magazine. We were not given a chance to approve it; it probably was not their practice. In the paper itself, we discussed the fact that "historically" lasted 20-35 years. In our university's press release, we emphasized that it is difficult to predict how long it will last given the changing climate conditions.

Dessler mentioned that there is only 1-2 cycles of this 60-year variability in the short climate record. We discussed this issue in our paper: The global instrumental record since 1850 contains only 2 and half cycles of this 65-year cycle. Tung and Zhou (2013, PNAS) extended it a few hundred years using Central England temperature data. We are currently reexamining Greenland ice-core data that extends the cycle back another thousand years. In addition, free-running models have produced this multidecadal cycles in their control runs (i.e. without anthropogenic forcing), although the latest batch of models have problems getting the period right.

Postscript, 2:13 p.m. | * In a followup chat, Tung asked to slightly expand the comment at the asterisk above.


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