Archive for January 2010

A. A. Bloom et al., Science, 327(5963), Large-scale controls of methanogenesis inferred from methane and gravity spaceborne data

Science (15 January 2010), Vol. 327, No. 5963, pp. 322–325; DOI: 10.1126/science.1175176

Reports

Large-scale controls of methanogenesis inferred from methane and gravity spaceborne data

A. Anthony Bloom,1 Paul I. Palmer,1,* Annemarie Fraser,1 David S. Reay,1 and Christian Frankenberg2
Abstract
Wetlands are the largest individual source of methane (CH4), but the magnitude and distribution of this source are poorly understood on continental scales. We isolated the wetland and rice paddy contributions to spaceborne CH4 measurements over 2003–2005 using satellite observations of gravity anomalies, a proxy for water-table depth {Gamma}, and surface temperature analyses TS. We find that tropical and higher-latitude CH4 variations are largely described by {Gamma} and TS variations, respectively. Our work suggests that tropical wetlands contribute 52 to 58% of global emissions, with the remainder coming from the extra-tropics, 2% of which is from Arctic latitudes. We estimate a 7% rise in wetland CH4 emissions over 2003–2007, due to warming of mid-latitude and Arctic wetland regions, which we find is consistent with recent changes in atmospheric CH4.
1 School of GeoSciences, University of Edinburgh, Edinburgh, U.K.
2 SRON Netherlands Institute for Space Research, Utrecht, The Netherlands. 



*Correspondence e-mail: pip@ed.ac.uk

Link:  http://www.sciencemag.org/cgi/content/abstract/327/5963/322

Real Climate: The Wisdom of Solomon

The wisdom of Solomon

Filed under:  Climate Science — gavin @ 29 January 2010 
 
A quick post for commentary on the new Solomon et al paper in Science Express. We’ll try and get around to discussing this over the weekend, but in the meantime I’ve moved some comments over. There is some commentary on this at DotEarth, and some media reports on the story – some good, some not so good. It seems like a topic that is ripe for confusion, and so here are a few quick clarifications that are worth making.
First of all, this is a paper about internal variability of the climate system in the last decade, not on additional factors that drive climate. Second, this is a discussion about stratospheric water vapour (10–15 km above the surface), not water vapour in general. Stratospheric water vapour comes from two sources – the uplift of tropospheric water through the very cold tropical tropopause (both as vapour and as condensate), and the oxidation of methane in the upper stratosphere (CH4+2O2 –> CO2 + 2H2O; NB: this is just a schematic, the actual chemical pathways are more complicated). There isn’t very much of it (between 3 and 6 ppmv), and so small changes (~0.5 ppmv) are noticeable.

The decreases seen in this study are in the lower stratosphere and are likely dominated by a change in the flux of water through the tropopause. A change in stratospheric water vapour because of the increase in methane over the industrial period would be a forcing of the climate (and is one of the indirect effects of methane we discussed last year), but a change in the tropopause flux is a response to other factors in the climate system. These might include El Nino–La Nina events, increases in Asian aerosols, or solar impacts on near-tropopause ozone – but this is not addressed in the paper and will take a little more work to figure out.

The study includes an estimate of the effect of the observed stratospheric water decadal decrease by calculating the radiation flux with and without the change, and comparing this to the increase in CO2 forcing over the same period. This implicitly assumes that the change can be regarded as a forcing. However, whether that is an appropriate calculation or not needs some careful consideration. Finally, no-one has yet looked at whether climate models (which have plenty of decadal variability too) have phenomena that resemble these observations that might provide some insight into the causes.

Link: http://www.realclimate.org/index.php/archives/2010/01/the-wisdom-of-solomon/

Stefan Rahmstorf & Yvo de Boer: Copenhagen: what next?

Copenhagen: what next?

It's coming up to six weeks since the end of the Copenhagen negotiations on climate change. Now that the dust has settled, there's time to stand back and take a more considered look. Here Yvo de Boer, executive secretary of the United Nations Framework Convention on Climate Change (UNFCCC), and Stefan Rahmstorf, professor of physics of the oceans at Potsdam University, Germany give their views on the outcome of the COP15 talks and the way forward
At a press conference last week, de Boer said that the outcome in Copenhagen made "the task to hand more urgent…the window of opportunity we have to come to grips with this issue is closing faster than it was before." But he claimed that the talks did raise climate-change issues to the highest level of government, helped to define temperature limits and financial contributions, and set 2015 as a date for reviewing whether global action needs to be more urgent.

The Copenhagen Accord, meanwhile, an agreement negotiated by China, South Africa, India, Brazil and the US, and noted by the other nations at the conference, "reflects a political consensus on the long-term global response" that is needed to climate change, according to de Boer. "We are now in a cooling off period," he added. "This gives useful time for countries to resume discussions with each other."

Climate scientist Stefan Rahmstorf thinks that the outcome of COP15 is depressing, but also tried to highlight some more upbeat aspects. "On the positive side: most of the actors in Copenhagen by far were quite willing to commit to a substantial effort to halt global warming – including many who were not willing to do this earlier, for example the US or Australia," he told environmentalresearchweb. "And some important developing countries have made very constructive pledges as well. We were closer than ever to major progress in fighting global warming."

Rahmstorf reckons that an agreement was not reached because "the consensus-based UN process with 192 ountries is very cumbersome, and it was exceptionally badly managed at this conference," because China did not play a very constructive role and because the US was not able to offer enough. "The IPCC deemed 25–40% emissions reductions below 1990 values necessary by 2020 by developed nations to limit warming to 2 °C, and what the US offered amounted to only 4%," he explained. "This is largely a result of the lost years under previous administrations, during which the US emissions increased steeply – unlike those in Europe."

During his briefing, de Boer said that he never ceases to be amazed by the vision that some people have of the UN. "To me it is a collection of countries that have created a body to facilitate negotiation among each other," he added. "If those governments were to go and negotiate in a different setting with a different secretariat I don't know if that would fundamentally change their behaviour."

Keeping on the UN track
Both de Boer and Rahmstorf would like to see the UN process continue. "Everybody I have spoken to so far doesn't want the Accord to be a third track," said de Boer.

Rahmstorf agrees. "I hope that the multilateral UN track to a global climate agreement will not die, however cumbersome it is, because the alternatives are even worse," he said, "for example, the G20 with only the biggest emitters on the table deciding alone on climate policy, without those affected, like the small island nations, having a proper voice." In the meantime, Rahmstorf says that "while we wait for our world leaders to get their act together, there is nothing to stop us as world citizens to do all we can to reduce emissions bottom-up."

The next UNFCCC negotiating session is due to take place in late May 2010 in Bonn, with the next COP meeting set for Mexico in late November. According to de Boer, many countries feel that there is a need for an intensified negotiating schedule this year – he plans to convene the COP bureau to determine whether it's possible to slot in another set of negotiations before May 2010.

The countries that negotiated the Copenhagen Accord – China, South Africa, India, Brazil and the US – account for around 80% of carbon emissions. "It's true to say there was not final agreement on the Accord, but an overwhelming majority supported it," said de Boer. "It was not formally adopted by COP – only noted – and we should be careful not to make it more than it is."

But de Boer believes the Accord is a political tool that has broad support at a high level and that can be usefully employed in negotiations. He says the Accord is clear on a long-term goal, on how it can be measured, on financial support and on a number of new institutions that need to be established. "It can be used by us to help speed up the negotiations," he said.

Countries have until 31 January to let the UN know if they wish to be associated with the Accord in the official report of the COP15 negotiations. Industrialized countries have the option of including details of the targets they intend to commit to, while developing nations can indicate the action that they plan to take. The deadline is for administrative reasons only; the list of countries associated with the Accord will be updated on the UNFCCC secretariat website as later details come in. "It's a soft deadline, there's nothing deadly about it," said de Boer.

The climate for science
But what does this mean for the day-to-day lives of researchers? Rahmstorf believes the outcome in Copenhagen has no direct or immediate effects on climate science. "The morale of many is shaken, though," he added. "We've got an important job: since the Copenhagen Accord calls for limiting global warming to a maximum of 2 °C, possibly even 1.5 °C (this option is left open at the end of the Accord), one of the major tasks of science will be to narrow down the range of future emissions that is compatible with these policy goals."

Rahmstorf reckons that climate scientists have communicated their work quite well, particularly through the IPCC. While 2010 is the UN year of biodiversity, the biodiversity community has "not yet managed to get as much high-level attention to the biodiversity crisis; it is only now calling to set up something like the IPCC for biodiversity." On the other hand, "climate science could still do a lot better if more climate scientists get involved, take an interest in public understanding of science and educate themselves more about how to effectively work with the media". Rahmstorf reckons that "too many scientists are still stuck in the ivory tower and – for example – shrug off and ignore wrong media reports about climate science, rather than recognizing that public perception matters and that they should not leave the public debate to people with a political agenda."

The last word goes to de Boer: while the Copenhagen negotiations "didn't produce the final cake," they did leave countries "with all the key ingredients to bake a new one." Although the proof of the pudding, as they say, is in the eating.

Link:  http://www.guardian.co.uk/environment/2010/jan/29/copenhagen-what-next

Susan Solomon: Water vapor caused one-third of global warming in 1990s

Water vapour caused one-third of global warming in 1990s, study reveals

Experts say their research does not undermine the scientific consensus on man-made climate change, but call for 'closer examination' of the way computer models consider water vapour
Cloud
A 10% drop in water vapour, 10 miles up has had an effect on global warming over the last 10 years, scientists say. Photograph: Getty

Scientists have underestimated the role that water vapour plays in determining global temperature changes, according to a new study that could fuel further attacks on the science of climate change.

The research, led by one of the world's top climate scientists, suggests that almost one-third of the global warming recorded during the 1990s was due to an increase in water vapour in the high atmosphere, not human emissions of greenhouse gases. A subsequent decline in water vapour after 2000 could explain a recent slowdown in global temperature rise, the scientists add.

The experts say their research does not undermine the scientific consensus that emissions of greenhouse gases from human activity drive global warming, but they call for "closer examination" of the way climate computer models consider water vapour.

The new research comes at a difficult time for climate scientists, who have been forced to defend their predictions in the face of an embarrassing mistake in the 2007 report of the Intergovernmental Panel on Climate Change (IPCC), which included false claims that Himalayan glaciers could melt away by 2035. There has also been heavy criticism over the way climate scientists at the University of East Anglia apparently tried to prevent the release of data requested under Freedom of Information laws.

The new research, led by Susan Solomon, at the US National Oceanic and Atmospheric Administration, who co-chaired the 2007 IPCC report on the science of global warming, is published today in the journal Science, one of the most respected in the world.

Solomon said the new finding does not challenge the conclusion that human activity drives climate change. "Not to my mind it doesn't," she said. "It shows that we shouldn't over-interpret the results from a few years one way or another."

She would not comment on the mistake in the IPCC report -- which was published in a separate section on likely impacts -- or on calls for Rajendra Pachauri, the IPCC chairman, to step down.

"What I will say, is that this [new study] shows there are climate scientists round the world who are trying very hard to understand and to explain to people openly and honestly what has happened over the last decade."

The new study analysed water vapour in the stratosphere, about 10 miles up, where it acts as a potent greenhouse gas and traps heat at the Earth's surface.

Satellite measurements were used to show that water vapour levels in the stratosphere have dropped about 10% since 2000. When the scientists fed this change into a climate model, they found it could have reduced, by about 25% over the last decade, the amount of warming expected to be caused by carbon dioxide and other greenhouse gases.

They conclude: "The decline in stratospheric water vapour after 2000 should be expected to have significantly contributed to the flattening of the global warming trend in the last decade."

Solomon said: "We call this the 10, 10, 10 problem. A 10% drop in water vapour, 10 miles up has had an effect on global warming over the last 10 years." Until now, scientists have struggled to explain the temperature slowdown in the years since 2000, a problem climate sceptics have exploited.

The scientists also looked at the earlier period, from 1980 to 2000, though cautioned this was based on observations of the atmosphere made by a single weather balloon. They found likely increases in water vapour in the stratosphere, enough to enhance the rate of global warming by about 30% above what would have been expected.

"These findings show that stratospheric water vapour represents an important driver of decadal global surface climate change," the scientists say. They say it should lead to a "closer examination of the representation of stratospheric water vapour changes in climate models."

Solomon said it was not clear why the water vapour levels had swung up and down, but suggested it could be down to changes in sea surface temperature, which drives convection currents and can move air around in the high atmosphere.

She said it was not clear if the water vapour decrease after 2000 reflects a natural shift, or if it was a consequence of a warming world. If the latter is true, then more warming could see greater decreases in water vapour, acting as a negative feedback to apply the brakes on future temperature rise.

Link:  http://www.guardian.co.uk/environment/2010/jan/29/water-vapour-climate-change

Yuan Revaluation Pending





These monetary maneuvers by the Chinese government surely presage a revaluation of the Yuan dollar peg.  It will now obviously benefit China by somewhat cooling things off internally and allowing them more time to place their huge US dollar pool. This should actually happen very quickly.

The Chinese are also diversifying their currency holdings but there is only so much that can be done quickly.  Again the next two years will be used to perfect this new policy.

The USA is still getting its fiscal house in order in a process that if not accelerated by government action, promises to last a decade.

So we can expect a slow delinking of the Yuan into a basket of currencies and a step by step advance in the value of the Yuan for at least ten years.  We may be impatient with them but recall this is about 1.3 billion people transitioning into a middle class consumer society and they are trying to bring the whole country along.  So far they are doing fantastic and have avoided hillside slums that is common most other places.


January 28, 2010


Alan Ruskin, who heads foreign exchange strategy at RBS Securities, notes there is more evidence of a strengthening U.S. dollar than there is to indicating a weakening in the currency. "The dollar's rallied quite sharply. There's a sense that as the U.S. economy is recovering it's hard to conceive of a dollar collapse," he said. 

Ruskin said he sees China's recent moves to scale back bank lending as a sign the country could move toward using exchange policies as another tool to tighten monetary policy and fight inflation.
International pressure for the yuan to rise is growing; there are strong expectations for yuan appreciation. Zhong said expectations for a stronger yuan were one of the factors that could weigh on China's exports in 2010, in addition to uncertainties about global economic recovery and trade disputes.

These semi-official comments from a Chinese Minister could indicate that
China will move earlier than this summer to begin re-appreciating the yuan versus the US dollar. It could also signal an increased likelihood of something in the range of 10% one off appreciation.


WSJ discusses one off appreciation versus gradual

The 23% surge in China's foreign reserves last year to $2.4 trillion is a much clearer signal that its currency is undervalued. 

China rightly worries that a new program of gradual appreciation would only encourage more hot money inflows. 

So the alternative is to do it all in one bang. To be sure, a one-off sharp revaluation would strike a major blow at China's export base and induce a significant slowdown in the economy. But since China's competitors would enjoy an exchange rate windfall, contagion would be limited.


Either way, doing nothing and so indefinitely postponing a more violent, involuntary bursting of the bubble is the worst option.

G. A. Catania & T. A. Neumann, GRL 37 (2010), Persistent englacial drainage features in the Greenland Ice Sheet

Geophysical Research Letters, 37 (2010) L02501; doi: 10.1029/2009GL041108.

Persistent englacial drainage features in the Greenland Ice Sheet

G. A. Catania (Institute for Geophysics, and the Department of Geology, University of Texas at Austin, Austin, TX, U.S.A.) and T. A. Neumann (Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Greenbelt, MD, U.S.A.)

Abstract

Surface melting on the Greenland Ice Sheet is common up to ∼1400 m elevation and, in extreme melt years, even higher. Water produced on the ice sheet surface collects in lakes and drains over the ice sheet surface via supraglacial streams and through the ice sheet via moulins. Water delivered to the base of the ice sheet can cause uplift and enhanced sliding locally. Here we use ice-penetrating radar data to observe the effects of significant basal melting coincident with moulins and calculate how much basal melt occurred. We find that more melting has occurred than can be explained by the release of potential energy from the drainage of surface meltwater during one melt season suggesting that these moulins are persistent for multiple years. We find only a few persistent moulins in our study area that drain the equivalent of multiple lakes per year and likely remain active over several years. Our observations indicate that once established, these persistent moulins might be capable of establishing well-connected meltwater drainage pathways. 

Received 26 September 2009; accepted 30 December 2009; published 29 January 2010

Citation: Catania, G. A., and T. A. Neumann (2010), Persistent englacial drainage features in the Greenland Ice Sheet, Geophys. Res. Lett., 37, L02501, doi:10.1029/2009GL041108. 

Feathered Dinosaurs




I have posted extensively on what we call dawn age reptiles. These are critters that are at home in swamps and deep water and are mostly aquatic.  I avoided talking about the later reptiles for the nonce.

The niche occupied by dawn age reptiles immediately solved a huge problem of temperature control.  They lived almost exclusively in water and avoided the whole issue.  Even our old friend Nessie fitted nicely into the oceanic version of this niche.

However, the minute we allow these critters to stray away from water, it is necessary to think about temperature control.  Exposed skin does a poor job of controlling temperature.  We do not go out and work naked in either the mid day sun or the dead of winter without serious consequences.

Every critter exploiting a wider range of temperature using any vigor must be insulated.  Basking is not an activity.  This has meant hair or feathers.

Not surprisingly, these late reptiles are showing signs of using feathers.  This probably thinned out as they became large.  The internal mass by itself would then be largely sufficient.  Down and feathers would be necessary for the young in any case.  I think that the default mode for active advanced reptiles included down and feathers as a pre condition to leaving the swamps.

I think this story is only beginning to be told.

Dinosaur Sported Colorful Feathers
By Jeanna Bryner, LiveScience Managing Editor
posted: 27 January 2010 01:01 pm ET



A meat-eating dinosaur called Sinosauropteryx likely sported a rim of colored feathers on its head, down its back and tail when it lived some 120 million years ago. The tail probably had a striped pattern of orange and white. Credit: © Chuang Zhao and Lida Xing.
_______________________________________
Our image of what dinosaurs looked like has just been colorized, thanks to fossilized feather remains showing one meat-eating beast sported a striped tail of white and gingery bands.

Not only do the results paint a jazzier picture of the ancient giants, they also confirm the presence of real feathers, not just "feather-like" or bristly structures, in some meat-eating dinosaurs called theropods, the scientists say. The finding has implications for understanding the origin of feathers, since scientists think birds evolved from a group of theropods called maniraptors, some 150 million years ago during the Jurassic period.

"Our research provides extraordinary insights into the origin of feathers," said Mike Benton, a professor of paleontology at the University of Bristol. "In particular, it helps to resolve a long-standing debate about the original function of feathers — whether they were used for flight, insulation, or display. We now know that feathers came before wings, so feathers did not originate as flight structures."
Rather, feathers were likely used for color display at first, he added.
Specifically, Benton and his colleagues found remains of melanosomes, which are tiny structures enclosing pigments that are embedded within the structure of feathers. Melanosomes are responsible, in part, for the colors exhibited by the feathers of some modern-day birds, such as zebra finch feathers.
The team looked at melanosomes from remains of theropods and primitive birds using a scanning electron microscope, finding melanosomes for reddish-brown to yellow pigment and those for black-grey pigment. While the remains didn't include actual pigments, the researchers matched the shapes of these melanosomes with those found in the feathers of today's birds to figure out the color. 

The pattern of the melanosome structures suggested the theropod Sinosauropteryx had simple bristles with alternating white and ginger, or chestnut-colored rings down its tail. And the early bird Confuciusornis had patches of white, black and orange-brown coloring on parts of its body.

"There's a very clear rim of feathers running down the top of the head kind of like a Mohican [Native American headdress] all the way down the back and along the tail," Benton said, referring to feathers on Sinosauropteryx, which lived some 120 million years ago.

In the past, some have suggested that what scientists assumed were fossilized feathers were actually bits of tissue.

"These bristles really are feathers," Benton said during a press briefing yesterday on the discovery. "If they were bits of skin or connective tissue or something else they would not contain melanosomes."

A Gust of Energy




I find this a good discussion on the need for an aggressive government program to expand and also rationalize energy production and transmission.  Beyond that I want to repeat a couple of comments of mine on the subject.  The first item is that most of the various issues disappear the moment we have some energy storage put in place.  For starters, Calcium hydride with thermal solar is a natural industrial grade energy storage system that could easily be used instead of having a power plant on standby for fifty hours of usage per year. 

The second issue is that the advent of the true electric car is imminent in some form or the other.  Each car becomes an energy storage device in its own right.  However the demand for all forms of energy production can be expected to sky rocket.

The USA should be gearing up to provide loan guarantees and sales contracts to accommodate this rapid build out that will compare to the headlong expansion taking place in China.  We could use three years of that.

The absolute best policy that the USA and Canada can enact is fund an aggressive replacement of all imported non North American oil.  We have more than enough internally if we swiftly displace transportation energy into electricity.  We will likely become net exporters of oil once we fully transition to wind, solar and geothermal through a national grid.

This is a huge job and a massive retooling of the North American economy comparable to declaring war and going to full mobilization.  Yet it is all naturally pays out through internal cash flow.



A gust of energy

22 JAN 2010 1:53 PM






The great hope for powering a sustainable world is renewable energy. The great barrier to powering a sustainable world is the cost and complexity of building a new national transmission grid that will transmit the carbon-free electricity generated by remote wind farms and solar power plants to population centers.

In 2008, the U.S. Department of Energy released a report that concluded the United States could obtain 20 percent of its electricity from wind power by 2030. This week the Energy Department’s National Renewable Energy Laboratory issued a study that shows how the eastern half of the U.S. could obtain as much as 30 percent of its electricity from wind by 2024. The study focused on what transmission geeks call the Eastern Interconnection, six linked regional power grids that run from the Great Plains to the Eastern Seaboard and from the Canadian border to the tip of Florida.

“Although significant costs, challenges, and impacts are associated with a 20 percent wind scenario, substantial benefits can be shown to overcome the costs,” the report’s authors wrote. “Such a scenario is unlikely to be realized with a business-as-usual approach, and that a major national commitment to clean, domestic energy sources with desirable environmental attributes would be required.”
Essentially, all we need to do is come up with at least $93 billion for new power lines and infrastructure and get myriad transmission operators and local agencies to cooperate on the design of a new high-voltage grid.
Sounds daunting. But let’s put the numbers in context. The $93 billion is roughly what the U.S. spends in eight months on the Iraq and Afghanistan wars. Or to use another metric, a little more than what Joe Taxpayer forked over to bail out AIG.
The payback to build a transmission grid, however, is likely to be far more productive.  Such an expansion of transmission capacity (and the resulting increase ) in wind power—and one assumes, other renewable energy—would displace coal-fired power plants, according to the NREL.
It would also solve one of the biggest problems with wind—its intermittency, which plays havoc with keeping electricity flowing smoothly. To greatly simplify, the wind is usually blowing somewhere. By multiplying the number of wind farms that feed into a single transmission grid from a broad swath of the country, transmission operators can rely less on fossil fuel power plants—read coal—as a backup when the wind dies, say, in South Dakota.
That will lower not only the price of renewable energy but utilities’ capital costs, which are, of course, passed on to their customers.
In California, for instance, utilities like PG&E spend billions on natural gas-fired power plants in order to provide emergency power for those few days each year when the grid is overloaded—hot summer afternoons when everyone cranks up their air conditioners at the same time.
“About 10 percent of our generation capacity sits idle for all but 50 hours a year,” Andrew Tang, a senior director at PG&E, tells me. “This industry is predicated on the premise that you always prepare for the worst day. It’s hugely expensive.”
Left unsaid in the NREL report is that the massive expansion of wind power needed to supply 20 to 30 percent of the nation’s electricity would be a green jobs machine.
At the beginning of 2009, according to the report, the U.S. had 25,000 megawatts of wind capacity installed and added another 4,500 megawatts during the first half of that year, despite the recession. To reach the 20 percent target, NREL estimates that 225,000 megawatts of new wind capacity must come online. Add another 105,000 megawatts to hit 30 percent.
The researchers offered different scenarios on how to achieve those goals, relying on varying mixes of wind from the Great Plains, the East and offshore. The 30 percent target relies heavily on developing wind farms off the East Coast, a capital-intensive undertaking that so far has run into huge political problems.
The NREL report, which was prepared by the consulting firm EnerNex, offers a highly technical discussion on how to reconfigure the grid to accommodate all that wind. But the bottom line is that between 8,352 and 11,102 miles of 800-volt direct current transmission lines, as well as thousands of miles of lower-voltage power lines, must be built. All in all, as many as 22,697 miles of new transmission lines would need to be installed, along with all the supporting infrastructure.
But the key takeaway is that NREL has concluded that there are no overriding technological hurdles or insurmountable financial obstacles to be overcome on the way to achieving the 20 percent target. It is basically a political problem—just imagine the NIMBY nightmare all those power lines would create.
Well, a political solution has been offered up by, of all people, Republican pollster Frank Luntz, who previously advised President George W. Bush on how to neutralize demands that the government take action on global warming.
Luntz has apparently undergone a climate change conversion. In a poll he released on Thursday, Luntz found that there is broad support among both Republicans and Democrats for climate change legislation when the issue is couched in terms of national security and energy independence.
“National security tops every other reason to support cap-and-trade,” Luntz concluded. “It’s about freeing the U.S. from foreign oil—and opening the door to greater security and prosperity.”
And as green energy advocates press to translate the NREL report into action, it’s worth remembering how a 20th century president managed to persuade Congress to fund a similarly ambitious infrastructure project, the interstate highway system.
Eisenhower did not argue that we needed to spend billions of dollars on a vast road system so we could develop the suburbs or drive coast-to-coast with ease. In the fearful fifties, he said building such a transportation network was all about creating the ability to move troops around the country in a national emergency. In other words, a national security argument secured what would become the driver of American prosperity in the coming decades.

Printing Lithium Batteries




For the present of course, researchers are discovering how far they can go with this.  We know that solar cells can be printed and doing the same with battery tech is an obvious fit.  This also suggests that folding can produce larger batteries. Again it is early days for the art itself.

 

The objective most attractive is to store solar energy without moving it at all.  That way we avoid unnecessary movement and storage and the related wastage.  Having the energy stored for example on the back of a solar panel is clearly most efficient and convenient.

 

That is the promise anyway.

 

I wonder if the ultra capacitor powder can be also printed.  This is much more promising and in time it will be more useful if it can be done.

 

As I described in my article on the reverse engineering of an UFO, several layers needed to be laminated together to produce the necessary working shell.  One layer been energy storage made good sense but was not necessary.

 

We are presently mastering the necessary arts.

 

 

Japanese Researchers Seeking to Print Out Li-polymer Battery

 

Jan 7, 2010 15:57Satoshi Okubo, Nikkei Electronics


A Japanese research group developed a lithium polymer battery that can be manufactured by printing technology.
The group is led by Advanced Materials Innovation Center (AMIC) of Mie Industry and Enterprise Support Center (MIESC), a Japan-based incorporated foundation.
The sheet-shaped battery is expected to be used with a flexible solar battery or display and to be attached to a curved surface. If the battery is integrated with a solar battery formed on a flexible substrate, it is possible to realize a sheet that can be used both as a power generator and a power storage, AMIC said.
Because the battery is made by using printing technology, it can be reduced in thickness, increased in area and laminated. Furthermore, when combined with a roll-to-roll production method, its costs can be reduced, AMIC said.
The lithium polymer battery was developed in a research project participated by MIESC, Toppan Printing Co Ltd, Shin-Kobe Electric Machinery Co Ltd, Kureha Elastomer Co Ltd, Kinsei Matec Co Ltd, Meisei Chemical Works Ltd, Mie University, Suzuka National College of Technology and Mie Prefecture Industrial Research Institute.
They prototyped two types of batteries. One has an output voltage of about 4V at a room temperature while the other has an output voltage of about 2V. The thickness of the battery is about 500μm, but the battery capacity was not disclosed. Its negative and positive electrodes were formed on a flexible substrate by using printing technology.
This time, the research group used a normal sheet-shaped flexible substrate but employed a printing technology that can be applied to roll-to-roll production, it said. When a roll-to-roll production method is used, the thickness of the flexible substrate can be reduced, enabling to manufacture thin batteries.
The group did not use a printing technology to package polymer electrolyte this time. It did not disclose the details of the polymer electrolyte or the negative or positive electrode materials.
The research project is a three-year project that will end in March 2011. In the final year, the research group plans to improve manufacturing technologies for commercial production, seek appropriate applications of the battery and set numerical targets such as of battery capacity.

S. Solomon et al., 10% decrease in water vapor in the stratosphere over the last 10 years has slowed Earth’s warming trends, researchers say

Ten percent decrease water vapor in the stratosphere slows Earth’s warming trends, researchers say





by Sindya N. Bhandoo, New York Times, January 28, 2010 
A decrease in water vapor concentrations in parts of the middle atmosphere has contributed to a slowing of Earth’s warming, researchers are reporting. The finding, they said, offers part of the explanation for a string of years with relatively stable global surface temperatures.

Despite the decrease in water vapor, the study’s authors said, the overall trend is still toward a warming climate, primarily caused by a buildup in emissions of carbon dioxide and other heat-trapping gases from human sources.

“This doesn’t alter the fundamental conclusion that the world has warmed and that most of that warming has to do with greenhouse gas emissions caused by man," said Susan Solomon, a climate scientist at the National Oceanic and Atmospheric Administration and the lead author of the report, which appears in the January 29, 2010, issue of the journal Science.

Water vapor, a potent heat-trapping gas, absorbs sunlight and re-emits heat into Earth’s atmosphere. Its concentrations in the stratosphere, the second of three layers in the atmosphere, appear to have decreased in the last 10 years, according to the study.

This has slowed the rate of Earth’s warming by about 25 percent, Dr. Solomon said.

“We use the 10-10-10 to describe it,” she said. “That is, a 10 percent change in water vapor, 10 miles above our head, over the past 10 years.”

The study also found that from 1980 to 2000, an increase in water vapor sped the rate of warming — the result of an increase in emissions of methane, another greenhouse gas, during the industrial period. Methane, when oxidized, produces water vapor. Why a decrease in water vapor has occurred in the last 10 years is still unknown.

Dr. Solomon emphasized that the study focused on the atmosphere’s middle layer, not to be confused with the troposphere, Earth’s first layer. It has been known for years that water vapor in the troposphere amplifies the effect of greenhouse gas emissions.

Some climate skeptics have claimed that a spate of years with relatively stable temperatures indicates that the threat of global warming has been overblown.

Last week, the National Aeronautics and Space Administration released figures indicating that the decade ending in 2009 was the warmest on record.

Link:  http://www.nytimes.com/2010/01/29/science/earth/29vapor.html

S. Solomon et al., Science, Contributions of stratospheric water vapor to decadal changes in the rate of global warming

Science, published online January 28, 2010; DOI: 10.1126/science.1182488

Contributions of stratospheric water vapor to decadal changes in the rate of global warming

Susan Solomon,1 Karen Rosenlof,1 Robert Portmann,1 John Daniel,1 Sean Davis,1,2 Todd Sanford,1,2 and Gian-Kasper Plattner3

1 NOAA Earth System Research Laboratory, Chemical Sciences Division, Boulder, CO, U.S.A.
2 Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, U.S.A.
3 Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland.  



Abstract

Stratospheric water vapor concentrations decreased by about 10% after the year 2000. Here, we show that this acted to slow the rate of increase in global surface temperature over 2000-2009 by about 25% compared to that which would have occurred due only to carbon dioxide and other greenhouse gases. More limited data suggest that stratospheric water vapor probably increased between 1980 and 2000, which would have enhanced the decadal rate of surface warming during the 1990s by about 30% compared to estimates neglecting this change. These findings show that stratospheric water vapor represents an important driver of decadal global surface climate change.

Link:  http://www.sciencemag.org/cgi/content/abstract/science.1182488

NASA (T. Markus et al.): Arctic 'Melt Season' Is Growing Longer, New Research Demonstrates

Arctic 'Melt Season' Is Growing Longer, New Research Demonstrates

by Kathryn Hansen, Goddard Space Flight Center, January 27, 2010

New NASA-led research shows that the melt season for Arctic sea ice has lengthened by an average of 20 days over the span of 28 years, or 6.4 days per decade. The finding stems from scientists' work to compile the first comprehensive record of melt onset and freeze-up dates -- the "melt season" -- for the entire Arctic.
Arctic melt imageLarger image
Arctic sea ice has been facing longer melt seasons, according to a new study. Credit: NASA/Thorsten Markus

The melt season begins each April when the sunless winter gives way to sunrise and spring, and water and air temperatures rise. By September, the sea ice shrinks to a minimum and begins refreezing, bringing the annual melt season to an end.

The longer melt season, described by Thorsten Markus of NASA's Goddard Space Flight Center in Greenbelt, Md., in the Journal of Geophysical Research -- Oceans, has implications for the future of Arctic sea ice. Open water that appears earlier in the season absorbs more heat from the sun throughout summer, further warming the water and promoting more melting.

"This feedback process has always been present, yet with more extensive open water this feedback becomes even stronger and further boosts ice loss," Markus said. "Melt is starting earlier, but the trend towards a later freeze-up is even stronger because of this feedback effect."
Researchers analyzed satellite data for 10 different Arctic regions and found trends in melt and freeze onset days as well as trends in melt season length. Larger image
Researchers analyzed satellite data for 10 different Arctic regions and found trends in melt and freeze onset days as well as trends in melt season length. Credit: NASA/Thorsten Markus 

To examine melt season length, Markus and colleagues used data from satellite passive microwave sensors, which can "see" indications of melt. The result is an accurate account of the melt seasons from 1979 to 2007.

"Given that the Arctic ocean is nearly twice the size of the continental United States, it would be impossible to track change like this without long-term satellite records," said Thomas Wagner, NASA's cryosphere program scientist at NASA Headquarters, Washington.

Analyzing melt-season trends for 10 different Arctic regions, the research team discovered that melt season lengthened the most -- more than 10 days per decade -- in Hudson Bay, the East Greenland Sea, the Laptev and East Siberian Seas, and the Chukchi and Beaufort Seas. Some of that change is due to melt onset occurring about three days earlier per decade in some areas. Earlier melt means more heat can be absorbed by the open water, promoting more melting and later freeze-up dates -- more than eight days per decade later in some areas. Only the Sea of Okhotsk turned up a shorter melt season. The reasons for the regional differences are currently being investigated.

"The onset of melting and melt season length are important variables for understanding the Arctic climate system," Markus added. "Given the recent large losses of the Arctic summer ice cover, it has become critical to investigate the causes of the decline and the consequences of its continued decline."

The lengthened melt season could impact more than just the Arctic ice and ocean. According to Markus, "marine ecosystems are very sensitive to changes in melt onset and freeze-up dates."

Between 1979 and 2007, Arctic sea ice has begun melting an average of 2.8 days per decade earlier in the spring, and has begun refreezing an average of 3.7 days per decade later in the autumn.Larger image

Between 1979 and 2007, Arctic sea ice has begun melting (left map) an average of 2.8 days per decade earlier in the spring, and has begun re-freezing (center map) an average of 3.7 days per decade later in the autumn. Altogether, the length of the Arctic melt season (right map) has increased by about 20 days over the past 30 years. These maps are based on satellite observations of microwave energy radiated from the surface of sea ice. Credit: NASA images by Robert Simmon, based on data from Jeffrey Miller and Thorsten Markus.

"Changes in the Arctic sea ice cover may have profound effects on North America’s climate," said Wagner.

"Studies like this one show us how ice responds to variations in the ocean and atmosphere and improve the predictive models that will help us plan for climate change."

Link:  http://www.nasa.gov/topics/earth/features/longer-melt-season.html