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On the Record

 

Newsroom | News Releases | Press Clips | Office of Government Affairs | For Journalists

UCAR President's Corner
Richard Anthes, president of UCAR and of the American Meteorological Society, writes periodically on the science and policy implications of weather and climate issues.

After the Nobel Prize, what to do—and not do? (Fall 2007)
The global trajectory, take two (Summer 2007)
Strange bedfellows and holy alliances (Fall 2006)
Conservation as a global and local imperative (Winter 2005-06)
Hurricane Katrina: An act of God? (Fall 2005)
Earth exploration for science and society (Spring 2005)

As a vital component of our mission to make science useful to society, our researchers publish in peer-reviewed journals, participate in news conferences and interviews, and respond to requests by Congress for information about their findings.

While professional journalists strive for accuracy in their reporting, the limited space allotted to news stories often results in statements appearing out of context. Such isolated comments may sometimes skew the author's or speaker's intention.

On the Record presents source material from NCAR, UCAR, and UOP researchers to provide context and accuracy.

 

Topics

Politics, science and the question of global warming and hurricane intensity (August 2006)

The effect of the Kyoto Protocol on global warming (Spring 2006)

Hurricanes and global warming (Winter 2004, updated June 2006)

Politics, science and the question of global warming and hurricane intensity

Greg Holland, Senior Scientist and
Director of the Mesoscale and Microscale Meteorology Division, NCAR
August 2006

Published article

Mixing Politics and Science in Testing a Hurricane Hypothesis

Curry, J.A., Webster, P.J., and Holland, G.J. (2006), "Mixing Politics and Science in Testing the Hypothesis that Greenhouse Warming Is Causing a Global Increase in Hurricane Intensity," Bulletin of the American Meteorological Society, August, pp. 1025–1037.

Abstract

The 2005 Atlantic hurricane season was the most active and costly season on record. Recent publications linking an increase in hurricane intensity to increasing tropical sea surface temperatures have fueled the debate on whether or not global warming is causing an increase in hurricane intensity. Because of the substantial implications of the hurricane–global warming issue for society and the immediate policy relevance associated with decision making related to Hurricane Katrina, attacks and rebuttals related to this research are being made in the media and on the World Wide Web without the rigor or accountability expected of scientific discourse. In this paper, we aim to promote a balanced and thoughtful examination of this subject by

• clarifying the debate surrounding the subject as to whether or not global warming is causing an increase in global hurricane intensity,

• illustrating a methodology of hypothesis testing to address multiple criticisms of a complex hypothesis that involves a causal chain, and

• providing a case study of the impact of politics, the media, and the World Wide Web on the scientific process.


The full article is available for download at no charge as a PDF by selecting "Print Version" on the article's Web page on the Bulletin of the American Meteorological Society site.

Related sites on the World Wide Web

News Release: Hurricanes Are Getting Stronger, Study Says (September 15, 2005)

Backgrounder: Hurricanes, Typhoons, and Cyclones

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Greg Holland

Greg Holland
(Photo by Carlye Calvin.)

 

 

The effect of the Kyoto Protocol on global warming

Tom M.L. Wigley, Senior Scientist, NCAR
Spring 2006

Published articles

Summary

Tom Wigley in 1998 reported research showing that adherence to the Kyoto Protocol alone, without subsequent action, would have a minimal impact on global warming.

Wigley concluded in the article, published in Geophysical Research Letters, "This does not mean that the actions implied by the Protocol are unnecessary." He called the protocol an important first step while pointing out that much more must be done after Kyoto to reduce future global warming by a significant amount.

Wigley used computer modeling to test several emissions scenarios for the "Annex B" countries—the industrialized and nearly industrialized countries called upon to reduce greenhouse gas emissions in the protocol. Each scenario was played out through 2010 (the midpoint of the Kyoto commitment period of 2008–2012) and then extended to the end of the century.

The first scenario looked at what would happen if, after the protocol expires, the Annex B countries continued to abide by Kyoto's limits but did not make any new commitments to further cut emissions for the rest of the century.

This "constant compliance" scenario would shave 0.11 to 0.21 degrees Celsius (0.20–0.38 degrees Fahrenheit) off global average temperatures by 2100. Stated another way, instead of heating up by 2.5°C (4.5°F), a midpoint in the range of projections of global warming, Earth would warm approximately 6% less.

For comparison, the study also examined a "business as usual" or "no climate policy" case. The starting point was IS92a, an emissions scenario included in the 2001 report of the Intergovernmental Panel on Climate Change, that incorporates a slight tapering off in emissions later this century due to global economic and social activities unrelated to climate change.

Wigley concluded that the impact on projected temperature increases, with all countries doing only what is required under Kyoto and then continuing with business as usual, would be a scant 0.06 to 0.11°C (0.11 to 0.20°F) shaved off the total warming, roughly a 3% reduction.

He also considered a third scenario in which the Annex B countries continue to reduce their emissions after the Kyoto period by 1% per year (a scenario that, like the other two scenarios, assumes continued growth of emissions in developing countries at a business-as-usual rate). In this case, the warming reduction by 2100 would be some 14%.

In a 2005 article in Science, Wigley found that Earth is already warming due to human actions. Averting further warming will require a global reduction in human-generated greenhouse gases by all nations, developed and developing, to substantially below present levels.

Published Article: The Kyoto Protocol

Wigley, T.M.L. (1998), "The Kyoto Protocol: CO2, CH4 and climate implications," Geophysical Research Letters, vol. 25, pp. 2285–88.

Abstract

Kyoto Protocol implications for CO2, temperature and sea level are examined. Three scenarios for post-Kyoto emissions reductions are considered. In all cases, the long-term consequences are small. The limitations specified under the Protocol are interpreted in terms of both CO2 and CH4 emissions reductions and a new emissions comparison index, the Forcing Equivalence Index (FEI), is introduced. The use of GWPs [Global Warming Potential values] to assess CO2-equivalence is assessed.

Excerpts from the conclusion, with annotations

Three Kyoto Protocol cases have been examined. These extend the Protocol beyond [2010]1 by assuming no further reductions in Annex B emissions;2 constant Annex B emissions; or a decline in Annex B emissions at 1% compound per year.3

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Large additional emissions reductions are required at some future date (certainly earlier than 2040) if concentration stabilization is to be achieved at 550 ppmv [parts per million by volume] or lower.

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Finally, reductions in temperature and sea level rise under the Protocol and the extensions considered here are relatively small, but nonetheless important as a first step towards stabilizing the climate system. (emphasis added)

Related Article: The Climate Change Commitment

Wigley, T.M.L. (2005), "The Climate Change Commitment," Science, vol. 307, pp. 1766–69.

Abstract

Even if atmospheric composition were fixed today, global-mean temperature and sea level rise would continue due to oceanic thermal inertia. These constant-composition (CC) commitments and their uncertainties are quantified. Constant-emissions (CE) commitments are also considered. The CC warming commitment could exceed 1°C. The CE warming commitment is 2° to 6°C by the year 2400. For sea level rise, the CC commitment is 10 centimeters per century (extreme range approximately 1 to 30 centimeters per century) and the CE commitment is 25 centimeters per century (7 to 50 centimeters per century). Avoiding these changes requires, eventually, a reduction in emissions to substantially below present levels. For sea level rise, a substantial long-term commitment may be impossible to avoid.

Excerpt from the conclusion

The CE results reinforce the common knowledge that, in order to stabilize global-mean temperatures, we eventually need to reduce emissions of greenhouse gases to well below present levels.4 The CC results are potentially more alarming, because they are based on a future scenario that is clearly impossible to achieve and so represent an extreme lower bound to climate change over the next few centuries. For temperature, they show that the inertia of the climate system alone will guarantee continued warming and that this warming may eventually exceed 1°C. For sea level, a continued rise of about 10 cm/century for many centuries is the best estimate. Although such a slow rate may allow many coastal communities to adapt, profound long-term impacts on low-lying island communities and on vulnerable ecosystems (such as coral reefs) seem inevitable. (emphasis added)

 Related sites on the World Wide Web 

For background

UN Framework Convention on Climate Change (three languages available)

         Relationship of Kyoto Protocol to UN Framework Convention

                  Text of the Kyoto Protocol (six languages available)

UN Environment Programme: Climate Change

Excerpts from interview with Tom Wigley, Earth & Sky Radio Series

For research

MAGICC and SCENGEN Computer Models

These coupled, interactive software suites were used in the 2001 IPCC Third Assessment Report and by Wigley for the 1998 article. The software allows experimenters to investigate future climate change and its uncertainties at both the global-mean and regional levels.

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Tom Wigley

Tom Wigley
(Photo by Carlye Calvin.)

 

 

Hurricanes and global warming

Kevin Trenberth, head of the Climate Analysis Section, NCAR
Winter 2004, updated June 2006

Published articles and news conference

Published article: Atlantic hurricanes and natural variability in 2005

Trenberth, K. E., and D. J. Shea (2006), "Atlantic hurricanes and natural variability in 2005," Geophysical Research Letters, 27 June, 33, L12704.

News Release: Global Warming Surpassed Natural Cycles in Fueling 2005 Hurricane Season, NCAR Scientists Conclude (June 22, 2006)

Perspective article: Uncertainty in Hurricanes and Global Warming

Trenberth, Kevin (2005), "Climate: Uncertainty in Hurricanes and Global Warming, Science, 17 June, vol. 308, no. 5729, pp. 1753–1754.

News Release: Hurricanes To Intensify as Earth Warms (June 16, 2005)

News conference, October 21, 2004

Center for Health and Global Environment
Harvard Medical School, Cambridge, Massachusetts

Written statement distributed at news conference

Human activities are changing the composition of the atmosphere and global warming is happening as a result. Global warming is manifested in unexpected ways. Sea level has risen 1.25 inches in the past 10 years as a result of warming of the oceans and glacier melting. The environment in which hurricanes form is changing. The result was a hurricane in late March 2004 in the South Atlantic, off the coast of Brazil: the first and only such hurricane in that region. Several factors go into forming hurricanes and where they track. But the evidence strongly suggests more intense storms and risk of greater flooding events, so that the North Atlantic hurricane season of 2004 may well be a harbinger of the future.

Opening statement excerpts

Global sea level has risen about an inch and a quarter in the past 10 years. This is good information—the first time we've had global information from satellites using a process called altimetry. Now most of this rise in sea level is due to expansion of the ocean as it warms up, and maybe 20 to 35% is from melting of glaciers. So the sea surface temperature is rising globally. It's been about 1 degree Fahrenheit over the 20th century and it's risen in particular in recent times in the Atlantic and other regions, of course, that affect hurricanes.

----------

And of course this is the fuel for the hurricanes and it also means that the hurricanes end up dropping a lot more precipitation and rainfall as a result. And so the environment in which these hurricanes form is changing and it's changing in ways that provide more fuel for them through the water vapor and the changes in sea surface temperature. 

----------

What we can say is that the high sea surface temperatures of water vapor make for more intense storms, and so this is consistent with the evidence that we're seeing. And so this is the main link with global warming that we can establish at the current time.

And so this is supported also by the modeling evidence and the theoretical evidence. There was a certain amount of activity regarding a paper that came out recently by a group headed by Tom Knutson at the Geophysical Fluid Dynamics Laboratorylaboratory for those of you, if I say it in American. And that supports the idea that indeed hurricanes are apt to become more intense in the future. So a key consequence, I think, is certainly perhaps increased damage from winds, but I think the biggest consequence is likely to be more heavy rains and flooding.

Other participants

Transcript of news conference

Full transcript pdf PDF version

Streaming audio from the Center for Health and Global Environment

Related sites on the World Wide Web

Backgrounder: Hurricanes, Typhoons, and Cyclones

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Files with the PDF symbol require free Adobe Reader Software

Kevin Trenberth

Kevin Trenberth
(Photo by Carlye Calvin.)

This document can be found at
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