------------------------------ Date: Thu, 4 Mar 1999 13:27:43 EST From: CSubject: GL: UCAR News-Indian Ocean ----------------------------Original message---------------------------- 1999-6 March 4, 1999 Contact: Anatta UCAR Communications Telephone: 303-497-8604 E-mail: anatta@ucar.edu NCAR Scientists, Aircraft, Instruments Head to Indian Ocean for Climate Change Experiment; UCAR Directs Operations BOULDER--How much do sulfate aerosols--a form of pollution--cool the climate? That's one of the most pressing questions for understanding global climate change. To help find the answer, the National Center for Atmospheric Research (NCAR) has sent researchers, instruments, and a C- 130 research aircraft owned by the National Science Foundation (NSF) to the $25-million Indian Ocean Experiment (INDOEX). NSF is NCAR's primary sponsor and a partial sponsor of INDOEX. INDOEX is based in the Republic of the Maldives, an archipelago southwest of India's southern tip. There, NCAR scientists are working alongside more than 70 researchers from a dozen nations to observe the tropical oceans and atmosphere from January to April. The University Corporation for Atmospheric Research, NCAR's parent organization, is overseeing operations from its support office for logistics and data management, headed by Richard Dirks of the UCAR Office of Programs. The highly instrumented C-130 aircraft will be based through March 27 at Mal=E9 airport, which occupies its own island in the archipelago. According to NCAR's Jeffrey Kiehl, a principal investigator for INDOEX, "In the future, pollution in the tropics will increase, so we'd better understand it now. The chemistry in the tropics is severely undersampled." The Indian subcontinent and surrounding nations are rich sources for many kinds of aerosols, including those produced from industrial and auto emissions, biomass burning, and soil dust. With Asia's population rising at a dramatic rate, the amount of sulfur dioxide released into the atmosphere is expected to increase. Sulfur dioxide is converted into sulfate aerosol in the atmosphere. The ability of sulfate aerosols to reflect the sun's radiation may be one reason that increasing greenhouse gases have not warmed the earth as much as some climate models have predicted. Sulfates also contribute to local pollution and acid rain. Kiehl helped design INDOEX to ensure that the project collects the data needed to advance global climate modeling. Some physical and chemical processes in the earth system are so complicated that modelers cannot simulate each detailed step. "With INDOEX data, we can actually test the way we treat aerosols in computer models against observations." The observation region is downwind of the Indian subcontinent during the spring and extends into the pristine Southern Hemisphere. With a forecast of pleasant weather--calm, with little rain--the investigators should be able to sample both polluted and clean air in clouds and clear sky. "It's a natural laboratory for studying direct and indirect effects of aerosols," says NCAR's Andrew Heymsfield, another INDOEX researcher. The direct effect of aerosols is the scattering that occurs when solar radiation bounces off particles in clear air. The indirect effects have to do with sulfates' interactions with clouds. Globally, aerosols are an important source of nuclei around which cloud droplets can condense, and in the tropics they are the chief source. The more cloud condensation nuclei, the brighter the cloud, that is, the more solar radiation reflected back into space before it reaches the earth's surface. This radiative effect is what makes clouds, and the indirect effects of aerosols, so important in climate change research. However, indirect effects are now so little understood that estimates in global climate models vary from almost no effect to more than enough cooling to offset global warming resulting from greenhouse gas increases. "A host of changes in cloud physical and microphysical properties are lumped under the term 'indirect effects,' " says NCAR scientist William Collins. Collins is using satellite measurements to estimate optical depths in clouds and the sizes of aerosol droplets. The Maldives archipelago runs in a north-south line from about 500 miles southwest of the tip of the Indian subcontinent to the equator. The personnel and observing systems are spread across several islands, with all transport by boat. Resources include five aircraft, two research ships, and a host of ground-based systems. Satellite data will be used for real-time weather forecasting, monitoring the motion of pollutants, and measuring radiation at different altitudes. This combination of ground, airborne, and satellite data is expected to vastly increase scientists' understanding of the nature and scope of aerosols' indirect effects. Heymsfield and NCAR colleague Gregory McFarquhar are studying some of the cloud microphysical changes using a scanning aerosol backscatter lidar, developed at NCAR and mounted on the C-130. From the aircraft the lidar can characterize cloud top and bottom. The scientists will observe the optical depth of clouds in both clear and cloudy aerosol-laden skies. "The government of the Maldives has been extraordinarily cooperative and accommodating," says Dirks. "They're deeply concerned with climate change research." The Maldives islands are vulnerable to rising sea levels due to climate change. INDOEX is coordinated by the Center for Clouds, Chemistry and Climate (C4), an NSF Science and Technology Center at the Scripps Institution of Oceanography. Paul J. Crutzen, director of the Max Planck Institute for Chemistry and a 1995 Nobel Laureate in Chemistry, and C4 director V. Ramanathan will serve as INDOEX chief scientists. -The End- Note to Editors: Please contact Anatta (information above) to interview INDOEX participants or to fly on the C-130 aircraft. For more information, see the INDOEX Web site: http://www-indoex.ucsd.edu=tm.htmltmlmd/index.htmll / ------------------------------ Date: Thu, 4 Mar 1999 14:09:37 EST From: C Subject: GL: 1990's Warmest Decade of Millenium, Climate Researchers Report 3 MARCH 1999 Contact: Harvey Leifert hleifert@agu.org 202-939-3212 American Geophysical Union 1998 Was Warmest Year Of Millenium, Climate Researchers Report WASHINGTON, D.C. -- Researchers at the Universities of Massachusetts and Arizona who study global warming have released a report strongly suggesting that the 1990s were the warmest decade of the millennium, with 1998 the warmest year so far. Researchers have also found that the warming in the 20th century counters a 1,000-year-long cooling trend. The study, by Michael Mann and Raymond Bradley of the University of Massachusetts and Malcolm Hughes of the University of Arizona, appears in the March 15 issue of Geophysical Research Letters, published by the American Geophysical Union. The research was supported by the U.S. Department of Energy and the National Science Foundation. "Temperatures in the latter half of the 20th century were unprecedented,"said Bradley. The study involved a close examination of natural archives, such as tree rings and ice cores, which record climate variations each year. These natural archives are called "proxy indicators" by scientists and allow researchers to consider the short instrumental record of climate in a longer-term perspective. Using proxy information gathered by scientists around the world during the past few decades, the team used sophisticated computer analysis and statistics to reconstruct yearly temperatures and their statistical uncertainties, going back to the year AD 1000. Specifically, they relied on three sets of 1,000-year-long tree-ring records from North America, plus tree rings from northern Scandinavia, northern Russia, Tasmania, Argentina, Morocco, and France. Additionally, they studied ice cores from Greenland and the Andes mountains. "As you go back farther in time, the data become sketchier. One can't quite pin things down as well," noted Mann, "but, our results do reveal that significant changes have occurred, and temperatures in the latter 20th century have been exceptionally warm compared to the preceding 900 years. Though substantial uncertainties exist in the estimates, these are nonetheless startling revelations." Research published by the same team last year reconstructed yearly global surface temperature patterns going back 600 years. That study and the current report both relied on natural archives, and determined that human-induced greenhouse gases were a major factor in 20th century global warming. The year 1998 was found to be the warmest year on record in separate reports released by National Aeronautics and Space Administration (NASA) and the National Oceanic and Atmospheric Administration (NOAA). The reports were issued in January 1999, reviewing climatic conditions for the previous year, but the studies examined records only going back 120 years. The new study puts the conclusions from NASA and NOAA in a much longer perspective. According to the researchers, the 1,000-year reconstruction reveals that temperatures dropped an average of 0.02 degrees Celsius per century prior to the 20th century. This trend is consistent with the "astronomical theory" of climate change, which considers the effects of long-term changes in the nature of the Earth's orbit relative to the Sun, which influence the distribution of solar energy at the Earth's surface over many millennia. "If temperatures change slowly, society and the environment have time to adjust," said Mann. "The slow, moderate, long-term cooling trend that we found makes the abrupt warming of the late 20th century even more dramatic. The cooling trend of over 900 years was dramatically reversed in less than a century. The abruptness of the recent warming is key, and it is a potential cause for concern." The latest reconstruction supports earlier theories that temperatures in medieval times were relatively warm, but "even the warmer intervals in the reconstruction pale in comparison with mid-to-late 20th-century temperatures," said Hughes. ### http://www.eurekalert.org/releases/agu-nww030399.html Notes: University of Massachusetts contact: Elizabeth Luciano -- 413-545-2989 -- luciano@journ.umass.edu University of Arizona contact: Lori Stiles -- 520-626-4402 -- lstiles@u.arizona.edu For further information on the science in this paper, journalists may contact: Raymond Bradley at 413-545-2120, rbradley@geo.umass.edu (through March 5). Michael Mann at 413-545-9573, mann@geo.umass.edu (from March 4). Malcolm Hughes at 520-621-2191, mhughes@ltrr.arizona.edu . An on-line press kit, including photos of the researchers, graphics, and a link to the report, is available at: http://www.umass.edu/newsoffice/press/99/0303climate.html . The images will be at: http://www.umass.edu/newsoffice/press/99/0303climateimages.html . FAQ will be at: http://www.umass.edu/newsoffice/press/99/0303climatefaq.htmltml . Journalists and science public information officers (only) may also obtain copies of the Mann et. al. paper upon request to Daryl Tate dtate@agu.org . Please include your fax number.