![]() ![]() "A big advantage was being able to interface satellite data with surface radiometric data, with satellite water vapor and ozone abundance data," Cess said. For the period studied, 1985 to 1988, they found no inconsistencies between the modeled and the observed clear-sky shortwave radiation measured at the surface. "We found excellent agreement between the models and the observations," Cess said. They also used aerosol optical depths from NOAA's National Environmental Satellite Data Service (NESDIS) as determined from Advanced Very High Resolution Radiometer (AVHHR) measurements. To account for atmospheric water vapor variability and atmospheric ozone, Cess and Jing used collocated measurements from the Television Infrared Observation Satellite (TIROS) using the Operational Vertical Sounder (TOVS). The other model, the National Center for Atmospheric Research Community Climate Model (CCM3), is a stand-alone model that computes surface insolation independently of satellite measurements. ![]() ![]() algorithm, determines surface insolation by converting satellite top of the atmosphere shortwave radiation measurements to surface insolation. Then, he and Jing then compared the clear-sky data with two atmospheric shortwave radiation models to see if there was any disagreement. "This was by far the most comprehensive test of clear-sky shortwave radiation models that has ever been done as far as comparing the data," Cess said. The radiometric scanner measurements from ERBS describe the amount of solar radiation reflected back to space from 1985 to 1988.īy collocating these satellite data with the surface measurements, the researchers created a clear-sky data set. The satellite measurements of shortwave radiation reflected at the top of the atmosphere were made from the Earth Radiation Budget Satellite (ERBS) as part of the Langley Earth Radiation Budget Experiment (ERBE). "That eliminated about 98 percent of our data, but since we were data-rich, that was not a real problem," Cess said. To focus their study on clear-sky days, Cess and Jing used satellite and surface-based measurements to remove data with clouds or forest fire smoke from nearby boreal forests. Made at 24 stations in southern Canada, the measurements consist of hourly surface insolation means collected over a four-year period from 1985 to 1988. Surface insolation measurements were obtained from the Canadian Atmospheric Environment Service. They composed a data set of clear-sky days using measurements of solar radiation at the Earth's surface (insolation) and satellite measurements of solar radiation at the top of the atmosphere. candidate at SUNY, designed an experiment to test the accuracy of clear-sky shortwave radiation models using an extensive data set. Since many of the studies used short-term data sets, Cess and Xiaodu Jing, a Ph.D. But, several other studies claim there are problems," said Robert Cess an atmospheric scientist at the State University of New York at Stony Brook. "A number of studies have not found any problem with our ability to model clear-sky shortwave radiation in the atmosphere. Scientists have created models to describe solar, or shortwave, radiation at the Earth's surface, but recent studies have yielded conflicting opinions of how accurately the models portray clear days. (Image courtesy of STS-31)įor more information, visit the Langley Atmospheric Sciences Data Center. (Animation by Susan Gonnelli, NASA TV)Įarth observation taken aboard the Space Shuttle Discovery, Orbiter Vehicle (OV) 103, during late afternoon shows the Andes Mountains and features sun glare, heavy cloud illumination, and a sunglint on the Pacific Ocean. Subsequently, this energy is emitted as longwave radiation, much of which gets trapped in the Earth's atmosphere by clouds and greenhouse gases. Some sunlight is reflected by clouds or the surface back up into space, while some is absorbed and then stored as heat. The CERES sensors are designed to help scientists understand the fate of sunlight after it enters the Earth's environment. Understanding the physical processes behind the solar radiation reflecting from Earth's surface on clear days, however, is far more difficult. At the time of publication, it represented the best available science.Īnyone who is outdoors on a clear day and feels the warmth of the sun can easily understand that the sun radiates energy to the Earth's surface. This page contains archived content and is no longer being updated. ![]()
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