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A Sea-Surface Radiation Data Set for Climate Applications in the Tropical Western Pacific and South China Sea

机译:用于热带西太平洋和南海气候应用的海面辐射数据集

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摘要

The sea-surface shortwave and longwave radiative fluxes have been retrieved from the radiances measured by Japan's Geostationary Meteorological Satellite 5. The surface radiation data set covers the domain 40S-40N and 90E-170W. The temporal resolution is 1 day, and the spatial resolution is 0.5 deg x 0.5 deg latitude-longitude. The retrieved surface radiation have been validated with the radiometric measurements at the Atmospheric Radiation Measuring (ARM) site on Manus island in the equatorial western Pacific for a period of 15 months. It has also been validated with the measurements at the radiation site on Dungsha island in the South China Sea during the South China Sea Monsoon Experiment (SCSMEX) Intensive Observing Period (May and June 1998). The data set is used to study the effect of El Nino and East Asian Summer monsoon on the heating of the ocean in the tropical western Pacific and the South China Sea. Interannual variations of clouds associated with El Nino and the East Asian Summer monsoon have a large impact on the radiative heating of the ocean. It has been found that the magnitude of the interannual variation of the seasonal mean surface radiative heating exceeds 40 W/sq m over large areas. Together with the Clouds and the Earth's Radiant Energy System (CERES) shortwave fluxes at top of the atmosphere and the radiative transfer calculations of clear-sky fluxes, this surface radiation data set is also used to study the impact of clouds on the solar heating of the atmosphere. It is found that clouds enhance the atmospheric solar heating by approx. 20 W/sq m in the tropical western Pacific and the South China Sea. This result is important for evaluating the accuracy of solar flux calculations in clear and cloudy atmospheres.
机译:海面短波和长波辐射通量已经从日本对地静止气象卫星5测得的辐射中获得。表面辐射数据集覆盖了40S-40N和90E-170W域。时间分辨率为1天,空间分辨率为0.5度x 0.5度经度。在赤道西太平洋马努斯岛的大气辐射测量(ARM)站点进行的辐射测量已验证了检索到的表面辐射,为期15个月。在南海季风实验(SCSMEX)密集观测期(1998年5月和1998年6月)在南海东沙岛辐射站点的测量结果中也进行了验证。该数据集用于研究厄尔尼诺现象和东亚夏季风对热带西太平洋和南中国海海洋加热的影响。与厄尔尼诺现象和东亚夏季风有关的云的年际变化对海洋的辐射加热有很大的影响。已经发现,在大面积上,季节性平均表面辐射加热的年际变化幅度超过40 W / sq m。结合大气层顶部的云和地球辐射能系统(CERES)短波通量以及晴空通量的辐射传递计算,该表面辐射数据集还用于研究云对太阳辐射的影响。气氛。据发现,云层将大气中的太阳热量提高了约20%。热带西太平洋和南中国海为20 W / sq m。该结果对于评估晴天和阴天大气中太阳通量计算的准确性非常重要。

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