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首页> 外文期刊>Geophysical Research Letters >Height distribution between cloud and aerosol layers from the GLAS spaceborne lidar in the Indian Ocean region
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Height distribution between cloud and aerosol layers from the GLAS spaceborne lidar in the Indian Ocean region

机译:印度洋地区GLAS星载激光雷达的云层和气溶胶层之间的高度分布

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The Geoscience Laser Altimeter System (GLAS), a nadir pointing lidar on the Ice Cloud and land Elevation Satellite (ICESat) launched in 2003, now provides important new global measurements of the relationship between the height distribution of cloud and aerosol layers. GLAS data have the capability to detect, locate, and distinguish between cloud and aerosol layers in the atmosphere up to 40 km altitude. The data product algorithm tests the product of the maximum attenuated backscatter coefficient b'(r) and the vertical gradient of b'(r) within a layer against a predetermined threshold. An initial case result for the critical Indian Ocean region is presented. From the results the relative height distribution between collocated aerosol and cloud shows extensive regions where cloud formation is well within dense aerosol scattering layers at the surface.
机译:地球科学激光测高仪系统(GLAS)是2003年发射的位于冰云和陆地高程卫星(ICESat)上的最低点激光雷达,现在提供了重要的全球新测量数据,用于测量云层和气溶胶层之间的高度关系。 GLAS数据可以检测,定位和区分高达40 km的大气层中的云层和气溶胶层。数据乘积算法针对预定阈值测试最大衰减后向散射系数b'(r)与一层内b'(r)的垂直梯度的乘积。介绍了关键印度洋地区的初步案例结果。根据结果​​,并列的气溶胶和云之间的相对高度分布显示出广泛的区域,在这些区域中,云的形成很好地位于表面的密集气溶胶散射层内。

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