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Satellite-only latent heat flux estimation

机译:仅卫星潜热通量估算

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Here we present a new method for recovering global latent heat flux (XE) using satellite sounding in conjunction with visible and infra-red geophysical products, from the AIRS (Atmospheric Infrared Sounder) and MODIS (Moderate Resolution Imaging Spectroradiometer) platforms at 1°×1° spatial domain. This method focuses on specifying the day-night net radiation, which is then used in a dynamic surface energy balance framework with day-night land surface temperature to directly retrieve net available energy. The evaporative fraction was estimated from the water vapour and temperature profile information in a Bowen ratio framework. Evaluation of available energy and latent heat flux against 30 terrestrial flux tower sites revealed a pooled root mean square deviation (RMSD) of 98, 72 and 79 Wm~(-2) for net radiation, net available energy, and latent heat flux between satellite and tower, respectively. The results show particular promise of this approach for latent heat flux retrieval under warm, moist conditions, but weaknesses under arid or semi- arid conditions subject to high radiative loads.
机译:在这里,我们介绍了一种新的方法,该方法利用卫星测深技术结合可见光和红外地球物理产品,从AIRS(大气红外测深仪)和MODIS(中分辨率成像光谱仪)平台以1°×的速度回收全球潜热通量(XE) 1°空间域。该方法着重于指定昼夜净辐射,然后将其用于具有昼夜陆地表面温度的动态地表能量平衡框架中,以直接获取净可用能量。根据鲍文比率框架中的水蒸气和温度分布信息估算蒸发分数。对30个地面通量塔站点的可用能量和潜热通量的评估显示,卫星之间的净辐射,净可用能量和潜热通量的集合均方根偏差(RMSD)为98、72和79 Wm〜(-2)。和塔。结果表明,该方法在温暖潮湿的条件下用于潜热通量的恢复特别有希望,但是在干旱或半干旱条件下承受高辐射负荷的情况下,其弱点。

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