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On the utility of land surface models for agricultural drought monitoring

机译:地表模型在农业干旱监测中的应用

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The lagged rank cross-correlation between model-derived root-zone soil moisture estimates and remotely sensed vegetation indices(VI) is examined between January 2000 and December 2010 to quantify the skill of various soil moisture models for agriculturaldrought monitoring. Examined modeling strategies range from a simple antecedent precipitation index to the application of modernland surface models (LSMs) based on complex water and energy balance formulations. A quasi-global evaluation of lagged VI/soil moisturecross-correlation suggests, when globally averaged across the entire annual cycle, soil moisture estimates obtained fromcomplex LSMs provide little added skill (< 5% in relative terms) in anticipating variations in vegetation condition relative to asimplified water accounting procedure based solely on observed precipitation. However, larger amounts of added skill (5–15% in relativeterms) can be identified when focusing exclusively on the extra-tropical growing season and/or utilizing soil moisture values acquired byaveraging across a multi-model ensemble.
机译:在2000年1月至2010年12月之间,研究了模型得出的根区土壤水分估算值与遥感植被指数(VI)之间的滞后秩相关性,以量化各种土壤水分模型用于农业干旱监测的技能。检验的建模策略范围从简单的前期降水指数到基于复杂水和能量平衡公式的现代地表模型(LSM)的应用。滞后VI /土壤水分互相关的准全局评估表明,当在整个年周期中对全球平均水平进行平均时,从复杂LSM获得的土壤水分估算值在预测植被状况相对于植被状况变化方面几乎没有增加技能(相对值小于5%)。仅基于观测到的降水量的简化水核算程序。但是,当仅专注于热带地区的生长季节和/或利用通过对多个模型集合求平均值而获得的土壤湿度值时,可以识别出大量的附加技能(相对而言为5-15%)。

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