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首页> 外文期刊>Advances in Water Resources >Requirements of a global near-surface soil moisture satellite mission: accuracy, repeat time, and spatial resolution
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Requirements of a global near-surface soil moisture satellite mission: accuracy, repeat time, and spatial resolution

机译:全球近地土壤湿度卫星任务的要求:准确性,重复时间和空间分辨率

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摘要

Soil moisture satellite mission accuracy, repeat time and spatial resolution requirements are addressed through a numerical twin data assimilation study. Simulated soil moisture profile retrievals were made by assimilating near-surface soil moisture observations with various accuracy (0, 1, 2, 3, 4, 5 and 10%v/v standard deviation) repeat time (1, 2, 3, 5, 10, 15, 20 and 30 days), and spatial resolution (0.5, 6, 12 18, 30, 60 and 120 arc-min). This study found that near-surface soil moisture observation error must be less than the model forecast error required for a specific application when used as data assimilation input, else slight model forecast degradation may result. It also found that near-surface soil moisture observations must have an accuracy better than 5%v/v to positively impact soil moisture forecasts, and that daily near-surface soil moisture observations achieved the best soil moisture and evapotranspiration forecasts for the repeat times assessed, with 1-5 day repeat times having the greatest impact. Near-surface soil moisture observations with a spatial resolution finer than the land surface model resolution (~30 arc-min) produced the best results, with spatial resolutions coarser than the model resolution yielding only a slight degradation. Observations at half the land surface model spatial resolution were found to be appropriate for our application. Moreover, it was found that satisfying the spatial resolution and accuracy requirements was much more important than repeat time.
机译:通过数值孪生数据同化研究解决了土壤湿度卫星任务的准确性,重复时间和空间分辨率的要求。通过以各种精度(0、1、2、3、4、5和10%v / v标准偏差)重复时间(1、2、3、5、3)吸收近地表土壤水分观测值,进行了模拟的土壤水分剖面反演。 10、15、20和30天)和空间分辨率(0.5、6、12、18、30、60和120 arc-min)。这项研究发现,当用作数据同化输入时,近地表土壤湿度观测误差必须小于特定应用所需的模型预测误差,否则可能会导致模型预测轻微退化。研究还发现,近地表土壤水分观测值的准确度必须高于5%v / v才能对土壤水分预测产生积极影响,并且每天的近地表土壤水分观测值在评估的重复时间上均获得了最佳的土壤水分和蒸散量预测,重复1-5天的影响最大。空间分辨率小于陆地表面模型分辨率(〜30 arc-min)的近地表土壤水分观测结果最好,空间分辨率大于模型分辨率的土壤分辨率也仅有轻微的下降。发现一半土地表面模型空间分辨率的观测值适合我们的应用。而且,发现满足空间分辨率和精度要求比重复时间重要得多。

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