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Accuracy Issues Associated with Satellite Remote Sensing Soil Moisture Data and Their Assimilation

机译:与卫星遥感土壤水分数据有关的精度问题及其同化

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Satellite remote sensing is widely used for monitoring the changing planet Earth. Many remote sensing data products are being generated and used every day. Among these data products are the microwave remote sensing data of land surface soil moisture. Soil moisture often limits the exchanges of water and energy between atmosphere and land surface,controls the partitioning of rainfall among evaporation,infiltration and runoff,and impacts vegetation photosynthetic rate and soil microbiologic respiratory activities. Their accuracy plays essential role for the success of their applications. Accurate measurement of this variable across the global land surface is thus required for global water,energy and carbon cycle sciences and many civil and military applications. Currently available satellite soil moisture data products have been generated from the low frequency channel observations of the currently flying microwave sensors (the TRMM Microwave Imager-TMI; Aqua Advanced Microwave Scanning Radiometer-AMSR-E,and Navel Research Lab's WindSat). However,because of several accuracy issues all of these soil moisture data have not yet been used in operational applications. The most apparent accuracy issue is that the soil moisture data retrievals from the three different sensors are significantly different from each other even when they are retrieved with the same algorithm. This might have been caused by the calibration errors in their brightness temperatures. A Simultaneous Conical-scanning Overpass (SCO) method is tested to address this issue.Secondly,satellite sensor footprints are usually several orders larger than the local points where in situ soil moisture measurements for validation are obtained. How to appropriately compare the satellite soil moisture retrievals of large spatial areas with the in situ measurements becomes an important issue. A point-to-pixel mapping approach is examined for a solution of this issue. The third issue is how to handle biases of the soil moisture retrievals from land surface model (LSM) simulations when they are assimilated into the LSM.Existing solutions for this issue are summarized and whether these error-handling strategies are effective or reliable are discussed. Finally general conclusions of this study are presented for users who are interested in satellite soil moisture data assimilation.
机译:卫星遥感被广泛用于监测不断变化的地球。每天都会产生并使用许多遥感数据产品。这些数据产品包括陆地表面土壤水分的微波遥感数据。土壤水分通常会限制大气与土地表面之间的水和能量交换,控制降雨在蒸发,渗透和径流之间的分配,并影响植被的光合速率和土壤微生物呼吸活动。它们的准确性对成功应用至关重要。因此,对于全球水,能源和碳循环科学以及许多民用和军事应用,需要在全球陆地表面上精确测量此变量。当前可用的卫星土壤水分数据产品是通过对当前飞行的微波传感器(TRMM微波成像仪-TMI; Aqua先进微波扫描辐射仪-AMSR-E和Navel Research Lab的WindSat)进行的低频通道观测生成的。但是,由于几个准确性问题,所有这些土壤湿度数据尚未在操作应用中使用。最明显的准确性问题是,即使使用相同的算法检索来自三个不同传感器的土壤水分数据,它们之间也存在显着差异。这可能是由于其亮度温度的校准错误引起的。测试了同时锥形扫描立交桥(SCO)的方法来解决此问题。其次,卫星传感器的覆盖区通常比获得原位土壤水分测量值以进行验证的局部点大几个数量级。如何适当地将大空间区域的卫星土壤水分反演结果与实地测量结果进行比较成为一个重要的问题。为了解决这个问题,研究了点到像素的映射方法。第三个问题是如何在将土地水分模型(LSM)模拟同化为LSM后,如何处理土壤水分反演中的偏差。总结了该问题的现有解决方案,并讨论了这些错误处理策略是否有效或可靠。最后,向对卫星土壤湿度数据同化感兴趣的用户提供了本研究的一般结论。

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