首页> 外文会议>IEEE International Geoscience and Remote Sensing Symposium >L-, C- AND X-BAND PASSIVE MICROWAVE SOIL MOISTURE RETRIEVAL ALGORITHM PARAMETERIZATION USING IN SITU VALIDATION SITES
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L-, C- AND X-BAND PASSIVE MICROWAVE SOIL MOISTURE RETRIEVAL ALGORITHM PARAMETERIZATION USING IN SITU VALIDATION SITES

机译:L-,C-和X波段被动微波土壤湿度检索算法参数化使用原位验证网站

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Soil moisture plays a significant role in disciplines such as hydrology, meteorology and agriculture, and passive microwave remote sensing has become a widely used technique for global soil moisture estimation over the past three decades. Several satellite missions carrying radiometers have been launched over the past years. Among them are Japan Aerospace Exploration Agency's (JAXA's) Advanced Microwave Scanning Radiometer-EOS (AMSR-E) launched on NASA's Aqua satellite, European Space Agency's (ESA's) Soil Moisture and Ocean Salinity (SMOS) mission, JAXA's Advanced Microwave Scanning Radiometer 2 (AMSR2) onboard the GCOM-W satellite, and NASA's Soil Moisture Active Passive (SMAP) mission. Based on the availability of these four missions, there is an opportunity to develop a consistent inter-calibrated long-term soil moisture data record. This study focuses on the parametrization of the tau-omega model for soil moisture retrieval at L-, C- and X-band using brightness temperature observations from the four missions and in-situ soil moisture and soil temperature data from the SMAP core validation sites across various land cover types. The ancillary data sets used in the SMAP baseline algorithm are used for the retrievals at different frequencies. Simultaneous calibrations of the vegetation parameter b and roughness parameter h at both horizontal and vertical polarizations are performed. A set of model parameters to successfully retrieve soil moisture at different validation sites at L-, C- and X-band are presented. A preliminary comparison of SMAP and AMSR2 soil moisture retrievals against in situ observations at the Yanco (Australia) and TxSON (U.S.) sites showed the best accuracy and correlation at L-band (RMSD=0.03-0.05 m~3/m~3; R=0.92-0.94). The C-/X-band performance was not as satisfactory as L-band (RMSD=0.08-0.17 m~3/m~3; R=0.24-0.79). This also indicates that retrieval at higher frequencies can be very challenging when dense vegetation is present.
机译:土壤水分在水文,气象学和农业等学科中起着重要作用,被动微波遥感已经成为过去三十年来全球土壤水分估算的广泛使用技术。几个卫星任务携带辐射仪已经在过去几年推出。其中包括日本航空航天勘探机构(JAXA)先进的微波扫描辐射计-EOS(AMSR-E)在美国宇航局的AQUA卫星,欧洲航天局(ESA)土壤水分和海洋盐度(SMOS)使命,JAXA先进的微波扫描辐射计2( AMSR2)船上GCOM-W卫星,美国宇航局的土壤湿气主动被动(SMAP)任务。根据这四项任务的可用性,有机会开发一致的间校准的长期土壤水分数据记录。本研究侧重于使用来自四个任务的亮度温度观测和来自SMAP核心验证网站的亮度温度观测的L-,C和X波段的土壤水分检测的Tau-oomega模型的参数化跨越各种陆地覆盖类型。 SMAP基线算法中使用的辅助数据集用于不同频率的检索。执行植被参数B和粗糙度参数H的同时校准,在水平和垂直偏振中进行。提出了一组成功检索在L-,C-和X波段的不同验证位点的土壤水分的模型参数。 SMAP和AMSR2土壤水分检索的初步比较在YANCO(澳大利亚)和TXSON(US)网站上的原位观察结果显示了L波段的最佳精度和相关性(RMSD = 0.03-0.05 m〜3 / m〜3; r = 0.92-0.94)。 C- / X波段性能与L波段不如令人满意(RMSD = 0.08-0.17 m〜3 / m〜3; r = 0.24-0.79)。这也表明,当存在密集的植被时,在较高频率下检索可能非常具有挑战性。

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