Advances in Earth Science ›› 2018, Vol. 33 ›› Issue (6): 590-605. doi: 10.11867/j.issn.1001-8166.2018.06.0590

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Passive Microwave Remote Sensing of Snow Depth and Snow Water Equivalent: Overview

Xiongxin Xiao( ), Tingjun Zhang *( )   

  1. Key Laboratory of Western China’s Environmental Systems (Ministry of Education), College of Earth Environmental Sciences, Lanzhou University, Lanzhou 730000,China
  • Received:2017-12-11 Revised:2018-05-15 Online:2018-06-20 Published:2018-07-23
  • Contact: Tingjun Zhang E-mail:xiaoxiongxin5118@126.com;tjzhang@lzu.edu.cn
  • About author:

    First author:Xiao Xiongxin (1991-), male, Fuping County, Shaanxi Province, Master student. Research areas include remote sensing of snow. E-mail:xiaoxiongxin5118@126.com

  • Supported by:
    Project supported by the National Key Scientific Research Program of China “Study on the remote sensing and multi-scale snow cover change of complex terrain”(No.2013CBA01802);The National Natural Science Foundation of China “Hydro(geo)logical processes and their impacts in permafrost regions in the upper reach of Heihe River in Northwest China”(No.91325202).

Xiongxin Xiao, Tingjun Zhang. Passive Microwave Remote Sensing of Snow Depth and Snow Water Equivalent: Overview[J]. Advances in Earth Science, 2018, 33(6): 590-605.

Snow cover is an informative indicator of climate change because it affects local and regional surface energy and water balance, hydrological processes and climate. Passive Microwave (PM) works all weather and round the clock and penetrates clouds and snow. Passive microwave remote sensing data have been widely applied to retrieving snow depth and snow water equivalent in the past few decades. Recently, the snow depth retrieval study has rapidly developed. This paper reviewed the research progress of snow depth and snow water equivalent inversion algorithm using PM data at home and abroad. Firstly, the basic theory of passive microwave remote sensing snow monitoring and passive microwave remote sensing data were introduced. Then, the current snow depth and snow water equivalent inversion algorithm were summarized into four categories: ① A statistically based linear inversion algorithm; ② An inversion algorithm based on microwave transmission snow model; ③ A nonlinear inversion algorithm based on prior knowledge; ④ Data fusion and data assimilation. Afterwards, the commonly used seven kinds of snow data products were introduced, and several factors affecting the snow depth and the snow water inversion accuracy were discussed. Finally, the possible direction of future snow parameter inversion research was prospected.

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