遥感与GIS应用

被动微波遥感数据反演地表温度研究进展

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  • 1. 中国科学院地理科学与资源研究所陆地水循环及地表过程重点实验室, 北京100101|
    2. 中国科学院研究生院, 北京100049
贾媛媛( 1979- )| 女, 陕西咸阳人, 博士研究生, 主要从事被动微波遥感反演地表参数研究. E- mail: jiayy.04b@igsnrr.ac.cn

收稿日期: 2005-12-01

  修回日期: 2006-03-01

  网络出版日期: 2006-05-25

基金资助

中国科学院2003 年度“百人计划”项目和国家杰出青年科学基金项目( 40425012) .

Progr ess in Land Sur face Temper atur e Retr ieval from Passive Microwave Remotely Sensed Data

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  • 1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographical Sciences and Natural Resources Research, CAS, Beijing 100101|
    2. Graduate School of the Chinese Academy of Sciences, Beijing 100049

Received date: 2005-12-01

  Revised date: 2006-03-01

  Online published: 2006-05-25

摘要

被动微波遥感具有穿透云层( 甚至雨区) 获取地表辐射信息的能力, 在处理云的问题上, 明 显优于可见光、红外遥感, 可更好地服务于相关领域研究。由于微波信号受多种因素的影响, 目前 被动微波反演地表温度的算法还不成熟。根据建模手段和方法的不同, 从经验反演模型和物理反 演模型两方面入手, 系统回顾国内外被动微波数据反演地表温度的算法并加以评述, 指出今后应 加强尺度转换、物理机理以及多数据源结合方面的研究。

本文引用格式

贾媛媛,李召良 . 被动微波遥感数据反演地表温度研究进展[J]. 地理科学进展, 2006 , 25(3) : 96 -105 . DOI: 10.11820/dlkxjz.2006.03.012

Abstract

Land surface temperature (LST) is of considerable importance for many applications, notably global climatic, hydrological, ecological and biogeochemical studies. In the past two decades, a large number of methods and algorithms have been developed to retrieve cloud free LST from thermal infrared data. As for all optical remote sensing, the Earth observation can only be realized for cloud free condition. In order to get LST for all weather conditions, microwave remotely sensed data, instead of thermal infrared data, from space is commonly used due to its capability to penetrate clouds and to some extent rain. Although the passive microwave remote sensing has some advantages compared to the thermal infrared, there are few algorithms developed to retrieve LST from it, mainly because there are various factors affected the microwave signal. In this paper, we review almost all existing algorithms found in literature, which can be roughly categorized into the statistical- based and physics- based retrieval algorithms, to retrieve LST from passive microwave remotely sensed data. The merits and the disadvantages are summarized for each method respectively. Finally further possible improvement and development directions on the scaling transfer, the microwave radiative transfer modeling and the combination of the different remote sensing data are given for LST retrieval from passive microwave data.

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