中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
A surface soil temperature retrieval algorithm based on AMSR-E multi-frequency brightness temperatures

文献类型:期刊论文

作者Han, ML (Han, Menglei)1,2; Lu, H (Lu, Hui)1,3; Yang, K (Yang, Kun)1,3,4; Qin, J (Qin, Jun)2,5; Chen, YY (Chen, Yingying)2,4; Zhao, L (Zhao, Long)6; Lazhu (Lazhu)2; Lu, H
刊名INTERNATIONAL JOURNAL OF REMOTE SENSING
出版日期2017
卷号38期号:23页码:6735-6754
关键词IN-SITU OBSERVATIONS TIBETAN PLATEAU RADIOFREQUENCY INTERFERENCE MOISTURE NETWORK VALIDATION PRODUCTS MODEL GHZ SIMULATIONS RESOLUTION
DOI10.1080/01431161.2017.1363438
文献子类Article
英文摘要In this study, a multi-frequency statistical algorithm is proposed for retrieving surface soil temperature (T-s) from AMSR-E (Advanced Microwave Scanning Radiometer for Earth Observation System) brightness temperature (T-B) observations. The algorithm was developed based on a regression analysis between T-B from all AMSR-E bands and the corresponding in situ T-s observed by a soil moisture and temperature network in the central Tibetan Plateau. The new algorithm effectively utilizes information from the different bands provided by AMSR-E, lessening the influence of soil moisture, vegetation, and water vapour. Further validations were conducted based on seven soil moisture and temperature observation networks distributed globally. The results showed that the new multi-frequency algorithm can produce T-s values with a mean bias of less than 2 K and a root mean square error of less than 3 K for different vegetation-covered areas of the globe. Compared with a widely used single-band inversion algorithm, the new multi-frequency algorithm has better accuracy in estimating T-s and does not suffer from considerable overestimation or underestimation across these networks, indicating good transferability. This algorithm could contribute to research relating to the land energy balance by providing consistent and independent long-term estimates of daily global T-s. Nevertheless, the new algorithm has limited ability to retrieve T-s of frozen soil, given that AMSR-E T-B values are affected by the deep soil temperature after a soil is frozen.
学科主题自然地理学
WOS研究方向Remote Sensing; Imaging Science & Photographic Technology
语种英语
WOS记录号WOS:000412545900015
源URL[http://ir.itpcas.ac.cn/handle/131C11/8377]  
专题青藏高原研究所_图书馆
通讯作者Lu, H
作者单位1.Tsinghua Univ, Dept Earth Syst Sci, Minist Educ, Key Lab Earth Syst Modelling, Beijing 100084, Peoples R China.
2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing, Peoples R China.
3.Joint Ctr Global Change Studies, Beijing, Peoples R China.
4.CAS Ctr Excellence Tibetan Plateau Earth Syst, Beijing, Peoples R China.
5.Univ Chinese Acad Sci, Beijing, Peoples R China.
6.Southwest Univ, Sch Geog Sci, Chongqing, Peoples R China.
推荐引用方式
GB/T 7714
Han, ML ,Lu, H ,Yang, K ,et al. A surface soil temperature retrieval algorithm based on AMSR-E multi-frequency brightness temperatures[J]. INTERNATIONAL JOURNAL OF REMOTE SENSING,2017,38(23):6735-6754.
APA Han, ML .,Lu, H .,Yang, K .,Qin, J .,Chen, YY .,...&Lu, H.(2017).A surface soil temperature retrieval algorithm based on AMSR-E multi-frequency brightness temperatures.INTERNATIONAL JOURNAL OF REMOTE SENSING,38(23),6735-6754.
MLA Han, ML ,et al."A surface soil temperature retrieval algorithm based on AMSR-E multi-frequency brightness temperatures".INTERNATIONAL JOURNAL OF REMOTE SENSING 38.23(2017):6735-6754.

入库方式: OAI收割

来源:青藏高原研究所

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