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	Mapping surface soil freeze-thaw cycles in china based on smmr and ssm/i brightness temperatures from 1978 to 2008
	Jin, Rui1,2; Zhang, Tingjun3; Li, Xin1,2; Yang, Xingguo4; Ran, Youhua1
刊名	Arctic antarctic and alpine research
	2015-05-01
卷号	47期号:2页码:213-229
ISSN号	1523-0430
DOI	10.1657/aaar00c-13-304
通讯作者	Zhang, tingjun(tjzhang@lzu.edu.cn)
英文摘要	This paper aims to provide a long time-series data set documenting the surface soil freeze-thaw cycles in china over a period of more than 30 years. the remote sensing data are from the daily brightness temperatures recorded by the scanning multichannel microwave radiometer (smmr, 1978-1987) and special sensor microwave imager (ssm/i, 1987-2008), which have a 25 km spatial resolution. the classification method used to identify the surface soil freeze-thaw states is a dual-indices algorithm based on the 37 ghz vertical polarization brightness temperature and spectral gradient between the 37 ghz and 18/19 ghz brightness temperatures. this algorithm has been recalibrated for smmr and ssm/i using the in situ daily minimal ground surface temperatures observed at 77 meteorological stations covering the dominant land surface types of china. the daily classifications of surface soil freeze-thaw states were validated by observations from an additional 273 meteorological stations. the classification accuracy of the frozen and thawed soils as well as the total accuracy exceed 80%. based on this data set, we analyzed the seasonal and interannual variations across the areal extent and timing of surface soil freezing, trend of the onset date of surface soil freezing and thawing, and duration of surface soil thawing in china. the results showed that the maximum frozen extent during 1978-1987 was 6.93 x 10(6) km(2) or 72.8% of the area, and it generally occurred in late december and january. the minimum frozen extent was 0.26 x 10(6) km(2) or 3.0% of the area, and it occurred in late july and august. the first day of soil freezing occurred between september and november, whereas the first day of soil thawing occurred between march and may. the trend analysis demonstrated that from 1978 to 2008, the onset date of surface freezing was postponed by 19.6 +/- 14.6 days, whereas the onset of surface thawing was advanced by -19.0 +/- 9.4 days, and the thawing period was prolonged by 34.3 +/- 16.5 days. these trends revealed a pattern of earlier thawing, later freezing, and longer growing seasons because of climate warming, especially in the seasonally frozen ground and permafrost regions with high ground temperatures.
收录类别	SCI
WOS关键词	SNOW COVER ; SCATTEROMETER DATA ; TIME-SERIES ; BOREAL ; CLASSIFICATION ; BOUNDARIES ; FORESTS ; SEASONS
WOS研究方向	Environmental Sciences & Ecology ; Physical Geography
WOS类目	Environmental Sciences ; Geography, Physical
语种	英语
出版者	INST ARCTIC ALPINE RES
WOS记录号	WOS:000355627500004
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/2555015
专题	寒区旱区环境与工程研究所
通讯作者	Zhang, Tingjun
作者单位	1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China 2.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China 3.Lanzhou Univ, Coll Earth & Environm Sci, MOE Key Lab West Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China 4.Meteorol Bur Gansu Prov, Lanzhou 730020, Gansu, Peoples R China
推荐引用方式 GB/T 7714	Jin, Rui,Zhang, Tingjun,Li, Xin,et al. Mapping surface soil freeze-thaw cycles in china based on smmr and ssm/i brightness temperatures from 1978 to 2008[J]. Arctic antarctic and alpine research,2015,47(2):213-229.
APA	Jin, Rui,Zhang, Tingjun,Li, Xin,Yang, Xingguo,&Ran, Youhua.(2015).Mapping surface soil freeze-thaw cycles in china based on smmr and ssm/i brightness temperatures from 1978 to 2008.Arctic antarctic and alpine research,47(2),213-229.
MLA	Jin, Rui,et al."Mapping surface soil freeze-thaw cycles in china based on smmr and ssm/i brightness temperatures from 1978 to 2008".Arctic antarctic and alpine research 47.2(2015):213-229.

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