Phenology shift from 1989 to 2008 on the Tibetan Plateau: an analysis with a process-based soil physical model and remote sensing data

doi:10.1007/s10584-013-0722-7

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	Phenology shift from 1989 to 2008 on the Tibetan Plateau: an analysis with a process-based soil physical model and remote sensing data
	Jin, Zhenong 1,2; Zhuang, Qianlai 1,3; He, Jin-Sheng 4,5; Luo, Tianxiang 6; Shi, Yue 4; Jin, ZN (reprint author), Purdue Univ, Interdisciplinary Grad Program, W Lafayette, IN 47907 USA.
	2013-07-01
发表期刊	CLIMATIC CHANGE
ISSN	0165-0009
卷号	119 期号:2 页码:435-449
文章类型	Article
摘要	Phenology is critical to ecosystem carbon quantification, and yet has not been well modeled considering both aboveground and belowground environmental variables. This is especially true for alpine and pan-arctic regions where soil physical conditions play a significant role in determining the timing of phenology. Here we examine how the spatiotemporal pattern of satellite-derived phenology is related to soil physical conditions simulated with a soil physical model on the Tibetan Plateau for the period 1989-2008. Our results show that spatial patterns and temporal trends of phenology are parallel with the corresponding soil physical conditions for different study periods. On average, 1 degrees C increase in soil temperature advances the start of growing season (SOS) by 4.6 to 9.9 days among different vegetation types, and postpones the end of growing season (EOS) by 7.3 to 10.5 days. Soil wetting meditates such trends, especially in areas where warming effect is significant. Soil thermal thresholds for SOS and EOS, defined as the daily mean soil temperatures corresponding to the phenological metrics, are spatially clustered, and are closely correlated with mean seasonal temperatures in Spring and Autumn, respectively. This study highlights the importance and feasibility of incorporating spatially explicit soil temperature and moisture information, instead of air temperature and precipitation, into phenology models so as to improve carbon modeling. The method proposed and empirical relations established between phenology and soil physical conditions for Alpine ecosystems on the Tibetan plateau could also be applicable for other cold regions.; Phenology is critical to ecosystem carbon quantification, and yet has not been well modeled considering both aboveground and belowground environmental variables. This is especially true for alpine and pan-arctic regions where soil physical conditions play a significant role in determining the timing of phenology. Here we examine how the spatiotemporal pattern of satellite-derived phenology is related to soil physical conditions simulated with a soil physical model on the Tibetan Plateau for the period 1989-2008. Our results show that spatial patterns and temporal trends of phenology are parallel with the corresponding soil physical conditions for different study periods. On average, 1 degrees C increase in soil temperature advances the start of growing season (SOS) by 4.6 to 9.9 days among different vegetation types, and postpones the end of growing season (EOS) by 7.3 to 10.5 days. Soil wetting meditates such trends, especially in areas where warming effect is significant. Soil thermal thresholds for SOS and EOS, defined as the daily mean soil temperatures corresponding to the phenological metrics, are spatially clustered, and are closely correlated with mean seasonal temperatures in Spring and Autumn, respectively. This study highlights the importance and feasibility of incorporating spatially explicit soil temperature and moisture information, instead of air temperature and precipitation, into phenology models so as to improve carbon modeling. The method proposed and empirical relations established between phenology and soil physical conditions for Alpine ecosystems on the Tibetan plateau could also be applicable for other cold regions.
WOS标题词	Science & Technology ; Life Sciences & Biomedicine ; Physical Sciences
DOI	10.1007/s10584-013-0722-7
关键词[WOS]	DELAYED SPRING PHENOLOGY ; CLIMATE-CHANGE ; VARIABILITY ; WINTER ; INDEX ; MODIS
收录类别	SCI
语种	英语
项目资助者	NSF(0919331) ; NSF Carbon and Water in the Earth Program(NSF-0630319) ; NASA Land Use and Land Cover Change program(NASA-NNX09AI26G) ; Department of Energy(DE-FG02-08ER64599) ; NSF Division of Information & Intelligent Systems(NSF-1028291)
WOS研究方向	Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
WOS类目	Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS记录号	WOS:000321955100017
引用统计	被引频次：57[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://210.75.249.4/handle/363003/3936
专题	中国科学院西北高原生物研究所
通讯作者	Jin, ZN (reprint author), Purdue Univ, Interdisciplinary Grad Program, W Lafayette, IN 47907 USA.
作者单位	1.Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA 2.Purdue Univ, Interdisciplinary Grad Program, W Lafayette, IN 47907 USA 3.Purdue Univ, Dept Agron, W Lafayette, IN 47907 USA 4.Peking Univ, Coll Urban & Environm Sci, Dept Ecol, Beijing 100871, Peoples R China 5.Chinese Acad Sci, Northwest Inst Plateau Biol, Key Lab Adaptat & Evolut Plateau Biota, Xining 810008, Peoples R China 6.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100085, Peoples R China
推荐引用方式 GB/T 7714	Jin, Zhenong,Zhuang, Qianlai,He, Jin-Sheng,et al. Phenology shift from 1989 to 2008 on the Tibetan Plateau: an analysis with a process-based soil physical model and remote sensing data[J]. CLIMATIC CHANGE,2013,119(2):435-449.
APA	Jin, Zhenong,Zhuang, Qianlai,He, Jin-Sheng,Luo, Tianxiang,Shi, Yue,&Jin, ZN .(2013).Phenology shift from 1989 to 2008 on the Tibetan Plateau: an analysis with a process-based soil physical model and remote sensing data.CLIMATIC CHANGE,119(2),435-449.
MLA	Jin, Zhenong,et al."Phenology shift from 1989 to 2008 on the Tibetan Plateau: an analysis with a process-based soil physical model and remote sensing data".CLIMATIC CHANGE 119.2(2013):435-449.

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