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	Evaluation of a coupled snow and energy balance model for Zhadang glacier, Tibetan Plateau, using glaciological measurements and time-lapse photography
	Huintjes, Eva1; Sauter, Tobias2,4; Schroeter, Benjamin3; Maussion, Fabien4,8; Yang, Wei5,6; Kropacek, Jan3,7; Buchroithner, Manfred3; Scherer, Dieter8; Kang, Shichang6,9; Schneider, Christoph1
刊名	ARCTIC ANTARCTIC AND ALPINE RESEARCH
	2015-08-01
卷号	47期号:3页码:573-590
ISSN号	1523-0430
DOI	10.1657/AAAR0014-073
通讯作者	Huintjes, Eva(eva.huintjes@geo.rwth-aachen.de)
英文摘要	We present a new open-source, collaborative "COupled Snowpack and Ice surface energy and MAss balance model" (COSIMA) that is evaluated for Zhadang glacier, Tibetan Plateau. The model is calibrated, run, and validated based on in situ measurements and atmospheric model data from the High Asia Refined analysis (HAR) over the period April 2009 to June 2012. Results for the model runs forced by both in situ measurements and HAR agree well with observations of various atmospheric, glaciological, surface, and subsurface parameters on the glacier. A time-lapse camera system next to the glacier provides a 3-year image time series of the mean transient snow line altitude and the snow cover pattern, which is used for the spatial and temporal validation of the model. The model output corresponds very well to the observed temporal and spatial snow cover variability. The model is then run for a 10-year period of October 2001 to September 2011 forced with HAR data. In general, the radiation components dominate the overall energy turnover (65%), followed by the turbulent fluxes (31%). The generally dry atmosphere on the Tibetan Plateau causes sublimation to be responsible for 26% of the total mass loss. A proportion of 11% of the surface and subsurface melt refreezes within the snowpack.
收录类别	SCI
WOS关键词	DISTRIBUTED SURFACE-ENERGY ; NAM CO BASIN ; MASS-BALANCE ; PRECIPITATION SEASONALITY ; NYAINQENTANGLHA RANGE ; SUMMER-ACCUMULATION ; HIMALAYAN GLACIERS ; CLIMATE-CHANGE ; HIGH ASIA ; RUNOFF
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:000359679000014
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/2557052
专题	寒区旱区环境与工程研究所
通讯作者	Huintjes, Eva
作者单位	1.Rhein Westfal TH Aachen, Dept Geog, D-52056 Aachen, Germany 2.Univ Erlangen Nurnberg, Dept Geog, D-91058 Erlangen, Germany 3.Tech Univ Dresden, Inst Cartog, D-01069 Dresden, Germany 4.Univ Innsbruck, Inst Meteorol & Geophys, A-6020 Innsbruck, Austria 5.Chinese Acad Sci, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China 6.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China 7.Univ Tubingen, Dept Geog, D-72070 Tubingen, Germany 8.Tech Univ Berlin, Dept Ecol, D-12165 Berlin, Germany 9.Chinese Acad Sci, State Key Lab Cryospher Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China
推荐引用方式 GB/T 7714	Huintjes, Eva,Sauter, Tobias,Schroeter, Benjamin,et al. Evaluation of a coupled snow and energy balance model for Zhadang glacier, Tibetan Plateau, using glaciological measurements and time-lapse photography[J]. ARCTIC ANTARCTIC AND ALPINE RESEARCH,2015,47(3):573-590.
APA	Huintjes, Eva.,Sauter, Tobias.,Schroeter, Benjamin.,Maussion, Fabien.,Yang, Wei.,...&Schneider, Christoph.(2015).Evaluation of a coupled snow and energy balance model for Zhadang glacier, Tibetan Plateau, using glaciological measurements and time-lapse photography.ARCTIC ANTARCTIC AND ALPINE RESEARCH,47(3),573-590.
MLA	Huintjes, Eva,et al."Evaluation of a coupled snow and energy balance model for Zhadang glacier, Tibetan Plateau, using glaciological measurements and time-lapse photography".ARCTIC ANTARCTIC AND ALPINE RESEARCH 47.3(2015):573-590.

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