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	Assessing and improving Noah-MP land model simulations for the central Tibetan Plateau
	Gao, Yanhong1; Li, Kai1; Chen, Fei2,3; Jiang, Yingsha1; Lu, Chungu4
刊名	JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
	2015-09-27
卷号	120期号:18页码:9258-9278
关键词	land-surface modeling Tibetan Plateau organic matter rhizosphere Noah-MP land model spin-up and forcing
ISSN号	2169-897X
DOI	10.1002/2015JD023404
通讯作者	Gao, Yanhong(gaoyh@lzb.ac.cn)
英文摘要	The Tibetan Plateau (TP) region experiences strong land-atmosphere interactions, and as an elevated heating source, significantly influences the formation of the Asian monsoon. Those interactions are not well represented in current land-surface models (LSMs), partly due to difficulties in representing heterogeneities in soil structures in LSM. Simulations using the Noah with multiparameterization options (Noah-MP) LSM are employed to assess the relative importance of parameterizing vertical soil heterogeneity, organic matter, and soil rhizosphere and their impacts on seasonal evolution of soil temperature, soil moisture, and surface energy and water budgets at the sparsely vegetated Amdo site located in central TP. The LSM spin-up time at the central TP depends on the complexity of the model physics, ranging from 4years with simplest soil physics to 30years with the addition of organic matter and spare to dense rhizosphere parameterization in Noah-MP. Representing layered soil texture and organic matter does not improve low biases in topsoil moisture. Reducing the saturated conductivity from the mucilage in the rhizosphere produces better results. Surface sensible and latent heat fluxes are better simulated in the monsoon season as well. Adding layered soil texture and organic matter in Noah-MP retard the thawing in deep soil layers, and the rhizosphere effect delays thawing even more in the transient season. Uncertainties in soil initialization significantly affect deep-soil temperature and moisture, but uncertainties in atmospheric forcing conditions mainly affect topsoil variables and consequently the surface energy fluxes. Differing land-surface physics cause 36% uncertainty in the accumulated evapotranspiration and subsurface runoff.
收录类别	SCI
WOS关键词	DATA ASSIMILATION SYSTEM ; SURFACE-ENERGY BUDGET ; DESERT STEPPE SITE ; SOIL-WATER CONTENT ; ARW-WRF ; CASES-97 OBSERVATIONS ; PHYSICAL-PROPERTIES ; CANOPY-RESISTANCE ; CLIMATE MODELS ; RIVER-BASIN
WOS研究方向	Meteorology & Atmospheric Sciences
WOS类目	Meteorology & Atmospheric Sciences
语种	英语
出版者	AMER GEOPHYSICAL UNION
WOS记录号	WOS:000363425900014
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/2557210
专题	寒区旱区环境与工程研究所
通讯作者	Gao, Yanhong
作者单位	1.Chinese Acad Sci, Key Lab Land Surface Proc & Climate Change Cold &, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou, Peoples R China 2.Natl Ctr Atmospher Res, Boulder, CO 80307 USA 3.China Meteorol Adm, Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing, Peoples R China 4.Natl Sci Fdn, Arlington, VA 22230 USA
推荐引用方式 GB/T 7714	Gao, Yanhong,Li, Kai,Chen, Fei,et al. Assessing and improving Noah-MP land model simulations for the central Tibetan Plateau[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2015,120(18):9258-9278.
APA	Gao, Yanhong,Li, Kai,Chen, Fei,Jiang, Yingsha,&Lu, Chungu.(2015).Assessing and improving Noah-MP land model simulations for the central Tibetan Plateau.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,120(18),9258-9278.
MLA	Gao, Yanhong,et al."Assessing and improving Noah-MP land model simulations for the central Tibetan Plateau".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 120.18(2015):9258-9278.

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