Modeling the influence of land surface flux on the regional climate of the Tibetan Plateau
文献类型:期刊论文
作者 | Ma, WQ; Ma, YM (Ma, Yaoming)1,2; Ma, WQ (Ma, Weiqiang)1,2 |
刊名 | THEORETICAL AND APPLIED CLIMATOLOGY
![]() |
出版日期 | 2016 |
卷号 | 125期号:1-2页码:45-52 |
关键词 | Soil Heat-flux Heterogeneous Landscape Energy Aster Parameterization Ndvi Sebs Area |
DOI | 10.1007/s00704-015-1495-x |
文献子类 | Article |
英文摘要 | Land surface heat fluxes over the heterogeneous landscape of the Tibetan Plateau can serve as boundary conditions for modeling the regional climate and the Asian monsoon system. The Weather Research and Forecasting (WRF) atmospheric modeling system has enabled us to model the land surface heat flux through sensitivity experiments that utilize in situ observation data and the regional land-atmosphere exchanges of water and heat fluxes that are foundational to understanding the water and energy cycles present during the Asian monsoon period. A series of sensitivity experiments based on the WRF model and field observations has been proposed and tested for deriving the land surface heat fluxes (surface net radiation flux, soil heat flux, sensible heat flux, and latent heat flux) over a heterogeneous land surface. The sensitivity experiments were simulated over the field area of the Coordinated Enhanced Observing Period Asia-Australia Monsoon Project on the Tibetan Plateau (CEOP-CAMP/Tibet), located on the northern Tibetan Plateau of China. A WRF modeling period from July to August 2007 was selected for the summer monsoon conditions. To validate the modeling results, the ground-measured or calculated variables (e.g., net radiation flux, soil heat flux, sensible heat flux, and latent heat flux) were compared to the simulated values. The modeling results show that the derived model land surface heat fluxes are in agreement with the land surface observations over the study area in summer. Therefore, the WRF model sensitivity experiments were successful in simulating the land surface heat fluxes over the study area. |
学科主题 | 自然地理学 |
语种 | 英语 |
WOS记录号 | WOS:000378884600004 |
源URL | [http://ir.itpcas.ac.cn/handle/131C11/7670] ![]() |
专题 | 青藏高原研究所_图书馆 |
通讯作者 | Ma, WQ |
作者单位 | 1.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China 2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China |
推荐引用方式 GB/T 7714 | Ma, WQ,Ma, YM ,Ma, WQ . Modeling the influence of land surface flux on the regional climate of the Tibetan Plateau[J]. THEORETICAL AND APPLIED CLIMATOLOGY,2016,125(1-2):45-52. |
APA | Ma, WQ,Ma, YM ,&Ma, WQ .(2016).Modeling the influence of land surface flux on the regional climate of the Tibetan Plateau.THEORETICAL AND APPLIED CLIMATOLOGY,125(1-2),45-52. |
MLA | Ma, WQ,et al."Modeling the influence of land surface flux on the regional climate of the Tibetan Plateau".THEORETICAL AND APPLIED CLIMATOLOGY 125.1-2(2016):45-52. |
入库方式: OAI收割
来源:青藏高原研究所
浏览0
下载0
收藏0
其他版本
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。