Climate Change Data Portal
DOI | 10.1657/1938-4246-41.3.396 |
Land-Atmosphere Energy Transfer and Surface Boundary Layer Characteristics in the Rongbu Valley on the Northern Slope of Mt. Everest | |
Zhong, Lei; Ma, Yaoming; Su, Zhongbo; Lu, Lixin; Ma, Weiqiang; Lu, Yaqiong | |
通讯作者 | Zhong, L (通讯作者) |
发表日期 | 2009 |
ISSN | 1523-0430 |
起始页码 | 396 |
结束页码 | 405 |
卷号 | 41期号:3 |
英文摘要 | The land-atmosphere interaction processes are unique at Mt. Everest as a result of high elevation. Based on turbulent data collected from April 2005 to March 2006 with the eddy covariance method at Quzong in the Rongbu Valley on the northern slope of Mt. Everest, land-atmosphere energy budget before and after the southwest monsoon onset and surface layer turbulent characteristics are Studied for the first time. It is found that energy budget components (net radiation flux, sensible heat flux, latent heat flux, and soil heat flux) and surface heating field have strong diurnal and seasonal variations. In particular under the influence of the southwest, monsoon, the characteristics of surface parameters can be clearly identified. From pre-monsoon to monsoon season, the sensible heat flux decreases whereas the latent heat flux increases. The latent heat flux and Evaporative Fraction at Quzong are relatively high most of the year. Furthermore, the intensity of heating source in the wet season (from June to August) is much greater than that in the dry season (from October to December). The relationship between normalized standard deviation of wind speed and atmospheric stability, variations of normalized standard deviation of temperature, and humidity with atmospheric stability are analyzed using the Monin-Obukhov similarity theory. The result reveals that the normalized standard deviation of velocity components of the three-dimensional wind speed follows similarity relationships in the convective and near-neutral surface layer, but does not seem to be valid in stable surface layer. However, the normalized standard deviation of temperature and humidity does not obey Monin-Obukhov similarity theory in the entire interval of atmospheric stratifications. |
关键词 | TIBETAN PLATEAUHEAT-FLUXTURBULENCEDESERTBUDGETAREA |
语种 | 英语 |
WOS研究方向 | Environmental Sciences & Ecology ; Physical Geography |
WOS类目 | Environmental Sciences ; Geography, Physical |
WOS记录号 | WOS:000269019100013 |
来源期刊 | ARCTIC ANTARCTIC AND ALPINE RESEARCH
![]() |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/257710 |
推荐引用方式 GB/T 7714 | Zhong, Lei,Ma, Yaoming,Su, Zhongbo,et al. Land-Atmosphere Energy Transfer and Surface Boundary Layer Characteristics in the Rongbu Valley on the Northern Slope of Mt. Everest[J]. 中国科学院青藏高原研究所,2009,41(3). |
APA | Zhong, Lei,Ma, Yaoming,Su, Zhongbo,Lu, Lixin,Ma, Weiqiang,&Lu, Yaqiong.(2009).Land-Atmosphere Energy Transfer and Surface Boundary Layer Characteristics in the Rongbu Valley on the Northern Slope of Mt. Everest.ARCTIC ANTARCTIC AND ALPINE RESEARCH,41(3). |
MLA | Zhong, Lei,et al."Land-Atmosphere Energy Transfer and Surface Boundary Layer Characteristics in the Rongbu Valley on the Northern Slope of Mt. Everest".ARCTIC ANTARCTIC AND ALPINE RESEARCH 41.3(2009). |
条目包含的文件 | 条目无相关文件。 |
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。