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Seasonal Characteristics of Surface Radiation Fluxes on the East Rongbuk Glacier in the Mt. Everest Region | |
Yang Xingguo; Qin Dahe![]() ![]() | |
发表日期 | 2010 |
ISSN | 0894-0525 |
EISSN | 2191-4788 |
卷号 | 24期号:6 |
英文摘要 | Ground-based measurements are essential for understanding alpine glacier dynamics, especially in remote regions where in-situ measurements are extremely limited. From 1 May to 22 July 2005 (the spring-summer period), and from 2 October 2007 to 20 January 2008 (the autumn-winter period), surface radiation as well as meteorological variables were measured over the accumulation zone on the East Rongbuk Glacier of Mt. Qomolangma/Everest at an elevation of 6560 m a.s.l. by using an automatic weather station (AWS). The results show that surface meteorological and radiative characteristics were controlled by two major synoptic circulation regimes: the southwesterly Indian monsoon regime in summer and the westerlies in winter. At the AWS site on the East Rongbuk Glacier, north or northwest winds prevailed with high wind speed (up to 35 m s(-1) in January) in winter while south or southeast winds predominated after the onset; of the southwesterly Indian monsoon with relatively low wind speed in summer. Intensity of incoming shortwave radiation was extremely high due to the high elevation, multiple reflections between the snow/ice surface and clouds, and the high reflective surrounding surface. These factors also caused the observed 10-min mean solar radiation fluxes around local noon to be frequently higher than the solar constant from May to July 2005. The mean surface albedo ranged from 0.72 during the spring-summer period to 0.69 during the autumn-winter period. The atmospheric incoming longwave radiation was greatly affected by the cloud condition and atmospheric moisture content. The overall impact of clouds on the net all-wave radiation balance was negative in the Mt. Qomolangma region. The daily mean net; all-wave radiation was positive during the entire spring-summer period and mostly positive during the autumn-winter period except for a few overcast days. On monthly basis, the net all-wave radiation was always positive. |
关键词 | Mt. Qomolangmaglaciersnow surfaceradiation featuremeteorological characteristic |
学科领域 | Meteorology & Atmospheric Sciences |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源期刊 | ACTA METEOROLOGICA SINICA
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来源机构 | 中国科学院西北生态环境资源研究院 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/111567 |
作者单位 | Univ Colorado, Cooperat Inst Res Environm Sci, Natl Snow & Ice Data Ctr, Boulder, CO 80309 USA |
推荐引用方式 GB/T 7714 | Yang Xingguo,Qin Dahe,Zhang Tingjun,et al. Seasonal Characteristics of Surface Radiation Fluxes on the East Rongbuk Glacier in the Mt. Everest Region[J]. 中国科学院西北生态环境资源研究院,2010,24(6). |
APA | Yang Xingguo,Qin Dahe,Zhang Tingjun,Kang Shichang,Qin Xiang,&Liu Hongyi.(2010).Seasonal Characteristics of Surface Radiation Fluxes on the East Rongbuk Glacier in the Mt. Everest Region.ACTA METEOROLOGICA SINICA,24(6). |
MLA | Yang Xingguo,et al."Seasonal Characteristics of Surface Radiation Fluxes on the East Rongbuk Glacier in the Mt. Everest Region".ACTA METEOROLOGICA SINICA 24.6(2010). |
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