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珠峰地区大气边界层结构的一次观测研究
引用本文:孙方林,马耀明,马伟强,李茂善.珠峰地区大气边界层结构的一次观测研究[J].高原气象,2006,25(6):1014-1019.
作者姓名:孙方林  马耀明  马伟强  李茂善
作者单位:1. 中国科学院,寒区旱区环境与工程研究所,甘肃,兰州,730000
2. 中国科学院,青藏高原研究所,北京,100085;中国科学院,寒区旱区环境与工程研究所,甘肃,兰州,730000
基金项目:中国科学院知识创新工程项目 , 国家重点基础研究发展计划(973计划) , 中国气象局成都高原气象研究所开放课题
摘    要:利用2005年8月31日~9月5日中国科学院珠穆朗玛峰综合观测研究站的LAP3000风廓线仪的观测资料,分析了该地区气温日变化和大气边界层风廓线结构。结果表明,该地区1500 m以下大气边界层主要受高原山地地形及珠峰地区冰川环境的影响,冰川风可能是引起观测期间下午强风天气的主要原因;1500 m以上高空受西风气流影响程度增大,但东南风仍占有一定比例。

关 键 词:珠峰地区  LAP3000风温廓线仪  大气边界层结构  冰川风
文章编号:1000-0534(2006)06-1014-06
收稿时间:2006-01-14
修稿时间:2006-01-142006-04-12

One Observational Study on Atmospheric Boundary Layer Structure in Mt. Qomolangma Region
SUN Fang-lin,MA Yao-ming,MA Wei-qiang,LI Mao-shan.One Observational Study on Atmospheric Boundary Layer Structure in Mt. Qomolangma Region[J].Plateau Meteorology,2006,25(6):1014-1019.
Authors:SUN Fang-lin  MA Yao-ming  MA Wei-qiang  LI Mao-shan
Institution:1. Cold and Arid Regions Environmental and Engineering Research Institute , Chinese Academy of Sciences, Lanzhou 730000, China; 2. Institute of Tibetan Plateau Research, Chinese Academy of Sciences , Beijing 100085, China
Abstract:Using the data of the LAP3000 Wind Profiler set on the Comprehensive Observation and Research Station on Qomolangma,CAS(CORSQ) from August 31 to September 5,2005,the diurnal change of air temperature and the atmospheric boundary layer wind profiles are analyzed.The result shows that the mountainous landform and the glacier environment of Mt.Qomolangma region had a major influence on the lower atmospheric boundary layer,and the strong wind that took place in late afternoon which was probably caused by the glacier wind from Mt Qomolangma.In the upper air above 1500 m,west airflow became the major,but the southeast wind sill existed at a ratio of about 15% during observation.
Keywords:Mt  Qomolangma region  LAP3000 wind profiler  Structure of atmospheric boundarylayer  Glacier wind
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