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Downward transport of ozone-rich air near Mt. Everest
Zhu, Tong ; Lin, Weili ; Song, Yu ; Cai, Xuhui ; Zou, Han ; Kang, Ling ; Zhou, Libo ; Akimoto, Hajime
刊名geophysical research letters
2006
关键词NONHYDROSTATIC ATMOSPHERIC SIMULATION PREDICTION SYSTEM ARPS BOUNDARY-LAYER AIR PART II MODEL VALLEY
DOI10.1029/2006GL027726
英文摘要High ozone concentrations ( 70 - 80 ppb) were found from late afternoon to midnight at sites at ca. 5000 m above sea level ( m. a. s. l.) on Mt. Everest. Observational data suggest that katabatic wind from Mt. Everest was "pumping down'' ozone-rich air from the upper troposphere. Numerical modelling demonstrates that cooling of glaciers and snow on the northern mountain slopes and heating of the valley surface play important roles in forming katabatic winds and accelerating vertical exchange between the upper atmosphere and surface air. These results suggest that the "pump-down'' mechanism at high mountains covered with snow/glaciers is an important process in terrestrial intercontinental transport of ozone and atmosphere - land exchanges of masses and energy.; Geosciences, Multidisciplinary; SCI(E); EI; 20; ARTICLE; 23; 33
语种英语
内容类型期刊论文
源URL[http://ir.pku.edu.cn/handle/20.500.11897/251177]  
专题环境科学与工程学院
推荐引用方式
GB/T 7714
Zhu, Tong,Lin, Weili,Song, Yu,et al. Downward transport of ozone-rich air near Mt. Everest[J]. geophysical research letters,2006.
APA Zhu, Tong.,Lin, Weili.,Song, Yu.,Cai, Xuhui.,Zou, Han.,...&Akimoto, Hajime.(2006).Downward transport of ozone-rich air near Mt. Everest.geophysical research letters.
MLA Zhu, Tong,et al."Downward transport of ozone-rich air near Mt. Everest".geophysical research letters (2006).
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