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Different attenuation correction methods for the X-band dual linear polarimetric radar are analyzed in this paper.The specific differential phase shift K DP is always considered as an effective factor in radar signal attenuation correction.However,the values of K DP for light rains are too small,which results in unstable quality and large errors of rainfall estimation.Therefore,radar horizontal reflectivity Z H and specific differential phase shift are combined together in the Z H –K DP method to correct th... 相似文献
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Ground-based measurements are essential for understanding alpine glacier dynamics,especially in remote regions where in-situ measurements are extremely limited.Prom 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... 相似文献
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Alpine glaciers usually feature with best hydrothermal condition in mountain climate,and present beautiful glacier scenery,various glacier landforms,rich biodiversity,and easier accessibility,compared with continental glaciers or ice sheets.Nevertheless,Alpine glaciers are more sensitive to climate warming,and climate warming has seriously affected Alpine glaciers and surroundingenvironment.The quality and attractiveness of Alpine glaciers to tourism has been and will continue to be diminished with tourists... 相似文献
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In order to verify the feasibility and stability of a degree-day model on simulating the long time series of glacier mass balance, we apply a degree-day model to simulate the mass balance of Urumqi Glacier No. 1 for the period 1987/1988-2007/2008 based on temperature and precipitation data from a nearby climate station. The model is calibrated by simulating point measurements of mass bal-ance, mass balance profiles, and mean specific mass balance during 1987/1988-1996/1997. The opti-mized parameters are obt... 相似文献
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1. Biographical information GuoDong Cheng, born on 11 July, 1943, in Shanghai, China, received his Bachelor of Science in 1965, from the Department of Hydrogeology and Engineering Geology at Beijing Geology College （now China University of Geosciences）. In the same year, he started his research career at the Lanzhou Institute of Glaciology, Geocryology, and Desert Research, Chinese Academy of Sciences （CAS）. Over the past 45 years, Professor Cheng has published more than 200 papers in peer-reviewed professional journals and 相似文献
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1. Biographical information GuoDong Cheng, born on 11 July, 1943, in Shanghai, China, received his Bachelor of Science in 1965, from the Department of Hydrogeology and Engineering Geology at Beijing Geology College （now China University of Geosciences）. In the same year, he started his research career at the Lanzhou Institute of Glaciology, Geocryology, and Desert Research, Chinese Academy of Sciences 相似文献
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CHEN BaiLian ZHANG RenHe SUN ShuFen BIAN LinGen XIAO CunDe & ZHANG TingJun Institute of Atmospheric Physics Chinese Academy of Sciences Beijing China Chinese Academy of Meteorological Sciences Beijing Graduate University of Chinese Academy of Sciences Beijing Cold Arid Regions Environmental Engineering Research Institute Lanzhou The National Snow Ice Data Center University of Colorado... 《中国科学:地球科学(英文版)》2010,(5)
A vertical one-dimensional numerical model for heat transferring within the near-surface snow layer of the Antarctic Ice Sheet was developed based on simplified parameterizations of associated physical processes for the atmosphere, radiation, and snow/ice systems. Using the meteorological data of an automatic weather station (AWS) at Dome A (80°22′S, 70°22′E), we applied the model to simulate the seasonal temperature variation within a depth of 20 m. Comparison of modeled results with observed snow temperat... 相似文献
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WU JiChun SHENG Yu WU QingBai & WEN Zhi State Key Laboratory of Frozen Soil Engineering Cold Arid Regions Environmental Engineering Research Institute Chinese Academy of Sciences Lanzhou China 《中国科学:地球科学(英文版)》2010,(1)
Climate warming must lead the mainly air temperature controlled permafrost to degrade.Based on the numerical simulation,the process of permafrost degradation can be divided into five stages,i.e.,starting stage,temperature rising stage,zero geothermal gradient stage,talic layers stage,and disappearing stage,according to the shape of ground temperature profile.Permafrost on the Qinghai-Tibet Plateau (QTP) is generally considered a relic from late Pleistocene,and has been degenerating as a whole during Holocen... 相似文献