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1971年以来珠穆朗玛峰地区气候变化
引用本文:杨续超,张镱锂,张玮,YAN Yuping,WANG Zhaofeng,DING Mingjun,CHU Duo.1971年以来珠穆朗玛峰地区气候变化[J].地理学报(英文版),2006,16(3):326-336.
作者姓名:杨续超  张镱锂  张玮  YAN Yuping  WANG Zhaofeng  DING Mingjun  CHU Duo
作者单位:1. 中国科学院地理科学与资源研究所
2. Laboratory for Climate Studies, National Climate Center, CMA, Beijing 100081, China
3. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;Graduate School of the Chinese Academy of Sciences, Beijing 100039, China
4. Tibet Institute of Plateau Atmospheric and Environmental Sciences, Lhasa 850000, China
基金项目:国家气象局资助项目,National Basic Research Program of China,中国科学院知识创新工程项目 
摘    要:Global climate change has profound influence on natural ecosystem and socioeconomic system and is a focus which governments, scientific societies as well as common people of various countries have paid much attention to. Observations indicate that there i…

关 键 词:珠穆朗玛峰  气候变化  温度  降水
收稿时间:2006-03-19
修稿时间:6/5/2006 12:00:00 AM

Climate change in Mt. Qomolangma region since 1971
Xuchao Yang,Yili Zhang,Wei Zhang,Yuping Yan,Zhaofeng Wang,Mingjun Ding,Duo Chu.Climate change in Mt. Qomolangma region since 1971[J].Journal of Geographical Sciences,2006,16(3):326-336.
Authors:Xuchao Yang  Yili Zhang  Wei Zhang  Yuping Yan  Zhaofeng Wang  Mingjun Ding  Duo Chu
Institution:(1) Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing, 100101, China;(2) Graduate School of the Chinese Academy of Sciences, Beijing, 100039, China;(3) Institute of Tibetan Plateau Research, CAS, Beijing, 100085, China;(4) Laboratory for Climate Studies, National Climate Center, CMA, Beijing, 100081, China;(5) Tibet Institute of Plateau Atmospheric and Environmental Sciences, Lhasa, 850000, China
Abstract:Using monthly average, maximum, minimum air temperature and monthly precipitation data from 5 weather stations in Mt. Qomolangma region in China from 1971 to 2004, climatic linear trend, moving average, low-pass filter and accumulated variance analysis methods, the spatial and temporal patterns of the climatic change in this region were analyzed. The main findings can be summarized as follows: (1) There is obvious ascending tendency for the interannual change of air temperature in Mt. Qomolangma region and the ascending tendency of Tingri, the highest station, is the most significant. The rate of increasing air temperature is 0.234 oC/decade in Mt. Qomolangma region, 0.302 oC/decade in Tingri. The air temperature increases more strongly in non-growing season. (2) Compared with China and the global average, the warming of Mt. Qomolangma region occurred early. The linear rates of temperature increase in Mt. Qomolangma region exceed those for China and the global average in the same period. This is attributed to the sensitivity of mountainous regions to climate change. (3) The southern and northern parts of Mt. Qomolangma region are quite different in precipitation changes. Stations in the northern part show increasing trends but are not statistically significant. Nyalam in the southern part shows a decreasing trend and the sudden decreasing of precipitation occurred in the early 1990s. (4) Compared with the previous studies, we find that the warming of Mt. Qomolangma high-elevation region is most significant in China in the same period. The highest automatic meteorological comprehensive observation station in the world set up at the base camp of Mt. Qomolangma with a height of 5032 m a.s.l will play an important role in monitoring the global climate change.
Keywords:Mt  Qomolangma region  climate change  temperature  precipitation
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