[1]李海东,沈渭寿,佘光辉,等.雅鲁藏布江源区近35年气候变化特征[J].水土保持研究,2010,17(05):63-67.
　LI Hai-dong,SHEN Wei-shou,SHE Guang-hui,et al.Climatic Changes in the Source Region of the Yarlung Zangbo River over Last 35 Years, China[J].Research of Soil and Water Conservation,2010,17(05):63-67.
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雅鲁藏布江源区近35年气候变化特征

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 17 期数: 2010年05期 页码: 63-67 栏目: 出版日期: 2010-10-20
Title:
Climatic Changes in the Source Region of the Yarlung Zangbo River over Last 35 Years, China
作者:
李海东1,2, 沈渭寿2, 佘光辉1, 程建敏3, 孙俊2, 孙明2
1. 南京林业大学 森林资源与环境学院, 南京 210037;
2. 环境保护部南京环境科学研究所, 南京 210042;
3. 江苏省水文水资源勘测局连云港分局, 江苏 连云港 222004
Author(s):
LI Hai-dong1,2, SHEN Wei-shou2, SHE Guang-hui1, CHENG Jian-min3, SUN Jun2, SUN Ming2
1. College of Forest Resources and Environment, Nanjing Forestry University, Nanjing 210037, China;
2. Nanjing Institute of Environmental Sciences, Ministry of Environmental Protection, Nanjing 210042, China;
3. Lianyungang Hydrology & Water Resource Survey Bureau of Jiangsu Province, Lianyungang, Jiangsu 222004, China
关键词:
雅鲁藏布江源区; 气候变化; 气温; 降水; 风速; 日照时数
Keywords:
source region of the Yarlung Zangbo River; climate change; temperature; precipitation; wind speed; sunshine duration
分类号:
P467
摘要:
为揭示雅江源区风沙化土地发育的气候变化背景，通过对雅江源区周边4个基本气象站1973-2007年的逐日气象资料进行等权平均取值，采用气候线性趋势分析法，研究了气温、降水、日照时数、风速等气象因子近35 a的变化特征及趋势。结果表明：（1）雅江源区多年平均降水量为206.12 mm，日平均气温为2.77℃、最高气温为10.72℃、最低气温为－4.81℃，年日照时数为3 295.16 h，年平均风速为2.92 m/s。（2）近35 a来，雅江源区气候变暖趋势明显，1986年以后，平均气温线性升温率为0.77℃/10 a，高于近35 a来的平均值0.47℃/10 a和珠峰地区5站平均线性升温率为0.234℃/10 a。（3）年平均降水量的波动较大，增加趋势不明显，平均增长率为0.43 mm/10 a。降水量主要集中于5-9 月，占全年降水量的89.72%。年平均日照时数波动性较大，上升趋势不显著。以5月和10月较高，1月最低。年平均风速下降趋势明显，以3月最大，为3.67 m/s，11月最小，为2.20 m/s。可见，雅江源区是中国同期升温最显著的区域。
Abstract:
The objective of this paper is to reveal the climate background of the aeolian sand landform development in the source region of the Yarlung Zangbo river. Based on air temperature, precipitation, the highest and lowest air temperature, duration of sunshine, and wind speed daily data from 4 meteorological stations around the source region of the Yarlung Zangbo river, the features of climatic change in this region were analyzed comprehensively over the last 35 years from 1973 to 2007 using climatic linear trend methods. The main findings can be summarized as follows: (1) The source region of the Yarlung Zangbo river belongs to the cold and semi-arid highland climate zone with the mean annual precipitation of 206.12 mm, daily average air temperature of 2.77℃, maximum air temperature of 10.72℃ and minimum air temperature of -4.81℃, annual average wind speed of 2.92 m/s, annual sunshine hours for the 3 295.16 h from 1973 to 2007. (2) There was an obvious ascending trend for daily average air temperature in recent 35 years, especially after 1986, the average temperature of the linear growth rate was 0.77℃/10 a, it was higher than the average linear growth rate of 0.47℃/10 a in the past 35 years and an average of 5 stations in Mt. Qomolangma region of 0.234℃/10 a. (3) The fluctuation of annual mean precipitation was lager, and its increasing trend was not obvious, with an average growth rate of 0.43 mm/10 a. Precipitation mainly concentrated in May and September, accounting for 89.72% throughout the year. The rising trend of annual average sunshine hour volatile was not significant, with the highest in May and October, and the lowest in January. The declining trend in annual average wind speed was significant, with the largest in March (3.67 m/s), the lowest in November (2.20 m/s). It can be seen that this region was the most significant heating up region over the same period in China.

参考文献/References:

[1] IPCC.Climate Change 2001:The Scientific Basis[M].Cambridge:Cambridge University Press,2001:140-165.
[2] 杨续超,张镱锂,张玮,等.珠穆朗玛峰地区近34年来气候变化[J].地理学报,2006,61(7):687-696.
[3] 冯松,汤懋苍,王冬梅.青藏高原是我国气候变化启动区的新证据[J].科学通报,1998,43(6):633-636.
[4] 刘晓东,侯萍.青藏高原及其邻近地区近30年气候变暖与海拔高度的关系[J].高原气象,1998,17(3):245-249.
[5] 姚檀栋,刘晓东,王宁练.青藏高原地区的气候变化幅度问题[J].科学通报,2000,45(1):98-106.
[6] 林振耀,赵晰栾.青藏高原气温降水变化的空间特征[J].中国科学(D辑),1996,26(40):354-358.
[7] 杜军,马玉才.西藏高原降水变化趋势的气候分析[J].地理学报,2004,59(3):375-382.
[8] 吴绍洪,尹云鹤,郑度,等.青藏高原近30年气候变化趋势[J].地理学报,2005,60(1):3-11.
[9] 李海东,沈渭寿,邹长新,等.雅鲁藏布江源区土壤侵蚀特征[J].生态与农村环境学报,2010,26(1):25-30.
[10] 樊萍,王得祥,祁如英.黄河源区气候特征及其变化分析[J].青海大学学报:自然科学版,2004,22(1):19-25.
[11] 边巴次仁.西藏气候变暖趋势将进一步加剧[N].西部时报,2009-09-11(02).
[12] 沈渭寿,李海东,张涛,等.西藏高寒风沙化土地飞播可行性分析[J].生态与农村环境学报,2009,25(1):106-111.
[13] Beniston M,Diaz H F,Bradley R S.Climatic change at high elevation sites:an overview[J].Climatic Change,1997,36:233-251.

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备注/Memo

收稿日期:2010-3-11;改回日期:2006-3-1。
基金项目:国家环保公益性行业科研专项（200809010）
作者简介:李海东（1984- ），男，博士生，主要从事水土保持及荒漠化防治、气候变化研究。E-mail：hdli2009@yahoo.com
通讯作者:佘光辉（1953- ），男，教授，博士生导师，主要研究方向为森林资源管理。E-mail：ghshe@njfu.com

更新日期/Last Update: 1900-01-01