地理学报 ›› 2013, Vol. 68 ›› Issue (1): 82-94.doi: 10.11821/xb201301010
祁威1,2, 张镱锂1, 高俊刚1, 杨续超3, 刘林山1, Narendra Raj KHANAL4
收稿日期:
2012-08-27
修回日期:
2012-10-21
出版日期:
2013-01-20
发布日期:
2013-01-20
通讯作者:
张镱锂(1962-),男,研究员,博导,中国地理学会会员(S110001007M)。E-mail:zhangyl@igsnrr.ac.cn
作者简介:
祁威(1987-),男,博士生,河北涿州人,从事山地与高原综合自然地理研究。E-mail:qiw.12b@igsnrr.ac.cn
基金资助:
全球变化研究国家重大科学研究计划(2010CB951704); 国家自然科学基金项目(40901057)
QI Wei1,2, ZHANG Yili1, GAO Jungang1, YANG Xuchao3, LIU Linshan1, Narendra R. KHANAL4
Received:
2012-08-27
Revised:
2012-10-21
Online:
2013-01-20
Published:
2013-01-20
Supported by:
The National Basic Research Program of China, No.2010CB951704; National Natural Science Foundation of China, No.40901057
摘要: 利用珠穆朗玛峰南坡尼泊尔境内(科西河流域) 的10 个气象站1971-2009 年月平均气温、月平均最高、最低气温和逐月降水资料, 采用线性趋势、Sen 斜率估计、Mann-Kendall 等方法分析区域气候变化状况及其时空特征, 并与珠穆朗玛峰北坡地区气候进行比较, 分析了珠穆朗玛峰地区气候变化的特征与趋势。结果表明:(1) 1971-2009 年间, 珠穆朗玛峰南坡年平均气温为20.0℃, 线性升温率为0.25℃/10a, 与北坡主要受年平均最低气温影响相反, 增幅主要受年平均最高气温升高的影响, 并且在1974 年及1992 年间出现两次显著增温, 增温特别明显的月份为2 月和9 月;(2) 该地区降水变化的局地性较强, 近40 年间年平均降水量为1729.01 mm, 年平均降水量以每年约4.27 mm的线性增幅有所增加, 但并不显著, 且降水月变化和季变化特征均不明显;(3) 由于珠穆朗玛峰南坡受到季风带来暖湿气流和喜马拉雅山阻挡的双重影响, 珠峰南坡的年平均降水量远高于北坡;(4) 珠穆朗玛峰南坡气温变暖的海拔依赖性并不明显, 且南坡地区的变暖趋势并没有北坡变暖趋势明显。
祁威, 张镱锂, 高俊刚, 杨续超, 刘林山, Narendra Raj KHANAL. 1971-2009 年珠穆朗玛峰地区尼泊尔境内气候变化[J]. 地理学报, 2013, 68(1): 82-94.
QI Wei, ZHANG Yili, GAO Jungang, YANG Xuchao, LIU Linshan, Narendra R. KHANAL. Climate change on southern slope of Mt. Qomolangma region in Nepal from 1971 to 2009[J]. Acta Geographica Sinica, 2013, 68(1): 82-94.
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