[1]蓝永超,胡兴林,丁宏伟,等.河西内陆河流域山区近50余年来气温变化的多尺度特征和突变分析[J].山地学报,2014,(02):163.
　LAN Yongchao,HU Xinglin,DIN Hongwei,et al.Multiple Time Scales Analysis of Jump and Variation of Air Temperature in Mountain Area of Hexi Inland River Basin in the Past More than 50 Years[J].Mountain Research,2014,(02):163.
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河西内陆河流域山区近50余年来气温变化的多尺度特征和突变分析()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2014年02期
页码:
163
栏目:
山地研究
出版日期:
2014-02-01

文章信息/Info

Title:
Multiple Time Scales Analysis of Jump and Variation of Air Temperature in Mountain Area of Hexi Inland River Basin in the Past More than 50 Years
作者:
蓝永超;胡兴林;丁宏伟;喇承芳;宋洁;邹松兵;尹振良;
1. 中国科学院内陆河流域生态水文重点实验室甘，甘肃 兰州 730000;
2.中国科学院寒区旱区环境与工程研究所，甘肃 兰州 730000;
3.甘肃省水文水资源局，甘肃 兰州 730000；
4.黄委会黄河上游水文水资源局，甘肃 兰州 730000
Author(s):
LAN Yongchao;  HU Xinglin;  DIN Hongwei; LA Chengfang;  SONG Jie; ZOUSongbin; YIN Zhenliang
1. Key Laboratory of Ecohydrology in Inland River Basin, CAS, Lanzhou 730000, China;
2. Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou 　730000, China;
3. Hydrology and Water Resources Bureau of Gansu Province, Lanzhou 730000, China;
4. Hydrology and Water Resources Bureau of the Upper Yellow River Headwater of the 　Yellow River Conservancy Committee, Lanzhou 730030,China
关键词:
青藏高原; 河西内陆河流域; 祁连山区; 三大内陆水系; 气候突变
Keywords:
QinghaiXizang plateau;  Qilian mountain area;  the three large river systems; the Hexi inland river basin;  abrupt change of climate
分类号:
P467，X16
文献标志码:
A
摘要:
基于青藏高原东北部边缘祁连山区及附近有关气象站1960—2011年的气温观测数据,利用线性倾向分析、滑动平均法、Mann-Kendall法等方法,对甘肃河西内陆河流域石羊河、黑河、疏勒河三大水系上游祁连山区气温系列的多尺度变化特征与突变进行了分析。结果表明,近50余年来,该区域气温变化与青藏高原整体的气温变化基本一致,但又有着鲜明的区域差异。具体表现为:三大水系上游山区气温的年代际、年际、各个季节的变化总体上均呈现显著的上升态势,但受区域地理环境的影响,各水系上游山区气温上升的幅度有所不同,气温的气候倾向率总体上呈现出由东向西逐渐增加的趋势。位于祁连山区东部的石羊河上游山区年平均气温突变发生时...
Abstract:
Based on the air temperature observation data of weather stations concerned in the northeast border region of QinghaiXizang Plateau during the period from 1960 to 2011, the multiple time scales characteristics of jump and variation of temperature in mountain area of Hexi inland river basin in the past more than 50 years are analyzed by some Trends and mutation analysis methods such as Linear Trend Analysis, Moving Average Analysis,MannKendall Analysis and Spearman rank analysis and so on. The results showed that the change of temperature in the region is basically the same with the integral QinghaiTibet Plateau, which is showed that all changes of the decadal and interannual and each seasonal change of temperature in the mountains at the upstream of the Shiyang, Heihe and Shule river systems respectively located the eastern, middle and western Qilian mountain area have presenting an observably rising states as a whole. But the rising extents of temperature in the mountains at the upstream of the various river systems are the different because of the influences of different regional geographical environment and climate tendency rate of the temperature in the in the mountains at the upstream of the various river systems present a gradually increase trend from east to west. The abrupt change of annual mean temperature in the upriver watershed of Shiyang river system located in the eastern Qilian mountain area occur in about the mid 1980 s, which is sooner than the late 1990s, the Jump time of temperature in the upriver watershed of Heihe and Shule river systems located in the middle and western Qilian mountain area. But the Jump extent of annual mean temperature in the upriver watershed of Shiyang river system is less than temperature in the upriver watershed of Heihe and Shule river systems and the Jump extent of annual mean temperature in the upriver watershed of Shiyang river system located in western Qilian mountain area is the largest. The 2000 s is the warmest decade in the upriver mountains of three large river systems of Hexi inland region in the past more than 50 years. Compared with the annual mean temperature and other season’s temperature, the rising extent of winter temperature (Nov.-Feb.) in the upriver mountains of every river system is largest, the rising extent of spring temperature (Mar.-May) in the upriver mountains of Heihe and Shule river system are least and the rising extent of summer temperature (June.-Sep.) in the upriver mountains of Shiyang river system is least.

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备注/Memo

备注/Memo:
收稿日期(Received date)：2013-06-12；改回日期(Accepted): 2013-08-10。
基金项目（Foundation item）：国家自然科学基金重大研究计划项目（91225302）和基金面上项目（41240002、91225301）共同资助。［Supported by National Nature Science Foundation of China (No． 9112502,41240002 and 91225301）．］
作者简介（Biography）：蓝永超( 1957- )，男，四川资阳人，研究员、博士生导师，主要从事气候变化、水文水资源等方面的研究工作。［Lan Yongchao，male，research professor，doctoral tutor，mainly engaged the research in hydrology，water and climate change．］E- mail:lyc@lzb.ac.cn;Tel: 0931-4967161
更新日期/Last Update: 1900-01-01