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青海湖流域近50年气温、降水变化特征研究
引用本文:曹生奎,曹广超,陈克龙,解家安,朱锦福,王记明.青海湖流域近50年气温、降水变化特征研究[J].青海师范大学学报(自然科学版),2013,29(2):37-41,47.
作者姓名:曹生奎  曹广超  陈克龙  解家安  朱锦福  王记明
作者单位:1. 青海师范大学生命与地理科学学院,青海西宁810008;青海师范大学青海省自然地理与环境过程重点实验室,青海西宁810008;中国科学院寒区旱区环境与工程研究所,甘肃兰州 730000
2. 青海师范大学生命与地理科学学院,青海西宁810008;青海师范大学青海省自然地理与环境过程重点实验室,青海西宁810008
3. 青海师范大学生命与地理科学学院,青海西宁,810008
基金项目:国家自然基金,国家社科基金,教育部重点项目(2012178)中科院"西部之光"项目和青海师范大学科技创新计划项目共同资助
摘    要:本文对青海湖流域1961-2010年近50年来的气温和降水变化特征进行了研究,结果表明,青海湖流域气温呈明显的增加趋势,线性增温率最大达到0.40℃/10a;存在较为明显的4次增温期,特别是最近一次增温期,持续时间长,最大增幅达0.1℃/a.降水量虽然没有明显的增加趋势,但存在三次明显的增多期,最大降水量出现在1988-1989年间.在季节变化上,气温均出现了不同程度的增加趋势,尤其以冬季和秋季增温趋势最明显;降水的季节增幅不明显,降水主要集中夏季,夏季多年平均降水量为239.30mm,占全年降水量的65%左右.近50年气温、降水变化特征表明青海湖流域目前正处于增温增湿阶段.

关 键 词:气温  降水量  变化  青海湖流域

Research in the variation characteristics of temperature and precipitation for lately 50 years in the Qinghai Lake basin
CAO Sheng-kui , CAO Guang-chao , CHEN Ke-long , XIE Jia-an , ZHU Jin-fu , WANG Ji-ming.Research in the variation characteristics of temperature and precipitation for lately 50 years in the Qinghai Lake basin[J].Journal of Qinghai Normal University(Natural Science Edition),2013,29(2):37-41,47.
Authors:CAO Sheng-kui  CAO Guang-chao  CHEN Ke-long  XIE Jia-an  ZHU Jin-fu  WANG Ji-ming
Institution:CAO Sheng-kui'2'3 ,CAO Guang-chao'2 , CHEN Ke-long' ,XIE Jia-an1'2 , (1. College of 2. Qinghai ZHUJin-fu1 ,WANG Ji-mi Life and Geography Science, Qinghai Normal ng U niversity, Xining 810008, China Province Key Laboratory of Physical Geography and Environmental process, Qinghai Normal University, Xining 810008, China; 3. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China)
Abstract:This paper has made a research about variation characteristics of temperature and precipitati- on from 1961 to 2010 years in the Qinghai Lake basin. The results showed that there emerged an increas- ing trend in the temperature, with the maximum linear rate of 0.40℃/10a. And there appeared four obvi- ous increasing temperature periods, especially the time of the recent warming period is very long and the maximum increase is 0.1℃/a. Although precipitation has no obvious increasing trend, there existed in three significant increase periods. Maximum precipitation appeared from 1988 to 1989 years. For the seasonal change, the temperature presented different increasing trends. There was especially obvi- ous increase in winter and autumn. The increase of seasonal precipitation is not obvious, and it mainly con- centrated in summer with the multi--year average rainfall of 239.30mm,accounting for about 65~ of the annual precipitation. The characteristics of temperature and precipitation change during recently 50 years indicated that there is being in an increasing stage of the temperature and precipitation in the Qinghai Lake basin at the present.
Keywords:temperature  precipitation  change  Qinghai Lake basin
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