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中国天山山区235 a气候变化及降水趋势预测
引用本文:魏文寿,袁玉江,喻树龙,张瑞波.中国天山山区235 a气候变化及降水趋势预测[J].中国沙漠,2008,28(5):803-808.
作者姓名:魏文寿  袁玉江  喻树龙  张瑞波
作者单位:中国气象局乌鲁木齐沙漠气象研究所,新疆,乌鲁木齐,830002;中国气象局树木年轮理化研究重点开放实验室,新疆,乌鲁木齐,830002
基金项目:公益性行业(气象)科研专项,科技部社会公益研究项目,科技基础性工作专项项目,中国气象局重点实验室开放研究项目
摘    要:  利用4个降水重建序列与天山山区10个气象站降水变化的响应关系,重建了天山山区近235 a来气候变化的年降水序列,重建序列的方差解释量达到47.7%。对过去235 a天山山区气候变化中降水变化的特征分析发现:降水大致经历了7干7湿的变化阶段,其中偏湿年份为124 a,多于偏干年份;天山山区的降水量以2.1 a、3.0 a、5.8 a、6.0 a的高频变化和24~25 a的低频变化周期最为显著。研究表明,近百年天山山区气候变化中的降水变化分为两个阶段,20世纪初到80年代,降水量逐渐减少,导致冰川退缩、河流径流量减少、湖泊萎缩、沙漠面积增大、植被覆盖率减少;80年代后期至今,降水量迅速增加,导致河川径流量增加、湖泊面积增大和沙尘暴日数减少,生态环境趋于好转,但同时造成洪水和地质灾害频繁。采用基于方差分析的周期叠加方法对天山山区未来23 a气候变化中降水的演变趋势进行预测,结果表明:未来23 a气候变化中天山山区以湿润为主,期间有部分年份可能较常年干旱。

关 键 词:天山山区  气候变化  树木年轮  降水  趋势预测
收稿时间:2007-10-25
修稿时间:2007-12-10

Climate Change in Recent 235 Years and Trend Prediction in Tianshan Mountainous Area
WEI Wen-shou,YUAN Yu-jiang,YU Shu-long,ZHANG Rui-bo.Climate Change in Recent 235 Years and Trend Prediction in Tianshan Mountainous Area[J].Journal of Desert Research,2008,28(5):803-808.
Authors:WEI Wen-shou  YUAN Yu-jiang  YU Shu-long  ZHANG Rui-bo
Institution:1.Institute of Desert and Meteorology, China Meteorological Administration, Urumqi 830002, China; 2.Key Laboratory of Tree-ring Physical and Chemical Research of China Meteorological Administration, Urumqi 830002, China
Abstract:Four reconstructed precipitation sequences and their relations responding to precipitation variation of ten weather stations in Tianshan mountainous area are applied to reconstruct the precipitation sequence in recent 235 years in Tianshan mountainous area. The explained variance of reconstructed sequence can reach up to 47.7%. The analyses on the precipitation change characters in recent 235 years in Tianshan mountainous area disclose that the 235-year precipitation process can be interpreted as 7 wet periods and 7 dry periods, totaling up to 124 years wet-year and 111 years dry-year. The reconstructed precipitation sequence shows remarkable high-frequency change cycles of 2.1 years, 3.0 years, 5.8 years, and 6.0 years, also a low-frequency change cycle of 24 to 25 years. Over the past one hundred years, the precipitation change in Tianshan mountainous area can be divided into two stages: from early 1900's to 1980's, precipitation gradually reduced, glaciers retreated, river runoff decreased, lake shrank, desert area increased and vegetation cover reduced; from late 1980's on, precipitation rapidly increased, consequently river runoff and lake area increased, sandstorm frequency reduced, the ecological environment improved, but simultaneously floods and geologic disasters frequently broke out. By the cycle superposition method that based on the variance analysis it is predicted that the climate change in future 23 years in Tianshan mountains area will be characterized by humid feature, totaling 14 years or 61 percent, possibly there will be several more drought years than the normal.
Keywords:Tianshan mountainous area  climate change  tree-ring  precipitation  trend prediction
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