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三峡库区近百年来气温变化特征
引用本文:张天宇,陈正洪,孙佳,程炳岩,任永建,张建平.三峡库区近百年来气温变化特征[J].长江流域资源与环境,2012,21(Z2):110-144.
作者姓名:张天宇  陈正洪  孙佳  程炳岩  任永建  张建平
作者单位:(1.重庆市气候中心,重庆 401147; 2.中国气象局武汉暴雨研究所, 湖北 武汉 430074;3.武汉区域气候中心, 湖北 武汉 430074; 4.重庆市气象科学研究所, 重庆 401147
基金项目:中国气象局气候变化专项(CCSF201220);三峡工程环境保护补偿经费(SX2009-004);国际科技合作项目(2010DFA21340)共同资助
摘    要:利用1924~2011年重庆和宜昌站气温资料,分析了三峡库区近百年来气温变化特征。结果表明:从线性趋势、年代变化、突变和周期分析表明近88 a重庆和宜昌气温的变化特征是比较一致的,两段显著偏暖的时期分别是20世纪20年代中期至40年代和20世纪90年代中期至今。用重庆和宜昌站的平均来代表三峡库区,库区气温阶段变化与重庆、宜昌站基本一致,20世纪90年代中后期至今出现的显著增温现象迟于我国1986年前后开始的普遍增温。库区各季节气温变化存在差异,4个季节最近一次增暖主要集中在20世纪90年代中期或中后期。近88 a来三峡库区年平均气温发生两次突变, 1947年左右突变为降温趋势; 1996年左右突变为增暖趋势。三峡库区年平均气温2~4a周期变化最为显著,4 a左右的周期1980年代后期开始显著。1920年代到1980年代存在的16~20 a的年代际周期,但能量较年际周期弱。近88 a三峡库区与全球气温变化存在较大差异,最近一次显著增暖时间比较,三峡库区比全球滞后约10 a

关 键 词:三峡库区  重庆  宜昌  气温变化

VARIATION CHARACTERISTICS OF TEMPERATURE IN THE THREE GORGES RESERVOIR AREA DURING THE PAST NEARLY 100 YEARS
ZHANG Tian-yu,CHEN Zheng-hong,SUN Jia,CHENG Bing-yan,REN Yong-jian,ZHANG Jian-ping.VARIATION CHARACTERISTICS OF TEMPERATURE IN THE THREE GORGES RESERVOIR AREA DURING THE PAST NEARLY 100 YEARS[J].Resources and Environment in the Yangtza Basin,2012,21(Z2):110-144.
Authors:ZHANG Tian-yu  CHEN Zheng-hong  SUN Jia  CHENG Bing-yan  REN Yong-jian  ZHANG Jian-ping
Institution:(1.Chongqing Climate Center, Chongqing 401147, China|2.Wuhan Heavy Rain Institute of China Meteorological Administration, Wuhan 430074,China|3.Wuhan Climate Center, Wuhan 430074, China4.Chongqing Institute of Meteorological Sciences,Chongqing 401147, China)〖
Abstract:By using the temperature data of the Chongqing and Yichang station(from 1924 to 2011),the variation characteristics of temperature in the Three Georges Reservoir Area during the past 88 years were analyzed.The results demonstrated that the linear trend,decadal variation,sudden change and the cycle analysis showed that the temperature changing characteristics of Chongqing station and Yichang were highly same in the last 88 years,and the two significantly warmer periods were the mid 1920s to the 1940s and the mid 1990s to the present.The Three Gorges Reservoir area could be represented by the average values of Chongqing and Yichang,and the temperature change in phases of the reservoir area was basically same with Chongqing,Yichang.The significant warming phenomenon appeared since the late 1990s was later than the China average warming stared at the year around 1986.The seasonal temperature changes had some differences,the latest warming of the four seasons mainly concentrated in periods of the mid 1990s and later 1990s.There were two sudden changes of the temperature in Three Gorges Reservoir area during the recent 88 years:one was a cooling trend around the year 1947,one was a warming trend around 1996.The 2-4 years cycle changes of the average temperature was the most significant,while the 4 years cycle changes were becoming very significant since the later 1980s.There was a 16-20 years decadal period between the 1920s and the 1980s,but its energy was weaker than the annual period.The Three Gorges Reservoir area temperature changes were different with the global temperature changes during the past 88 years.Compared the latest significant warming time,the temperature change in Three Gorges Reservoir Area was about 10 years behind the global temperature change.〖
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