全球变暖情景下中国气温分区的未来变化
首发时间:2009-04-06
摘要:利用SRES A2情景下IPCC AR4的13个模式资料,结合我国平均温度观测资料对当前和未来我国气温的分区进行对比研究,发现1961-1990a、2021-2050a和2071-209a三个时段年平均气温分区在我国西部变化不大,而在我国东部发生了显著变化,在1961-1990a我国东部被华北分区带分为南、北两个区,在2021-2050a由于1961-1990a间的华北分区带北移,而在两广以北同时出现另一分区带,使得该时段我国东部分成东北区、华北和华中区以及华南区三个区,在2071-1097a年北方分区带消失,而南方的分区带北移至长江一带,使得该时段我国东部仍可分为南、北两区。通过比较三个时段不同分区年平均温度时间变化发现,导致分区变化的原因主要是由于在不同时段各分区年平均温度的变率和增温幅度不一致所致。
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Temperature subarea change in the future under the warming scenarios in China
Abstract:Using the outputs of thirteen IPCC AR4 CGCMS under SRES A2 condition and the daily mean temperature data from 548 stations for the period 1961-1990 in China ,evaluated the division of the temperature of china in the future. The mean temperature division in west of China almost retains the same for the period of 1961-1990a、2021-2050a and 2071- 2097a,however,in east of china,it represents remarkable transformation.For the period of 1961-1990a, the west of China can be divided into southern and northern districts by North China division belt.For the period of 2021-2050a,the North China division belt moves northward,meanwhile,another division belt appears to the north of Guangdong and Guangxi province, so in this period ,the east of China can be divided into three districts--northeast, north and central,south of China. For the period of 2071-2097a,the North China division belt disappears,the south China division belt moves northward to Changjiang River, the west of China can be divided into southern and northern districts.By comparing the different division of China for these three periods,found the main reason of the difference is the disagreement between the variability of the mean temperature data and the temperature range of warming up.
Keywords: Air temperature future scenarios subarea change
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No.3109645750612389****
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