1961~2011 年中国降水时空变化特征分析
Analysis of the Characteristics of China Precipitation Changes during 1961-2011
DOI: 10.12677/CCRL.2013.24025, PDF, HTML, XML,  被引量 下载: 3,262  浏览: 11,648 
作者: 高正华*:安徽省淮南市气象局,淮南
关键词: 降水时空变化EOF 分析减少Rainfall; Space-Time Change; EOF Analysis; Reduce
摘要:

利用中国气象局国家气象信息中心 1961~2011 年的中国地面逐月降水量网格数据集,通过数据统计以及 EOF 分解对中国区域 51 年间的降水时空分布特征进行了分析,结果显示:1961~2011 年间,降水量总体上经过了先减少后增加再减少的过程,经历了两次较为明显的低谷,分别为 1963~1973 年以及 2003 年以来;我国降水量从东南向西北递减,在东南沿海地区分布较多,新疆、青海以及甘肃西北部地区降水分布较少,7 月和 10月降水量的高值区出现东南沿海偏内陆地区,出现多个降水大值中心;且在 EOF 分解中第一个主模态全国区域表现为相似的变化特征,我国东南沿海地区的变化特征为主要的变化特征区域;我国东南沿海的降水量变化可主导中国整个区域的降水量变化特征。

Abstract: Statistical and EOF analysis was conducted to investigate the 51 years (from 1961 to 2011) of temporal and spatial distribution of precipitation over China by using monthly gridded precipitation data from the National Meteoro- logical Information Center of China. Generally speaking, from 1961 to 2011, precipitation decreases from 1963 to 1973 then increases until 2003, after then precipitation decreases again. Precipitation amount decreases from the southeast of China to the northwest. Precipitation is more over the southeast coastal area of China, while it is less over Xinjiang, Qinhai and Gansu province. The high value zone of precipitation amount in July and October appears over the southeast coast inland. The first mode of EOF decomposition shows similar variation characteristics over the whole country. Southeast China is the primary variation characteristic area. The precipitation amount variation of Southeast China can dominate the precipitation variation characteristic of the entire country.
文章引用:高正华. 1961~2011 年中国降水时空变化特征分析[J]. 气候变化研究快报, 2013, 2(4): 147-152. http://dx.doi.org/10.12677/CCRL.2013.24025

参考文献

[1] IPCC. Summary for policymakers of the synthesis report of the IPCC fourth assessment report. Cambridge: Cambridge Univer- sity Press, 2007: 2-22.
[2] R. S. Bradly, H. F. Diaz, J. K. Eischeid, et al. Precipitation fluc- tuations over northern hemisphere land areas since the mid-19th century. Science, 1987, 237: 171-175.
[3] M. Hulme. A 1951-80 global land precipitation climatology for the evaluation of general circulation models. Climate Dynam- ics, 1992, 7: 57-72.
[4] 丁一汇, 任国玉, 石广玉等. 气候变化国家评估报告(I): 中国气候变化的历史和未来趋势[J]. 气候变化研究进展, 2006, 2(1): 3-8.
[5] 刘晓冉, 李国平, 范广洲, 程炳岩, 李洪权. 我国西南地区1960~2000年降水资源变化的时空特征[J]. 自然资源学报2007, 22(5): 783-792.
[6] 卢燕宇, 吴必文等. 1961~2005年淮河流域降水时空演变特征分析[A]. 第26届中国气象学会年会气候变化分会场论文集[C], 2009.
[7] 张文纲, 李述训, 庞强强. 青藏高原40年来降水量时空变化趋势[J]. 水科学进展, 2009, 20(2): 168-176.
[8] 南庆红, 杨舵, 杨青. 应用EOF方法分析新疆降水变化特征[J]. 中国沙漠, 2003, 23(5): 554-559.
[9] 刘毅, 何金海等. 近40年重庆地区夏季降水的气候特征[J]. 气象科学, 2005, 25(5): 490-498.