地理科学 ›› 2011, Vol. 31 ›› Issue (4): 401-407.doi: 10.13249/j.cnki.sgs.2011.04.401
刘敬华1,2, 张平中2, 孟彩红3, 张德忠2, 杨勋林4
收稿日期:
2010-06-10
修回日期:
2010-09-16
出版日期:
2011-04-20
发布日期:
2011-04-20
基金资助:
LIU Jing-hua1,2, ZHANG Ping-zhong2, MENG Cai-hong3, ZHANG De-zhong2, YANG Xun-lin4
Received:
2010-06-10
Revised:
2010-09-16
Online:
2011-04-20
Published:
2011-04-20
摘要: 基于武都万象洞高分辨率石笋δ18O和高精度230Th定年数据,结合利用周边地区史料恢复的旱涝指数序列,重建季风区边缘近500 a以来降水变化。结果显示:在年际至百年时间尺度上,万象洞石笋δ18O变化指示亚洲季风带来的降水量信息。季风区边缘降水变化可分减弱期(1470~1700 A.D.)、平稳期(1701~1875 A.D.)和增强期(1876~2003 A.D.)三个气候段,其间季风降水的强弱变化响应史料记载的极端旱涝事件。在小冰期向20世纪暖期转换过程中,本区呈现阶梯式过渡降水模式,这是一种较大空间尺度上气候特征,在年代际至百年时间尺度上与北半球温度、中国温度变化具有同步性。
中图分类号:
刘敬华, 张平中, 孟彩红, 张德忠, 杨勋林. 季风区边缘近500年的降水变化特征[J]. 地理科学, 2011, 31(4): 401-407.
LIU Jing-hua, ZHANG Ping-zhong, MENG Cai-hong, ZHANG De-zhong, YANG Xun-lin. A Comprehensive Study on Precipitation Change Over Monsoon Marginal Areas During Last Five Centuries[J]. SCIENTIA GEOGRAPHICA SINICA, 2011, 31(4): 401-407.
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