地理科学进展 ›› 2016, Vol. 35 ›› Issue (3): 331-338.doi: 10.18306/dlkxjz.2016.03.007
收稿日期:
2015-08-01
接受日期:
2015-09-01
出版日期:
2016-03-25
发布日期:
2016-03-25
通讯作者:
郑景云
E-mail:haozx@igsnrr.ac.cn;zhengjy@igsnrr.ac.cn
作者简介:
作者简介:郝志新(1975-),女,内蒙赤峰人,研究员,主要从事气候变化研究,E-mail:
基金资助:
Zhixin HAO1(), Di SUN1,2, Xuezhen ZHANG1, Jingyun ZHENG1,*(
)
Received:
2015-08-01
Accepted:
2015-09-01
Online:
2016-03-25
Published:
2016-03-25
Contact:
Jingyun ZHENG
E-mail:haozx@igsnrr.ac.cn;zhengjy@igsnrr.ac.cn
Supported by:
摘要:
本文根据1901年以来的62次强火山(VEI≥4)喷发年表和英国东安格利亚大学气候研究中心发布的格点气温资料(CRU TS v.3.22),采用时序叠加分析方法,辨识了不同纬度、不同季节强火山喷发对中国温度变化区域差异的影响。结果表明:不同纬度强火山喷发后的1~2年,中国温度基本以下降为主,但降温强度存在显著的区域与季节差异。高纬火山喷发后的显著降温区域发生在东北和东南地区,冬半年温度下降达1.2°C,夏半年温度下降2.0°C;中低纬火山喷发后,冬半年温度的显著下降区域发生在青藏、东南和东中部地区,幅度为1.3~2.2°C,夏半年温度下降幅度比冬半年小;赤道火山喷发后,冬半年温度显著下降区域发生在东北、东南和青藏地区,且降温幅度均大于1.2°C,夏半年西北和东中部地区降温幅度偏小。此外,强火山喷发后第3年,部分地区还出现二次降温现象,降幅甚至超过第一次;然而,同一纬度强火山喷发后,其所造成的降温幅度和降温区域差异与强火山喷发的季节关系不大。
郝志新, 孙迪, 张学珍, 郑景云. 20世纪以来强火山喷发对中国温度变化区域差异的影响[J]. 地理科学进展, 2016, 35(3): 331-338.
Zhixin HAO, Di SUN, Xuezhen ZHANG, Jingyun ZHENG. Regional differences in temperature response in China to the large volcanic eruptions since the 20th century[J]. PROGRESS IN GEOGRAPHY, 2016, 35(3): 331-338.
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