地理学报 ›› 2022, Vol. 77 ›› Issue (5): 1120-1137.doi: 10.11821/dlxb202205006
收稿日期:
2021-02-03
修回日期:
2022-04-11
出版日期:
2022-05-25
发布日期:
2022-07-25
通讯作者:
巩远发(1963-), 男, 博士, 教授, 主要从事短期气候异常变化的诊断和模拟研究。E-mail: gyfa@cuit.edu.cn作者简介:
谭政华(1991-), 男, 辽宁朝阳人, 硕士, 工程师, 主要从事天气动力学和短期气候预测研究。E-mail: ln-tanzhenghua@outlook.com
基金资助:
TAN Zhenghua1,2,3(), GONG Yuanfa2(
)
Received:
2021-02-03
Revised:
2022-04-11
Published:
2022-05-25
Online:
2022-07-25
Supported by:
摘要:
本文使用1961—2016年NCEP1再分析资料和GPCC全球降水分析资料,确定了亚洲夏季风北部边缘带的空间范围,分析了季风边缘带的南北边界位置、降水、面积的相互关系和年代/际变化特征,讨论了造成季风边缘带夏季降水异常的影响因子。主要结论如下:亚洲夏季风北部边缘带平均位置位于青藏高原中部经黄土高原和中国东北地区向亚洲东岸延伸的带状区域上,根据下垫面性质、区域生态环境和气候特征,将季风北边缘带划分为青藏高原区(85°E~105°E)、黄土高原区(105°E~115°E)和中国东北区(115°E~135°E)3段,季风边缘带降水的年际变化与其南边界位置有显著的正相关,青藏高原季风边缘带面积变化与其南界位置显著负相关,黄土高原季风边缘带和东北季风边缘带面积与北边界位置显著正相关,且3段季风边缘带的位置、面积、降水均有明显的年际、年代际变化特征。季风边缘带夏季降水偏少与欧亚中高纬对流层上层自西向东传播的欧亚(EU)遥相关波列密切相关,季风边缘带夏季降水偏少时期,亚洲低纬度地区对流活动偏弱、非洲东岸近赤道地区200 hPa异常辐合可能造成索马里急流和亚洲夏季风强度整体偏弱,200 hPa亚洲急流强度弱且位置偏北,500 hPa中国北方受西风带异常高压控制,东亚夏季风降水主要集中在中国南方地区,季风边缘带夏季降水异常偏少。季风边缘带夏季降水偏多与欧亚中高纬对流层上层沿亚洲急流向东传播的丝绸之路(SRP)波列密切相关,200 hPa、500 hPa环流形势与季风边缘带夏季降水偏少时期基本相反,东亚夏季风降水空间分布呈北多南少特征,季风边缘带夏季降水异常偏多。
谭政华, 巩远发. 亚洲夏季风北部边缘带变化及中高纬度行星波对其影响[J]. 地理学报, 2022, 77(5): 1120-1137.
TAN Zhenghua, GONG Yuanfa. Characteristics of the northern marginal zone of the Asian summer monsoon and the influence of planetary waves in middle-high latitudes on its variation[J]. Acta Geographica Sinica, 2022, 77(5): 1120-1137.
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