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过去500年印度夏季风降水与ENSO的关系
引用本文:李方腾,刘飞,柴静. 过去500年印度夏季风降水与ENSO的关系[J]. 大气科学学报, 2021, 44(4): 558-572
作者姓名:李方腾  刘飞  柴静
作者单位:南京信息工程大学气候动力学中心,江苏南京210044;国家海洋环境预报中心海洋气象预报室,北京100081;南京信息工程大学气候动力学中心,江苏南京210044
基金项目:国家自然科学基金资助项目(41975107)
摘    要:为了研究大尺度背景场对ENSO和印度夏季风降水关系的调制作用,更好地预报气候变暖背景下印度夏季风降水的年际变化,本文利用重建的10套ENSO指数和印度降水资料,研究了ENSO和印度夏季风降水在过去500 a(1470-1999年)中的关系,其存在的原因以及如何理解这一现象,主要侧重于ENSO对印度夏季风的影响.结果 表...

关 键 词:印度夏季风  降水  ENSO
收稿时间:2017-11-23
修稿时间:2018-03-21

Relationship between Indian summer monsoon precipitation and ENSO in the past 500 years
LI Fangteng,LIU Fei,CHAI Jing. Relationship between Indian summer monsoon precipitation and ENSO in the past 500 years[J]. Transactions of Atmospheric Sciences, 2021, 44(4): 558-572
Authors:LI Fangteng  LIU Fei  CHAI Jing
Affiliation:Center of Climate Dynamics, Nanjing University of Information Science and Technology, Nanjing 210044, China;Marine Meteorological Forecasting Office, National Marine Environmental Forecasting Center, Beijing 100081, China
Abstract:In order to study the modulation effect of large-scale background field on the relationship between ENSO and Indian summer monsoon precipitation, and to better predict the interannual variation of Indian summer monsoon precipitation under the climate warming background, this paper studies the relationship between ENSO and Indian summer monsoon precipitation in the past 500 years based on ten sets of reconstructed ENSO indices and Indian precipitation data, the reasons for its existence and how to understand this phenomenon.This paper mainly focuses on the influence of ENSO on Indian summer monsoon.Results show that, firstly, the relationship between ENSO and Indian summer monsoon precipitation is not immutable in the past 500 years (1470-1999), generally shows a negative correlation.The negative correlation is weak during Little Ice Age (LIA) and strengthened during Current Warm Period (CWP), but begins to weaken after the 1980s.Secondly, the relationship between Indian summer monsoon precipitation anomaly and ENSO in the past 500 years is certain, not random.Thirdly, the relationship between the Indian summer monsoon precipitation anomaly and the amplitude and cycle of Niño indices are very different during LIA and CWP.The amplitude and cycle of ENSO during CWP are significantly larger than those during LIA, which leads to a stronger negative correlation between Indian summer monsoon and ENSO during CWP.But the average states of the two periods are almost same.
Keywords:Indian summer monsoon  precipitation  ENSO
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