Nonstationarity and potential multi-decadal variability in Indian Summer Monsoon Rainfall and Southern Annular Mode teleconnection

被引:3
|
作者
Dwivedi, Suneet [1 ,2 ]
Pandey, Pushpa [1 ,2 ]
Goswami, B. N. [3 ]
机构
[1] Univ Allahabad, K Banerjee Ctr Atmospher & Ocean Studies, Allahabad 211002, Uttar Pradesh, India
[2] Univ Allahabad, MN Saha Ctr Space Studies, Allahabad 211002, Uttar Pradesh, India
[3] Cotton Univ, Dept Phys, Gauhati, India
关键词
Indian Summer Monsoon Rainfall; Southern Annular Mode; Southern Indian Ocean Dipole; Atlantic Multidecadal Oscillation; Indian Monsoon Teleconnection; SEA-SURFACE TEMPERATURE; ARABIAN SEA; SNOW DEPTH; OSCILLATION; DEFINITION; MYSTERY; DIPOLE;
D O I
10.1007/s00382-022-06146-y
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
While the El Nino-Southern Oscillation and Indian Summer Monsoon Rainfall (ISMR) relationship is weak in recent years, a strong correlation between May Southern Annular Mode Index (SAMI) and June-July (JJ) ISMR is a southern hemispheric source of ISMR predictability. Here, using observed and reanalysis data, we find that the SAMI-ISMR relationship is non-stationary with a potential multi-decadal variability. Both during high/low correlation periods (1980-2010)/(1949-1979), a Southern Indian Ocean Dipole (SIOD) pattern of JJ sea surface temperature anomaly is found to reverse sign during strong and weak SAMI years. The changes in the strength and location of the northern pole of SIOD during the two time blocks are consistent with corresponding changes in the cross equatorial flow and monsoon south-westerlies together with change in SAMI-ISMR correlations. Our analysis indicates teleconnection pathways through which the Atlantic Multidecadal Oscillation (AMO) may be responsible for the multi-decadal swings of SAMI-ISMR correlations through modulation of the SIOD.
引用
收藏
页码:671 / 683
页数:13
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