Abstract
Leaving out the strong El Niño Southern Oscillation (ENSO) years, our understanding in the interannual variation of the Indian summer monsoon rainfall (ISMR) stands poor for the rest. This study quantifies the role of ENSO in the preceding winter on ISMR with a particular emphasis on ENSO-neutral summer and La Niña winter. Results show that, unlike the simultaneous ENSO-ISMR relationship, La Niña of previous winter reduces mean rainfall over the country by about 4% even during ENSO neutral summer. Moreover, when ENSO changes phase from La Niña in winter to El Niño in summer, ISMR is anomalously lower than during persisting El Niño years (−14.5% and −5.3%, respectively), increasing the probability of severe drought. This suppression effect of La Niña of the preceding winter on summer monsoon precipitation over India is mostly experienced in its western and southern parts. Principal component analysis of the zonal propagation of surface pressure anomalies from winter to summer along Northern Hemisphere subtropics decomposes interannual variations of seasonally persisting anomalies from zonal propagations. The dominant modes are associated with the seasonal transition of the ENSO phase, and are well correlated with date of onset and seasonal mean rainfall of monsoon over India. These results improve our understanding of the interannual variations of ISMR and could be used for diagnostics of general circulation models.
Highlights
The interannual variation of Indian summer monsoon rainfall (ISMR) bears crucial socio-economic values to the country of teeming millions [1, 2]
If N34SST is less than −0.5◦C, we identify that season as La Niña (El Niño), the rest being El Niñ o Southern Oscillation (ENSO) neutral
We focus on years of ENSO neutral summer since interannual variations of ISMR during those years are least understood
Summary
The interannual variation of Indian summer monsoon rainfall (ISMR) bears crucial socio-economic values to the country of teeming millions [1, 2]. It is known that the El Niño Southern Oscillation (ENSO) impacts ISMR by controlling the strength and position of this circulation [10, 11]. ENSO could impact ISMR through modulation of the stationary Rossby wave of the midlatitude [12, 13]. The strength of Indian monsoon in summer (weak or strong) skews the probability of development of El Niño or La Niña in the following winter [14, 15]. Such interactions have associated time scales that control the lagged response between components of the system
Published Version
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