Journal
INTERNATIONAL JOURNAL OF CLIMATOLOGY
Volume 41, Issue 13, Pages 6017-6030Publisher
WILEY
DOI: 10.1002/joc.7165
Keywords
Asian jet-stream; north India; sea surface temperature; subsidence; summer monsoon; tropospheric wind shear
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Funding
- IITM
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The study reveals the pathway of equatorial central Pacific sea surface temperature affecting summer rainfall in north India. This influence strengthens the Asian subtropical westerly jet-stream, leading to restricted convective activities in north India due to strong wind shear.
The summer monsoon season contributes about 80% of annual rainfall in the highly populated region of north India. The teleconnections moderating the variation of summer monsoon rainfall in this region are not satisfactorily understood. A pathway of the equatorial central Pacific sea surface temperature (PSST) influences the north India summer rainfall is revealed from the high-resolution, more reliable, and state-of-the-art 41-year (1979-2019) observational data analysis and numerical experiment. The rise in PSST intensifies convection over the equatorial central Pacific with compensatory subsidence over the western equatorial Pacific. Consequently, a much broader and intense anomalous convergence is developed at the upper-troposphere, which subsequently intensifies the Asian subtropical westerly jet-stream. The Asian jet intensification strengthens the tropospheric wind shear at north India, as the low-level monsoonal winds are easterlies over there. The strong wind shear restricts the convective activities in north India. These results are also confirmed using the CFSv2 model sensitivity experiment and a case study of the year 2010.
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