Variations of Energy Fluxes with ENSO, IOD and ISV of Indian Summer Monsoon Rainfall over the Indian Monsoon Region

被引:2
|
作者
Bal, Prasanta Kumar [1 ,2 ]
Dasari, Hari Prasad [3 ]
Prasad, Narayan [4 ]
Salunke, Popat [1 ]
Parihar, Ruchi Singh [1 ,5 ]
机构
[1] Indian Inst Technol Delhi, Ctr Atmospher Sci, New Delhi, India
[2] Civil Aviat Author, Qatar Meteorol Dept, Doha, Qatar
[3] King Abdullah Univ Sci & Technol, Phys Sci & Engn Div, Thuwal, Saudi Arabia
[4] Dayalbagh Educ Inst, Fac Mech Engn, Agra, Uttar Pradesh, India
[5] Graph Era Deemed Univ, Dehra Dun, Uttarakhand, India
关键词
ENSO; Indian Ocean Dipole; Energy budget; Indian summer monsoon; OCEANIC HEAT-BUDGET; EL-NINO; INTERANNUAL VARIABILITY; RADIATION; FEATURES; DYNAMICS; PLATEAU; DIPOLE; IMPACT; LAYER;
D O I
10.1016/j.atmosres.2021.105645
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Variations of energy fluxes with ENSO, IOD, and Intra-Seasonal Variability of Indian Summer Monsoon Rainfall (ISMR) over the Indian monsoon region are examined using ECMWF Era Interim reanalysis over a period of 1979-2013. The composite anomalies of radiative fluxes, viz. shortwave and longwave, latent, and sensible heat as well as precipitation and winds are analyzed for the years associated with El Nin & tilde;o, La Nin & tilde;a, positive and negative IOD phases, active, and break phases of ISMR with respect to the normal years. It is observed that, the lesser (more) precipitation over the region in the El Nin & tilde;o (La Nin & tilde;a) years is accompanied with enhanced (reduced) top of the atmosphere absorbed solar radiation and outgoing long wave radiation, as well as more (less) surface absorbed solar radiation, and surface sensible heat flux. During the positive IOD phase, enhanced convective activity and precipitation rainfall over the western Equatorial Indian Ocean, Arabian Sea, and west coast of India, with reduced rainfall over the eastern equatorial Indian ocean is accompanied with enhanced shortwave and long wave radiative fluxes over most parts of the Indian subcontinent. The conditions during the negative IOD phases are largely the opposite.
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页数:12
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