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• W4387614056 endingPage "107050" @default.
• W4387614056 startingPage "107050" @default.
• W4387614056 abstract "The Indian Ocean basin has undergone significant changes over the past two decades, and this study examines major shifts in the onset characteristics of the Indian Summer Monsoon (ISM) in response to changes in the dynamical and thermodynamic conditions. A thermodynamic index shows that the post-2000 period witnesses an approximately 3-day earlier (May 27) onset of ISM than the pre-2000 period. In the absence of an abrupt and distinct change from the dry to the wet season, the post-2000 era can be distinguished by its early and longer onset process. The Subtropical Indian Ocean Dipole (SIOD) undergoes a phase change during its evolution, which weakens the Mascarene High (MH) and hence the pressure gradient.. The weakening of the MH along with the heterogeneity in SST trends have led to a weaker meridional pressure gradient over the Indian monsoon domain, resulting in a weak onset of the ISM. Additionally, warming in the Arabian Sea starts earlier than expected. The prolonged duration of the Indian Summer Monsoon (ISM) onset process in the post-2000 era can be attributed to several factors. These include the broader ascending limb of the Hadley cell over the south equatorial Indian Ocean, reduced wind shear, and the early development of a warmer Arabian Sea prior to the onset of the monsoon." @default.
• W4387614056 created "2023-10-14" @default.
• W4387614056 creator A5050132872 @default.
• W4387614056 creator A5073542508 @default.
• W4387614056 creator A5088313962 @default.
• W4387614056 date "2023-10-01" @default.
• W4387614056 modified "2023-10-16" @default.
• W4387614056 title "Paradigm shift in the onset phase of the Indian Summer Monsoon since 2000 and its potential connection to South Indian Ocean" @default.
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• W4387614056 doi "https://doi.org/10.1016/j.atmosres.2023.107050" @default.
• W4387614056 hasPublicationYear "2023" @default.
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