The Role of Tropical Easterly Jet on the Bay of Bengal’s Tropical Cyclones: Observed Climatology and Future Projection
Autor: | Abdullah A. Fahad, Oreste Reale, Andrea Molod, Tahmidul Azom Sany, Md Tashin Ahammad, Dimitris Menemenlis |
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Rok vydání: | 2023 |
Předmět: | |
Zdroj: | Journal of Climate. :1-34 |
ISSN: | 1520-0442 0894-8755 |
DOI: | 10.1175/jcli-d-22-0804.1 |
Popis: | Tropical cyclones (TCs) in the Bay of Bengal (BoB) are among the most devastating events in nature, significantly influencing human life. They affect the region between April and December, being separated into two distinct phases: the pre-monsoon (April-May-June, AMJ) and post-monsoon (October-November-December, OND), with little activity during the monsoon peak. In this article, the influence of the Tropical Easterly Jet (TEJ) on the observed BoB TC activity, and the expected changes under global warming conditions, are investigated using reanalyses and coupled model intercomparison project 6 (CMIP6) models. The general assumption is that TC activity should increase in response to warmer sea surface temperature (SST). However, several dynamical processes are needed to create organized convection, which is a prerequisite for TC development. The results show that the frequency and accumulated energy should decrease in the future (2020-2049), compared to the historical climate (1950-1979), during both phases. The change of the mean TEJ and intermittent shear relaxations in the future climate are found to play a major role in the change of TC activity. During AMJ, a southward shift of the mean TEJ and TEJ intermittent shear relaxations are associated with reduced TC activity. During OND, the decrease of the frequency of TEJ and Subtropical Jet (STJ) intermittent shear relaxations are associated with the reduction of TC activity. The increase in SST in the future seems to play a minor role. This study clarifies the importance of both the mean and intermittency of the TEJ in determining the future of TC activity in the BoB. |
Databáze: | OpenAIRE |
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