Relationship between Precipitation and Cyclones in the Bay of Bengal India during 2015-2019: Using Tropical Rainfall Measurement Mission (TRMM) 

Authors

  • Anupama Sahoo Department of Atmospheric and Ocean Sciences, Indian Institute of Technology, Bhubaneswar Orissa India -752050, India https://orcid.org/0009-0009-8962-009X
  • Ghulam G. Zahid Department of Atmospheric and Ocean Sciences, Indian Institute of Technology, Bhubaneswar Orissa India -752050, India https://orcid.org/0009-0007-4002-0080
  • Nepal Singh Department of Geology, Aligarh Muslim University Aligarh India -202002, India
  • Usman Aarif Chaudhary Department of Geology, Aligarh Muslim University Aligarh India -202002, India
  • Mohammad Zahbi Faculty of Earth and Environmental Sciences and Engineering, University of Miskolc, Hungary
  • Dr. Ajhar Hussain Department of Geology, Aligarh Muslim University Aligarh India -202002, India https://orcid.org/0009-0008-4336-5997

Keywords:

(BoB) Bay of Bengal, TRMM, tropical cyclone, precipitation, SST

Abstract

The Bay of Bengal (BoB) is a cyclone hotspot as it's warmer than the Arabian Sea. The North Indian Ocean, according to Neumann, was home to 7% of all worldwide Tropical Cyclones (TCs) (NIO). TCS was relatively common in the Bay of Bengal (BoB), accounting for 5% of all worldwide TCs. May, October, and November were the months with the greatest TC activity, while January, April, and July had the weakest TC activity. To evaluate the distribution of TC rainfall throughout an inter-annual and monthly timescale, rainfall data from the Tropical Rainfall Measurement Mission (TRMM) were employed (i.e., how much TC contributed to total rainfall). Using TC best track data from the Indian Meteorological Department, this article initially examined TC activity in this region from 2015 to 2019 (January–December) (IMD). The present study describes the role of cyclones in seasonal rainfall over the period from 2015 to 2019. The precipitation does not depend upon any stage of cyclones, it sometimes peaks higher value at the D stage, sometimes also at its mature stage. The study also concludes that the maximum rainfall does not have to be proportional to the intensity. The rainfall areas of a TC are not proportional to its intensity; Therefore, TC categories with higher intensities do not generate excessive rainfall.

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Published

2024-12-19

How to Cite

Sahoo, A., Zahid, G. G., Singh, N., Aarif Chaudhary, U., Mohammad Zahbi, & Hussain, A. (2024). Relationship between Precipitation and Cyclones in the Bay of Bengal India during 2015-2019: Using Tropical Rainfall Measurement Mission (TRMM) . International Journal of Convergent Research, 1(1 | July - December). Retrieved from https://ijcres.in/index.php/ijcr/article/view/21