Dynamics of Orographic Rainfall for mountain corner over north-east India

Authors

  • Prasanta Das Department of Mathematics, Ramananda College, Bishnupur, Bankura, W.B., India
  • Somenath Dutta India Meteorological Department (IMD), Pune, India

DOI:

https://doi.org/10.54302/mausam.v76i3.6220

Keywords:

RFI, CMH, SWMS, Gridded rainfall data

Abstract

In north-east India, the Corner Mountain is an almost right angled corner, which is made between the Khasi-Jayantia hills (KJH) & the Assam-Burma hills (ABH). In this paper, has been made to analysis the effects of orographic rainfall during the south west monsoon season (SWMS) over the north-east region of India, in a baroclinic mean flow. To construct this model a 3-D laminar, non-viscous, adiabatic, Boussinesq & non rotational moist airflow has been considered. The basic flow has two components, zonal wind U(z) and meridional wind V(z) and the Brunt-Väisälä frequency (N) is taken to be variant with height. The non-linear governing equations of the airflow are linearized by using the perturbation technique. To compute the rainfall intensity (RFI), the vertical velocity ( ) is obtained by quasi-numerical approach. In this study, two selective dates has been considered and all results have compared to the earlier researchers. 

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Published

01-07-2025

How to Cite

[1]
P. Das and S. Dutta, “Dynamics of Orographic Rainfall for mountain corner over north-east India”, MAUSAM, vol. 76, no. 3, pp. 934–941, Jul. 2025.

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