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Table 2 Relative contributions of vapor source regions to precipitation for each season

From: Seasonal variation in isotopic composition and the origin of precipitation over Bangladesh

  LND BOB ARS NID SID PAC
Pre-monsoon Sylhet 10% 34% 26% 11%   
Dhaka   36% 24% 13%   
Chittagong   28% 21% 15%   
Indian Summer Monsoon Sylhet 19% 23% 16% 15% 14%  
Dhaka 10% 20% 16% 13% 13%  
Chittagong   22% 16% 15% 15%  
Post-monsoon Sylhet 24% 12%     37%
Dhaka 19% 18%     26%
Chittagong 20% 11%     29%
  1. Values less than 10% were omitted. LND land surface (the recycling of water), BOB the Bay of Bengal, ARS the Arabian Sea, NID the northern part of the Indian Ocean, SID the southern part of the Indian Ocean, PAC the Pacific Ocean