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Progress in Earth and Planetary Science

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
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