This process can lead to the formation of NIDW (Figure B-32), particularly in 

 the region south of about 5° S. latitude and east of about 80° E. longitude 

 (also see Figure C-5). As noted by Rochford, 1966a, the preferential westward 

 flow of BIW is along or south of 10° S. latitude, particularly in the region west 

 of the Chagos Archipelago. 



94 



