Extensive observations made in the central and eastern Arabian Sea und
er JGOFS (India) programme suggest strong seasonal variations in conce
ntrations of oxygen and nutrients in the water column. In the intermed
iate waters (depth range 150-800 m) oxygen concentrations were lowest
during winter (with values near zero at similar to 400 m) in relation
to those in the other two seasons (intermonsoon and southwest monsoon)
. This together with nitrate distributions revealed the occurrence of
intense reducing conditions in intermediate waters during winter becau
se of the sluggish water movement and high surface productivity, Secon
dary nitrite, an indicator of occurrence of denitrification was presen
t at oxygen levels < 10 mu M. Nitrate deficits reached a maximum of 10
mu M in winter, whereas, it was half this value in monsoon, The avera
ge deficits suggest increasing reducing conditions in the order monsoo
n (1.6 mu M), intermonsoon (3.7 mu M) and winter (4.0 mu M).