Intra-seasonal oscillations were observed in the meteorological and oceanog
raphic fields of Bay of Bengal during the summer monsoon season of 1999. Sp
ectral analysis revealed prominent peaks in the intra-seasonal (10 to 32 da
ys), inertial (2.2 days), diurnal and semi-diurnal bands. Oscillation of in
traseasonal periodicity significantly influences the circulation pattern, T
he variations in oceanographic fields were dominated by remote forcing comp
ared to local forcing.