Hareeshkumar, P V; Dr.Basil, Mathew(Cochin University of Science And Technology, January , 1992)
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Abstract:
The Arabian Sea is an area of complex air-sea interaction
processes with seasonal reversing monsoons. The associated
thermohaline variability in the upper layers appears to
control the large scale monsoon flow which is not yet
completely understood.
The variability in the thermohaline fields is known to
occur in temporal domain ranging from intra-diurnal to
inter-annual time scales and on spatial domains of few tens of
kilometers to few thousands of kilometers. In the Arabian Sea
though the surface temperature was routinely measured by both
conventional measurements and satellites, the corresponding
information on the subsurface thermohaline field is very
sparse due to the lack cw adequate measurements. In such
cases the numerical models offer promise in providing
information on the subsurface features given an initial
thermohaline field and surface heat flux boundary conditions.
This thesis is an outcome of investigations carried out
on the various aspects of the thermohaline variability on
different time scales. In addition to the description of the
mean annual cycle. the one dimensional numerical models of
Miller (1976) and Price et a1 (1986) are utilised to simulate
the observed mixed layer characteristics at selected locations
in the Arabian Sea on time scales ranging from intra-diurnal
to synoptic scales under variable atmospheric forcing.