Timely and accurate prediction of the cyclone
life cycle from genesis to dissipation is a challenging scientific problem.
Though solutions from numerical models have resolved many complex physical processes
responsible for cyclone formation, development and dissipation, many issues are to be unfolded.
Thus, in addition to improving the understanding of the physics
of the problem, critical examination of input parameters that are used in the
numerical models is also important. Along with a number of atmospheric
parameters, Sea Surface Temperature (SST) is the only oceanographic parameter
used in the models for cyclone prediction. However, cyclones interact with the
upper layer of the ocean rather with the sea surface skin temperature
represented by SST alone. A number of studies have shown a relationship between
the thermal structure of the ocean and cyclone intensity (CI). Read more>>>>>>>>>>>>
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