A simple 1.5 layer reduced gravity transport model is used to understand the influence of a moving tropical cyclone on the upper layer of the Bay of Bengal. The wind stress used to force the model is derived from an idealised cyclone. The model cyclone is considered to be a symmetric vortex with both tangential and radial winds. The cyclone center moves northwestwards between the points 97 E, 8 N and 82 E, 23 N. In the control experiment, the cyclone is allowed to move the total distance in 5 days. The oceanic response is asymmetric in contrast to the symmetric wind forcings. Right bias found in the maxima of model circulation and upper layer thickness deviations, is in agreement with other modelling studies. Fifteen sensitivity experiments...
The upper ocean is dramatically affected during tropical cyclones (TCs). Cyclones interact not only ...
Gulf of Mexico is evaluated to determine what aspects of ocean model performance need to be improved...
The year to year variability of surface mixing in the Bay of Bengal (BoB) is examined with the help ...
The sensitivity of the ocean mixed layer response to different parameters such as model horizontal r...
The understanding of significant changes in the oceanic mixed layer is important for dynamical predi...
A simplified analytical model is developed to describe the baroclinic and barotropic ocean response ...
ABSTRACT This study used the Princeton ocean model (POM) which includes second-order turbulent closu...
International audienceA simplified analytical model is developed to describe the baroclinic and baro...
A numerical model of tropical cyclone development (Sundqvist, 1970a) has been used to study and comp...
Control mechanisms of tropical cyclone size are investigated with the axisymmetric cloud model HURMO...
This paper assesses the impact of air-sea coupling on Indian Ocean tropical cyclones (TCs) by compar...
Most extant studies of tropical cyclone movement consider a barotropic vortex on a $ plane. However,...
The present study is aimed to investigate sub-surface ocean processes and their contribution to the ...
A coupled atmosphere–ocean–wave model was used to examine mixing in the upper-oceanic layers under ...
Surface cooling induced by tropical cyclones (TCs) is about three times larger during premonsoon tha...
The upper ocean is dramatically affected during tropical cyclones (TCs). Cyclones interact not only ...
Gulf of Mexico is evaluated to determine what aspects of ocean model performance need to be improved...
The year to year variability of surface mixing in the Bay of Bengal (BoB) is examined with the help ...
The sensitivity of the ocean mixed layer response to different parameters such as model horizontal r...
The understanding of significant changes in the oceanic mixed layer is important for dynamical predi...
A simplified analytical model is developed to describe the baroclinic and barotropic ocean response ...
ABSTRACT This study used the Princeton ocean model (POM) which includes second-order turbulent closu...
International audienceA simplified analytical model is developed to describe the baroclinic and baro...
A numerical model of tropical cyclone development (Sundqvist, 1970a) has been used to study and comp...
Control mechanisms of tropical cyclone size are investigated with the axisymmetric cloud model HURMO...
This paper assesses the impact of air-sea coupling on Indian Ocean tropical cyclones (TCs) by compar...
Most extant studies of tropical cyclone movement consider a barotropic vortex on a $ plane. However,...
The present study is aimed to investigate sub-surface ocean processes and their contribution to the ...
A coupled atmosphere–ocean–wave model was used to examine mixing in the upper-oceanic layers under ...
Surface cooling induced by tropical cyclones (TCs) is about three times larger during premonsoon tha...
The upper ocean is dramatically affected during tropical cyclones (TCs). Cyclones interact not only ...
Gulf of Mexico is evaluated to determine what aspects of ocean model performance need to be improved...
The year to year variability of surface mixing in the Bay of Bengal (BoB) is examined with the help ...