Abstract. Levelling observations conducted during the Great Trigonomet-rical Survey of India (1858{1909) and subsequent observations showed that mean sea level along the coast of India is higher in the Bay of Bengal than in the Arabian Sea, the dierence in sea level between Vishakhapatnam and Mumbai (Bombay) being about 30 cm. Using simulations with a 1 1 2-layer reduced-gravity model, we attribute this to the mean, large-scale wind-forced circulation (60%) and the alongshore gradient in salinity (40%). The former (latter) is a consequence of the distribution of wind stress (rainfall) because of the monsoon
Not AvailableCoastal West Bengal, the low-lying landward extension of the continental shelf of the B...
206-209Tide gauge observations near Madras Port, Tamil Nadu, India are presented and sea level fluct...
A nonlinear, 4-layer reduced-gravity ocean model with active thermodynamics and mixed layer physics ...
Levelling observations conducted during the Great Trigonometrical Survey of India (1858-1909) and su...
The Mumbai (Bombay) tide gauge data, the only century-long record in the Indian Ocean, show that int...
The contribution of atmospheric pressure and local wind to sea level variability at Goa (West coast ...
The global mean sea level (GMSL) changes derived from modelling do not match actual measurements of ...
Sea level changes can be of two types: (i) changes in the mean sea level and (ii) changes in the ext...
A framework involving long baroclinic waves, which treats the north Indian Ocean as a single dynamic...
The contribution of atmospheric pressure and wind to sea level variability at Goa (West coast of Ind...
Mean sea level variation is a global phenomenon with spatial variations in trends on regional levels...
The present communication discusses sea-level-rise trends in the north Indian Ocean, particularly of...
The study examines the observed storm-generated sea level variation due to deep depression (event 1:...
In this paper, we show that a linear, continuously stratified ocean model reproduces observed wind-d...
International audienceIndian Ocean is the home to many tropical low lying islands and highly populat...
Not AvailableCoastal West Bengal, the low-lying landward extension of the continental shelf of the B...
206-209Tide gauge observations near Madras Port, Tamil Nadu, India are presented and sea level fluct...
A nonlinear, 4-layer reduced-gravity ocean model with active thermodynamics and mixed layer physics ...
Levelling observations conducted during the Great Trigonometrical Survey of India (1858-1909) and su...
The Mumbai (Bombay) tide gauge data, the only century-long record in the Indian Ocean, show that int...
The contribution of atmospheric pressure and local wind to sea level variability at Goa (West coast ...
The global mean sea level (GMSL) changes derived from modelling do not match actual measurements of ...
Sea level changes can be of two types: (i) changes in the mean sea level and (ii) changes in the ext...
A framework involving long baroclinic waves, which treats the north Indian Ocean as a single dynamic...
The contribution of atmospheric pressure and wind to sea level variability at Goa (West coast of Ind...
Mean sea level variation is a global phenomenon with spatial variations in trends on regional levels...
The present communication discusses sea-level-rise trends in the north Indian Ocean, particularly of...
The study examines the observed storm-generated sea level variation due to deep depression (event 1:...
In this paper, we show that a linear, continuously stratified ocean model reproduces observed wind-d...
International audienceIndian Ocean is the home to many tropical low lying islands and highly populat...
Not AvailableCoastal West Bengal, the low-lying landward extension of the continental shelf of the B...
206-209Tide gauge observations near Madras Port, Tamil Nadu, India are presented and sea level fluct...
A nonlinear, 4-layer reduced-gravity ocean model with active thermodynamics and mixed layer physics ...