Sea level changes can be of two types: (i) changes in the mean sea level and (ii) changes in the extreme sea level. The former is a global phenomenon while the latter is a regional phenomenon. Estimates of mean sea level rise made from past tide gauge data at selected stations along the coast of India indicate a rise of slightly less than 1 mm/year; however these estimates need to be corrected by including the rates of vertical land movements, whose measurements are not available at present. Simulation results of a regional climate model, HadRM2, were analysed for the northern Indian Ocean to provide the future scenarios of the occurrence of tropical cyclones in the Bay of Bengal for the period 2041-60. This model simulations consist of a c...
The global mean sea level (GMSL) changes derived from modelling do not match actual measurements of ...
1513-1520Since recent past a growing concern has been raised by designers of various coastal and off...
Twentieth-century regional sea level changes are estimated from 12 climate models from phase 5 of th...
Mean sea level variation is a global phenomenon with spatial variations in trends on regional levels...
Coastal flooding due to storm surge and high tides is a serious risk for inhabitants of the Ganges–B...
Climate change is a causative factor of profound series of changers including sea level rising, incr...
The study examines the observed storm-generated sea level variation due to deep depression (event 1:...
A framework involving long baroclinic waves, which treats the north Indian Ocean as a single dynamic...
Sea-level rise is an inevitable consequence of climate change due to increased external forcings and...
International audienceIndian Ocean is the home to many tropical low lying islands and highly populat...
The present communication discusses sea-level-rise trends in the north Indian Ocean, particularly of...
Future changes in wave climate will influence the marine ecosystem, coastal erosion, design of coast...
Storm surges generated by the strong tangential wind stressesand normal atmospheric pressure gradien...
Estimates of return periods of extreme sea level events along the coast are useful for impact assess...
The global mean sea level (GMSL) changes derived from modelling do not match actual measurements of ...
1513-1520Since recent past a growing concern has been raised by designers of various coastal and off...
Twentieth-century regional sea level changes are estimated from 12 climate models from phase 5 of th...
Mean sea level variation is a global phenomenon with spatial variations in trends on regional levels...
Coastal flooding due to storm surge and high tides is a serious risk for inhabitants of the Ganges–B...
Climate change is a causative factor of profound series of changers including sea level rising, incr...
The study examines the observed storm-generated sea level variation due to deep depression (event 1:...
A framework involving long baroclinic waves, which treats the north Indian Ocean as a single dynamic...
Sea-level rise is an inevitable consequence of climate change due to increased external forcings and...
International audienceIndian Ocean is the home to many tropical low lying islands and highly populat...
The present communication discusses sea-level-rise trends in the north Indian Ocean, particularly of...
Future changes in wave climate will influence the marine ecosystem, coastal erosion, design of coast...
Storm surges generated by the strong tangential wind stressesand normal atmospheric pressure gradien...
Estimates of return periods of extreme sea level events along the coast are useful for impact assess...
The global mean sea level (GMSL) changes derived from modelling do not match actual measurements of ...
1513-1520Since recent past a growing concern has been raised by designers of various coastal and off...
Twentieth-century regional sea level changes are estimated from 12 climate models from phase 5 of th...