Severe thunderstorms form over the Eastern and Northeastern parts of India, i.e., Gangetic West Bengal, Jharkhand, Orissa, Assam and parts of Bihar during the pre-monsoon months (April-May). These storms are known as "Nor'wester" as they move from Northwest to Southeast. In this study we have made numerical simulations of 10 thunderstorms that formed over the West Bengal region during April-May of 2005 and 2006. Numerical simulations have been carried out using MM5 mesoscale model (at 10 km resolution) using conventional and non-conventional observations from Doppler Weather Radar (DWR) and satellites. Composite characteristics of the Nor'wester have been made based upon the simulations. Results indicate that the Nor'westers occur generally...
The thunderstorms are typical mesoscale systems dominated by intense convection. Mesoscale models ar...
Thunderstorm is one of the most spectacular weather phenomena in the atmosphere. Many parts over the...
The thunderstorms are typical mesoscale systems dominated by intense convection. Mesoscale models ar...
A common feature of the weather during the pre-monsoon season (March–May) over the east and northeas...
The weather systems that predominantly affect the eastern and northeastern parts of India during the...
Thunderstorm, resulting from vigorous convective activity, is one of the most spectacular weather ph...
North India is comprised, in parts, of complex Himalayan mountain ranges having different altitudes ...
419-433Simulation of three severe local storms occurring over Gangetic West Bengal and surrounding a...
A severe thunderstorm produced a tornado (F3 on the Fujita-Pearson scale), which affected Rajkanika ...
In the tropics, most of the extreme weather events are convective in nature. Many parts over the Ind...
Radar observations of nor'wester (premonsoon thunderstorm) as experienced over the Gangetic West Be...
A non-hydrostatic version of PSU /NCAR mesoscale model is used to simulate the characteristic featur...
Northern India is comprised of complex Himalayan mountain ranges having different altitude and orien...
Simulation studies have been carried out for two weather systems namely; a pre-monsoon thunderstorm ...
Severe local storms, including tornadoes, damaging hail and wind gusts, frequently occur over the ea...
The thunderstorms are typical mesoscale systems dominated by intense convection. Mesoscale models ar...
Thunderstorm is one of the most spectacular weather phenomena in the atmosphere. Many parts over the...
The thunderstorms are typical mesoscale systems dominated by intense convection. Mesoscale models ar...
A common feature of the weather during the pre-monsoon season (March–May) over the east and northeas...
The weather systems that predominantly affect the eastern and northeastern parts of India during the...
Thunderstorm, resulting from vigorous convective activity, is one of the most spectacular weather ph...
North India is comprised, in parts, of complex Himalayan mountain ranges having different altitudes ...
419-433Simulation of three severe local storms occurring over Gangetic West Bengal and surrounding a...
A severe thunderstorm produced a tornado (F3 on the Fujita-Pearson scale), which affected Rajkanika ...
In the tropics, most of the extreme weather events are convective in nature. Many parts over the Ind...
Radar observations of nor'wester (premonsoon thunderstorm) as experienced over the Gangetic West Be...
A non-hydrostatic version of PSU /NCAR mesoscale model is used to simulate the characteristic featur...
Northern India is comprised of complex Himalayan mountain ranges having different altitude and orien...
Simulation studies have been carried out for two weather systems namely; a pre-monsoon thunderstorm ...
Severe local storms, including tornadoes, damaging hail and wind gusts, frequently occur over the ea...
The thunderstorms are typical mesoscale systems dominated by intense convection. Mesoscale models ar...
Thunderstorm is one of the most spectacular weather phenomena in the atmosphere. Many parts over the...
The thunderstorms are typical mesoscale systems dominated by intense convection. Mesoscale models ar...