Visakhapatnam:A low-pressure area formed in the Bay of Bengal on Saturday is likely to intensify into a cyclone by Monday, according to the India Meteorological Department (IMD). The system is expected to move west-northwestwards, heading towards the Tamil Nadu and S...
Downstream and In Situ: Two Perspectives on the Initiation of Monsoon Low‐Pressure Systems Over the Bay of BengalMonsoonLow pressure systemmonsoon depressionMonsoon low pressure systems (LPS) contribute to more than half of the total summer monsoon rainfall over central India. As their genesis ...
The structure of a monsoon low over the Bay of Bengal during 3-6 July 1979 and cover the land on 9 July 1979 has been investigated in respect of wind, temperature, vertical tilt, relative humidity, relative vorticity and vergence. The structure of the depression of the respective parameters ...
Sea surface temperature measured by the Tropical Rainfall Measuring Mission Microwave Imager (TMI) over the Bay of Bengal during monsoon was found to exhibit a low-period intra-seasonal mode of 8-16 days, in addition to the 30-60 days mode. This unique feature is attributed to the coherent ...
This sudden enhancement of westerly wind was mainly due to the rapidly intensified mid-level cross-equatorial flow. Our results show that a high-pressure system in the Southern Hemisphere induced this strong, mid-level, cross-equatorial flow. During the rapid intensification period of TC Nargis (...
The idea of formalizing IPs is hotly contested, but identifying those who are not breaking regulations and integrating them into the mainstream healthcare delivery system would not only ease the pressure on the overburdened system, but would also enable resource limited countries reach the poor and...
ANALYSIS OF AMBIENT FIELDS AND SATELLITE IMAGERY CHARACTERISTICS OF EFFECT OF BAY OF BENGAL STORMS ON LOW- LATITUDE PLATEAUANALYSIS OF AMBIENT FIELDS AND SATELLITE IMAGERY CHARACTERISTICS OF EFFECT OF BAY OF BENGAL STORMS ON LOW- LATITUDE PLATEAU热带气象风暴...
The low-latitudinal cyclones (LLCs, originating between 5°N–10°N) constitute≈40% of tropical cyclones (TCs) formed in the Bay of Bengal (BoB). We investigate the interannual variability of post-monsoonal (October to December) BoB LLCs and their teleconnection with El Nio Southern ...
This paper reports the observation of persistently low tropopause temperatures (100hPa temperatures, T-100) and ozone at 100hPa throughout the year as compared to the corresponding zonal mean values over the Bay of Bengal (BOB) region. The long term mean T-100 (i.e., from January 2006-...
Appearance of the persistently low tropopause temperature and ozone over the Bay of Bengal regionTROPOPAUSEOZONE layerMONSOONSMIDDLE atmosphereSTRATOSPHEREThis paper reports the observation of persistently low tropopause temperatures (100hPa temperatures, T100) and ozone at 100hPa throughout the year as ...