Tag Archives: Port Blair

Tropical Cyclone Mocha Develops over Bay of Bengal

Tropical Cyclone Mocha developed over the Bay of Bengal on Thursday morning. At 5:00 a.m. EDT on Thursday the center of Tropical Cyclone Mocha was located at latitude 11.2°N and longitude 88.1°E which put it about 310 miles (500 km) west of Port Blair. Mocha was moving toward the north-northwest at 4 m.p.h. (6 km/h). The maximum sustained wind speed was 50 m.p.h. (80 km/h) and there were wind gusts to 65 m.p.h. (105 km/h). The minimum surface pressure was 993 mb.

A low pressure system over the Bay of Bengal strengthened during Wednesday night and the India Meteorological Department classified the system as Tropical Cyclone Mocha. The circulation around Tropical Cyclone Mocha was organizing rapidly on Thursday morning. The inner end of a rainband wrapped around the center of Mocha’s circulation and a large eye appeared to be forming. Bands of showers and thunderstorms were revolving around the developing inner core of Tropical Cyclone Mocha. Storms near the center of circulation generated strong upper level divergence that pumped mass away from the tropical cyclone. The removal of mass was causing the surface pressure to decrease. Winds to tropical storm force extended out 115 miles (185 km) from the center of Mocha’s circulation.

Tropical Cyclone Mocha will move through an environment very favorable for intensification during the next 48 hours. Mocha will move over water where the Sea Surface Temperatures are near 30˚C. It will move under the center of an upper level ridge over the Bay of Bengal. The upper level winds are weak near the center of the ridge and there will be little vertical wind shear. Tropical Cyclone Mocha will intensify during the next 48 hours. Mocha could intensify rapidly once the inner core with an eye and eyewall are completely formed. Mocha is likely to intensify to the equivalent of a hurricane/typhoon during the next 24 hours. Mocha could intensify to the equivalent of a major hurricane in two or three days.

Tropical Cyclone Mocha will move around the western end of a high pressure system that extends from the Western North Pacific Ocean to Southeast Asia. The high pressure system will steer Mocha toward the north during the next 24 hours. Mocha will start to move toward the north-northeast on Friday after it moves around the western end of the high pressure system. Tropical Cyclone Mocha is likely to make landfall near the border between Bangladesh and Myanmar during the weekend. Mocha could be the equivalent of a major hurricane when it makes landfall. Tropical Cyclone Mocha will bring strong winds and locally heavy rain to Myanmar and Bangladesh. Heavy rain is likely to cause flash floods in some locations. Mocha could also cause a storm surge of up to 10 feet (3 meters) along portions of the coast where the wind blows the water toward the shore.

Tropical Cyclone Forming over Bay of Bengal

A tropical cyclone was forming over the Bay of Bengal on Tuesday morning. At 11:00 a.m. EDT on Tuesday the center of a low pressure system was located at latitude 8.3°N and longitude 88.3°E which put it about 370 miles (595 km) southwest of Port Blair. The low pressure system was moving toward the northwest at 10 m.p.h. (16 km/h). The maximum sustained wind speed was 35 m.p.h. (55 km/h) and there were wind gusts to 45 m.p.h. (75 km/h). The minimum surface pressure was 998 mb.

A low pressure system was strengthening over the southern Bay of Bengal on Tuesday morning. The India Meteorological Department classified the system as a well marked low pressure system and the Joint Typhoon Warning Center designated the system as Invest 91B. The circulation around the low pressure system exhibited more organization on Tuesday morning. Several bands of showers and thunderstorms were beginning to revolve around the center of circulation. The strongest bands were in the southern and western parts of the low pressure system. Storms near the center of circulation began to generate upper level divergence that pumped mass away from the low pressure system. The removal of mass was causing the surface pressure to decrease.

The low pressure system will move through an environment favorable for intensification during the next few days. The low pressure system will move over water where the Sea Surface Temperatures are near 30˚C. It will move under the center of an upper level ridge over the Bay of Bengal. The upper level winds are weak near the center of the ridge and there will be little vertical wind shear. The low pressure system will intensify during the next 48 hours. It is likely to strengthen to a tropical cyclone during the next 24 hours. The low pressure system is likely to intensify to the equivalent of a hurricane/typhoon later this week.

The low pressure system will move around the western end of a high pressure system that extends from the Western North Pacific Ocean to Southeast Asia. The high pressure system will steer the low pressure system toward the north during the next 24 hours. On its anticipated track the center of circulation will pass west of the Andaman Islands and the Nicobar Islands. Bands of showers and thunderstorms in the eastern side of the circulation will bring gusty winds and locally heavy rain to the Andaman Islands and the Nicobar Islands. The low pressure system will move toward the north-northeast later this week. It is likely to make landfall near the border between Bangladesh and Myanmar in a few days. The low pressure system is likely to be the equivalent of a hurricane/typhoon when it makes landfall.

Tropical Cyclone 02B Develops over Bay of Bengal

Tropical Cyclone 02B developed over the Bay of Bengal southwest of Port Blair on Saturday morning. At 5:00 a.m. EDT on Saturday the center of Tropical Cyclone 02B was located at latitude 9.9°N and longitude 90.9°E which put it about 165 miles (265 km) southwest of Port Blair, Andaman Islands. Tropical Cyclone 02B was moving toward the northwest at 9 m.p.h (15 km/h). The maximum sustained wind speed was 45 m.p.h. (75 km/h) and there were wind gusts to 60 m.p.h. (95 km/h). The minimum surface pressure was 995 mb.

The circulation around a low pressure system over the eastern Bay of Bengal strengthened on Saturday morning and the center was designated as Tropical Cyclone 02B. More thunderstorms formed near the center of Tropical Cyclone 02B. The inner end of a rainband wrapped around the southern side of the center of circulation. Other bands of showers and thunderstorms were revolving around the center. Storms near the center of circulation generated upper level divergence that pumped mass away from the tropical cyclone. Winds to tropical storm force extended out 70 miles (110 km) from the center of circulation.

Tropical Cyclone 02B will move through an environment favorable for intensification during the next 36 hours. The tropical cyclone will move over water where the Sea Surface Temperatures are near 31˚C. It will move under the southern part of an upper level ridge over the Bay of Bengal. The upper level ridge will produce easterly winds that will blow toward the top of the low pressure system. Those winds will cause some vertical wind shear, but the shear will not be large enough to prevent intensification. Tropical Cyclone 02B will intensify during the next 36 hours and it could strengthen to the equivalent of a hurricane/typhoon.

Tropical Cyclone 02B will move around the southwestern side of a high pressure system over Southeast Asia. The high pressure system will steer the tropical cyclone toward the northwest during the next 36 hours. On its anticipated track Tropical Cyclone 02B will move slowly away from the Andaman Islands and the Nicobar Islands. The tropical cyclone will continue to drop locally heavy rain over the Nicobar Islands and the Andaman Islands until it moves farther northwest of those areas. Heavy rain could cause flash floods in some locations.

Low Pressure System Forms over Eastern Bay of Bengal

A low pressure system formed over the eastern Bay of Bengal near the Nicobar Islands on Friday morning. At 8:00 a.m. EDT on Friday the center of a low pressure system was located at latitude 8.6°N and longitude 92.5°E which put it about 45 miles (75 km) south-southwest of Malacca, Nicobar Islands and about 205 miles (330 km) south of Port Blair, Andaman Islands. The low pressure system was moving toward the northwest at 9 m.p.h (15 km/h). The maximum sustained wind speed was 30 m.p.h. (50 km/h) and there were wind gusts to 40 m.p.h. (65 km/h). The minimum surface pressure was 1001 mb.

A surface low pressure system, also designated as Invest 92B, formed over the eastern Bay of Bengal near the Nicobar Islands on Friday morning. The circulation around the low pressure system exhibited more organization on conventional and microwave satellite images. The strongest thunderstorms were occurring in a band just to the west of the center of the low pressure system. Other bands of showers and thunderstorms were revolving around the center of circulation. Storms near the center were generating upper level divergence that was pumping mass away from the low pressure system. The removal of mass was causing the surface pressure to decrease.

The low pressure system will move through an environment favorable for intensification during the next 24 hours. The low pressure system will move over water where the Sea Surface Temperatures are near 31˚C. It will move under the southern part of an upper level ridge over the Bay of Bengal. The upper level ridge will produce easterly winds that will blow toward the top of the low pressure system. Those winds will cause some vertical wind shear, but the shear will not be large enough to prevent intensification. The low pressure system will strengthen during the next 24 hours and it could intensify to a tropical cyclone during the weekend.

The low pressure system will move around the southwestern side of a high pressure system over Southeast Asia. The high pressure system will steer the low pressure system toward the northwest during the next 24 hours. On its anticipated track the low pressure system will move slowly away from the Nicobar Islands. The low pressure system will drop locally heavy rain over the Nicobar Islands and the Andaman Islands. Heavy rain could cause flash floods in some locations.

Tropical Cyclone Amphan Develops Quickly Over Bay of Bengal

Tropical Cyclone Amphan developed quickly over the Bay of Bengal on Saturday.  At 5:00 p.m. EDT on Saturday the center of Tropical Cyclone Amphan was located at latitude 11.2°N and longitude 86.3°E which put it about 430 miles (695 km) west of Port Blair.  Amphan was moving toward the north at 8 m.p.h (13 km/h).  The maximum sustained wind speed was 50 m.p.h. (80 km/h) and there were wind gusts to 65 m.p.h. (105 km/h).  The minimum surface pressure was 992 mb.

The circulation around a low pressure system over the Bay of Bengal organized quickly on Saturday and the Indian Meteorological Department designated the system as Tropical Cyclone Amphan.  Thunderstorms formed around the center of Amphan and recent microwave images suggested that an eye could be forming.  Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Amphan.  The stronger bands were in the western half of the circulation.  Storms near the core of the circulation were generating strong upper level divergence which was pumping mass away from the tropical cyclone in all directions.  Winds to tropical storm force extended out 100 miles (160 km) from the center of Amphan.

Tropical Cyclone Amphan will move through an environment very favorable for intensification.  Amphan will move over water where the Sea Surface Temperature is near 31°C.  It will move under the axis of an upper level ridge over the Bay of Bengal.  The upper level winds are weak near the axis of the ridge and there will be little vertical wind shear.  Tropical Cyclone Amphan is likely to intensify rapidly during the next 36 hours.  Amphan is likely to strengthen into the equivalent of a hurricane/typhoon within 24 hours and it could become the equivalent of a major hurricane within 36 to 48 hours.

Tropical Cyclone Amphan will move around the eastern end of a high pressure system over southeast Asia.  The high will steer Amphan toward the north during the next several days.  On its anticipated track Tropical Cyclone Amphan could approach the coast of northeast Indian and Bangladesh in 72 hours.  Amphan will likely be the equivalent of a major hurricane when it approaches the coast.  Tropical Cyclone Amphan could generate a catastrophic storm surge along the north coast of the Bay of Bengal.