Tag Archives: Tamil Nadu

Tropical Cyclone Fengal Drops Heavy Rain on Southern India

Tropical Cyclone Fengal dropped heavy rain on parts of southern India on Sunday.  At 4:00 a.m. EST on Sunday the center of Tropical Cyclone Fengal was located at latitude 12.1°N and longitude 79.8°E which put the center about 75 miles (120 km) south-southwest of Chennai, India.  Fengal was moving toward the west-northwest at 3 m.p.h. (5 km/h).  The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 995 mb.

Tropical Cyclone Fengal was dropping heavy rain on Sunday as it moved slowly inland over southern India.  Heavy rain was falling in the east central and northeastern parts of Tamil Nadu.

Tropical Cyclone Fengal was weakening gradually as it moved slowly inland over southern India.  The strongest winds were occurring in the part of Fengal’s circulation that were still over the Bay of Bengal.  Winds to tropical storm force extended out 45 miles (75 km) from the center of Tropical Cyclone Fengal.  The winds in the parts of Fengal’s circulation that were over land were blowing at less than tropical storm force.

Tropical Cyclone Fengal will move around the southern side of a high pressure system over eastern and southern Asia.  The high pressure system will steer Fengal toward the west during the next 48 hours.  On its anticipated track, Tropical Cyclone Fengal will continue to move slowly across southern.  Fengal could move over the Arabian Sea in 48 hours.

Tropical Cyclone Fengal will weaken gradually as it moves farther inland over southern India.  Fengal will continue to drop heavy rain on parts of Tamil Nadu during the next 24 hours.   Heavy rain is likely to cause floods in some locations.

Tropical Cyclone Fengal Brings Wind and Rain to Southeastern India

Tropical Cyclone Fengal brought wind and rain to southeastern India on Saturday.  At 10:00 a.m. EST on Saturday the center of Tropical Cyclone Fengal was located at latitude 12.4°N and longitude 80.5°E which put the center about 45 miles (75 km) south of Chennai, India.  Fengal was moving toward the west at 5 m.p.h. (8 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 989 mb.

The center of Tropical Cyclone Fengal made landfall on the coast of southeastern India between Chennai and Puducherry on Saturday.  Fengal was the equivalent of a tropical storm at the time of landfall.  Winds to tropical storm force extended out 70 miles (110 km) from the center of Tropical Cyclone Fengal.

Tropical Cyclone Fengal will move around the southern side of a high pressure system over eastern and southern Asia.  The high pressure system will steer Fengal toward the west during the next 24 hours.  On its anticipated track, Tropical Cyclone Fengal will move across southern India during the next 24 hours.

Tropical Cyclone Fengal will bring strong winds and heavy rain to Tamil Nadu.  Heavy rain is likely to cause floods in some locations.  Fengal could also cause a storm surge of up to 4 feet (1 meter) along the coast of Tamil Nadu.

Tropical Cyclone Fengal Forms Over Southwestern Bay of Bengal

Tropical Cyclone Fengal formed over the southwestern Bay of Bengal on Friday.  At 4:00 a.m. EST on Friday the center of Tropical Cyclone Fengal was located at latitude 11.2°N and longitude 82.2°E which put the center about 165 miles (270 km) east-southeast of the Puducherry, India. Fengal was moving toward the north-northwest at 8 m.p.h. (13 km/h).  The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 966 mb.

A low pressure system over the southwestern Bay of Bengal strengthened during Thursday night and the India Meteorological Department designated the system as Tropical Cyclone Fengal.  Thunderstorms formed near the center of Tropical Cyclone Fengal.  More thunderstorms also formed in bands revolving around the center of Fengal’s circulation.  Storms near the center of Fengal generated upper level divergence that pumped mass away from the tropical cyclone.  The removal of mass caused the surface pressure to decrease.

Tropical Cyclone Fengal will move through an environment favorable for intensification during the next 24 hours.  Fengal will move over water where where the Sea Surface Temperatures are near 29°C.  It will move under the axis of an upper level ridge that extends from India across the southern 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 Fengal is likely to intensify during the next 24 hours.

Tropical Cyclone Fengal will move around the southern side of a high pressure system over eastern and southern Asia.  The high pressure system will steer Fengal toward the west-northwest during the next 24 hours.  On its anticipated track, Tropical Cyclone Fengal will approach the coast of southeastern India near Puducherry in 24 hours.

Tropical Cyclone Fengal will bring strong winds and heavy rain to Tamil Nadu.  Heavy rain is likely to cause floods in some locations.  Fengal could also cause a storm surge of up to 4 feet (1 meter) along the coast of Tamil Nadu.

Tropical Cyclone Michaung Brings Wind and Rain to Southeast India

Tropical Cyclone Michaung brought wind and rain to southeast India on Monday night. At 7:00 p.m. EST on Monday the center of Tropical Cyclone Michaung was located at latitude 14.7°N and longitude 80.1°E which put it about 30 miles (50 km) northeast of Nellore, India. Michaung was moving toward the northwest at 6 m.p.h. (10 km/h). The maximum sustained wind speed was 70 m.p.h. (110 km/h) and there were wind gusts to 85 m.p.h. (135 km/h). The minimum surface pressure was 987 mb.

Tropical Cyclone Michaung intensified to the threshold of a hurricane/typhoon before the center made landfall on the coast of Andhra Pradesh north of Nellore. The inner end of a rainband wrapped around the center of Michaung’s circulation. Bands of showers and thunderstorms were revolving around the center of Tropical Cyclone Michaung. Winds to tropical storm force extended out 115 miles (185 km) from the center of Tropical Cyclone Michaung.

Tropical Cyclone Michaung will move around the southwestern part of a high pressure system over East Asia. The high pressure system will steer Michaung toward the north-northwest during the next 24 hours. On its anticipated track, the center of Tropical Cyclone Michaung will move along the southern coast of Andhra Pradesh. The center of Michaung will pass near Ongole on Tuesday. The India Meteorological Department issued Cyclone Warnings for the coasts of Andhra Pradesh, North Tamil Nadu and Puducherry. Bands in the northern and western parts of Michaung’s circulation were already dropping rain over northern Tamil Nadu and southern Andhra Pradesh. There were reports of flooding in Chennai.

Tropical Cyclone Michaung will weaken gradually as the center of circulation remains inland as it moves near the coast of Andhra Pradesh. Michaung will drop heavy rain on parts of Andhra Pradesh as it weakens. Heavy rain could cause additional floods in other locations. Tropical Cyclone Michaung could also cause a storm surge of up to seven feet (two meters) along the coast.

Tropical Cyclone Michaung Intensifies Southeast of Nellore, India

Tropical Cyclone Michaung intensified over the Bay of Bengal southeast of Nellore, India on Monday morning. At 10:00 a.m. EST on Monday the center of Tropical Cyclone Michaung was located at latitude 14.1°N and longitude 80.7°E which put it about 60 miles (95 km) southeast of Nellore, India. Michaung was moving toward the northwest at 6 m.p.h. (10 km/h). The maximum sustained wind speed was 70 m.p.h. (110 km/h) and there were wind gusts to 85 m.p.h. (135 km/h). The minimum surface pressure was 987 mb.

Tropical Cyclone Michaung intensified to the threshold of a hurricane/typhoon over the Bay of Bengal southeast of Nellore, India on Monday morning. The inner end of a rainband wrapped around the center of Michaung’s circulation. Bands of showers and thunderstorms were revolving around the center of Tropical Cyclone Michaung. Storms near the center of circulation generated upper level divergence that pumped mass away from the tropical cyclone. The removal of mass caused the surface pressure to decrease. Winds to tropical storm force extended out 115 miles (185 km) from the center of Tropical Cyclone Michaung.

Tropical Cyclone Michaung will move through an environment favorable for intensification during the next 12 hours. Michaung will move over water where the Sea Surface Temperatures are near 29°C. It will move under the southwestern part of an upper level ridge over the Bay of Bengal. The upper level ridge will produce southerly winds that will blow toward the top of Michaung’s circulation. Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification. The western part of Tropical Cyclone Michaung’s circulation will be over southeastern India. Even though almost half of Michaung will be over land, the center of circulation will still be over the Bay of Bengal. Tropical Cyclone Michaung could intensify to the equivalent of a hurricane/typhoon during the next 12 hours.

Tropical Cyclone Michaung will move around the southwestern part of a high pressure system over East Asia. The high pressure system will steer Michaung toward the north-northwest during the next 24 hours. On its anticipated track, Tropical Cyclone Michaung will move toward the coast of southeast India. The center of Michaung will approach the coast between Nellore and Machilipatnam in 18 hours. The India Meteorological Department issued Cyclone Warnings for the coasts of Andhra Pradesh, North Tamil Nadu and Puducherry. Tropical Cyclone Michaung will bring strong winds and locally heavy rain to parts of southeast India. Bands in the western side of Michaung’s circulation were already dropping rain over northern Tamil Nadu and southern Andhra Pradesh. There were reports of flooding in Chennai. Heavy rain could cause additional floods in other locations. Tropical Cyclone Michaung could cause a storm surge of up to seven feet (two meters) along the coast.

Tropical Cyclone Michaung Strengthens East of Chennai, India

Tropical Cyclone Michaung strengthened over the Bay of Bengal east of Chennai, India on Sunday. At 4:00 p.m. EST on Sunday the center of Tropical Cyclone Michaung was located at latitude 13.1°N and longitude 81.7°E which put it about 105 miles (165 km) east of Chennai, India. Michaung was moving toward the northwest at 9 m.p.h. (15 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 996 mb.

Tropical Cyclone Michaung strengthened gradually on Sunday. The inner end of a rainband wrapped around the western side of the center of Michaung’s circulation. Bands of showers and thunderstorms were revolving around the center of Tropical Cyclone Michaung. Storms near the center of circulation generated upper level divergence that pumped mass away from the tropical cyclone. The removal of mass caused the surface pressure to decrease. Winds to tropical storm force extended out 115 miles (185 km) from the center of Tropical Cyclone Michaung.

Tropical Cyclone Michaung will move through an environment favorable for intensification during the next 24 hours. Michaung will move over water where the Sea Surface Temperatures are near 29°C. It will move under the southwestern part of an upper level ridge over the Bay of Bengal. The upper level ridge will produce southeasterly winds that will blow toward the top of Michaung’s circulation. Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification. Tropical Cyclone Michaung system will intensify during the next 24 hours. Michaung could strengthen to the equivalent of a hurricane/typhoon.

Tropical Cyclone Michaung will move around the southwestern part of a high pressure system over East Asia. The high pressure system will steer Michaung toward the north-northwest during the next 24 hours. On its anticipated track, Tropical Cyclone Michaung will move toward the coast of southeast India. The center of Michaung will approach the coast between Nellore and Machilipatnam in 36 hours. The India Meteorological Department issued Cyclone Alerts for the coasts of Andhra Pradesh, North Tamil Nadu and Puducherry. Tropical Cyclone Michaung will bring strong winds and locally heavy rain to parts of southeast India. Bands in the western side of Michaung’s circulation were already dropping rain over northern Tamil Nadu and southern Andhra Pradesh. Heavy rain could cause floods in some locations. Tropical Cyclone Michaung could cause a storm surge of up to seven feet (two meters) along the coast.

Tropical Cyclone Michaung Develops over Southwest Bay of Bengal

Tropical Cyclone Michaung developed over the southwestern Bay of Bengal on Saturday evening. At 10:00 p.m. EST on Saturday the center of Tropical Cyclone Michaung was located at latitude 11.7°N and longitude 82.3°E which put it about 185 miles (300 km) southeast of Chennai, India. Michaung was moving toward the west-northwest at 7 m.p.h. (11 km/h). The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h). The minimum surface pressure was 1001 mb.

A low pressure system over the southwestern Bay of Bengal strengthened on Saturday evening and the India Meteorological Department designated the system as Tropical Cyclone Michaung. Bands of showers and thunderstorms were revolving around the center of Michaung’s circulation. Storms near the center of circulation generated upper level divergence that pumped mass away from the tropical cyclone. The removal of mass caused the surface pressure to decrease. Winds to tropical storm force extended out 60 miles (95 km) from the center of Tropical Cyclone Michaung.

Tropical Cyclone Michaung will move through an environment favorable for intensification during the next 24 hours. Michaung will move over water where the Sea Surface Temperatures are near 29°C. It will move under the southwestern 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 Michaung’s circulation. Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification. Tropical Cyclone Michaung system will intensify during the next 24 hours. Michaung could strengthen to the equivalent of a hurricane/typhoon.

Tropical Cyclone Michaung will move around the southwestern part of a high pressure system over East Asia. The high pressure system will steer Michaung toward the northwest during the next 24 hours. On its anticipated track, Tropical Cyclone Michaung will move toward the coast of southeast India. The center of Michaung could be east of Chennai in 24 hours. Tropical Cyclone Michaung will bring strong winds and locally heavy rain to parts of southeast India. Heavy rain could cause floods in some locations. The India Meteorological Department issued Cyclone Alerts for the coasts of Andhra Pradesh, North Tamil Nadu and Puducherry.

Tropical Cyclone Mandous Makes Landfall in Southern India

Tropical Cyclone Mandous made landfall in southern India on Friday. At 4:00 p.m. EST on Friday the center of Tropical Cyclone Mandous was located at latitude 12.8°N and longitude 80.4°E which put it about 150 miles (240 km) southwest of Chennai, India. Mandous was moving toward the northwest at 10 m.p.h. (16 km/h). The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h). The minimum surface pressure was 1000 mb.

The center of Tropical Cyclone Mandous made landfall on the coast of southern India between Chennai and Puducherry on Friday. Mandous moved into a mass of drier air and weakened prior to landfall. Tropical Cyclone Mandous was the equivalent of a tropical storm at the time of landfall. Winds to tropical storm force extended out 70 miles (110 km) from the center of Mandous’ circulation. The heaviest rain was falling in bands in the western half of Tropical Cyclone Mandous.

Tropical Cyclone Mandous will move around the southern side of a high pressure system over southern Asia. The high pressure system will steer Mandous toward the west-northwest during the next 24 hours. On its anticipated track, Tropical Cyclone Mandous move farther inland over southern India during the next 24 hours. Mandous will weaken gradually as it moves farther inland. Tropical Cyclone Mandous will bring gusty winds and locally heavy rain to parts of Puducherry, northern Tamil Nadu and southern Andhra Pradesh. Heavy rain could cause flash floods in some locations.

Tropical Cyclone Mandous Strengthens over Southwest Bay of Bengal

Tropical Cyclone Mandous strengthened over the southwestern Bay of Bengal on Thursday. At 4:00 p.m. EST on Thursday the center of Tropical Cyclone Mandous was located at latitude 10.7°N and longitude 81.9°E which put it about 215 miles (345 km) southeast of Chennai, India. Mandous was moving toward the west-northwest at 9 m.p.h. (15 km/h). The maximum sustained wind speed was 65 m.p.h. (105 km/h) and there were wind gusts to 80 m.p.h. (130 km/h). The minimum surface pressure was 988 mb.

The circulation around Tropical Cyclone Mandous strengthened on Thursday. Even though Mandous was stronger, the distribution of thunderstorms continued to be asymmetrical. Many of the thunderstorms were occurring in bands in the western half of Mandous’ circulation. Bands in the eastern half of Mandous consisted primarily of showers and lower clouds. Storms west of the center of Mandous generated upper level divergence that pumped mass away to the west of the tropical cyclone. Winds to tropical storm force extended out 150 miles (240 km) from the center of Tropical Cyclone Mandous.

Tropical Cyclone Mandous will move through an environment that will become unfavorable for intensification during the next 24 hours. Mandous will move over water where the Sea Surface Temperatures are near 28˚C. It will move under the southwestern part of an upper level ridge over Southeast Asia and the Bay of Bengal. The ridge will produce easterly winds that will blow toward the top of Mandous’ circulation. Those winds will cause moderate vertical wind shear. The wind shear is already contributing to the asymmetrical distribution of thunderstorms and the shear will inhibit intensification. The western side Tropical Cyclone Mandous will interact with a mass of drier air over India, when Mandous gets closer to the coast of India. A combination of moderate vertical wind shear and drier air is likely to cause Mandous to begin to weaken during the next 24 hours.

Tropical Cyclone Mandous will move around the southern side of a high pressure system over southern Asia. The high pressure system will steer Mandous toward the northwest during the next 24 hours. On its anticipated track, Tropical Cyclone Mandous will be near the coast of southern India near Chennai in 24 hours. Mandous will bring gusty winds and locally heavy rain to Puducherry, northern Tamil Nadu and southern Andhra Pradesh. Tropical Cyclone Mandous will also drop heavy rain over northern Sri Lanka. Heavy rain could cause flash floods in some locations.

Tropical Cyclone Mandous Forms over Southwest Bay of Bengal

Tropical Cyclone Mandous formed over the southwestern Bay of Bengal east of Sri Lanka on Wednesday afternoon. At 10:00 p.m. EST on Wednesday the center of Tropical Cyclone Mandous was located at latitude 9.6°N and longitude 83.8°E which put it about 360 miles (580 km) southeast of Chennai, India. Mandous was moving toward the west-northwest at 6 m.p.h. (10 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 997 mb.

The circulation around a low pressure system over the southwestern Bay of Bengal strengthened on Wednesday afternoon and the India Meteorological Department designated the system as Tropical Cyclone Mandous. The distribution of thunderstorms around Tropical Cyclone Mandous was asymmetrical. Many of the thunderstorms were occurring in bands in the western half of Mandous’ circulation. Bands in the eastern half of Mandous consisted primarily of showers and lower clouds. Storms west of the center of Mandous generated upper level divergence that pumped mass away to the west of the tropical cyclone. Winds to tropical storm force extended out 85 miles (135 km) from the center of Tropical Cyclone Mandous.

Tropical Cyclone Mandous will move through an environment somewhat favorable for intensification during the next 24 hours. Mandous will move over water where the Sea Surface Temperatures are near 28˚C. It will move under the southwestern part of an upper level ridge over Southeast Asia and the Bay of Bengal. The ridge will produce easterly winds that will blow toward the top of Mandous’ circulation. Those winds will cause moderate vertical wind shear. The wind shear is contributing to the asymmetrical distribution of thunderstorms and the shear will inhibit intensification. The vertical wind shear may not be strong enough to prevent intensification during the next 24 hours and Tropical Cyclone Mandous could strengthen during that time period.

Tropical Cyclone Mandous will move around the southern side of a high pressure system over southern Asia. The high pressure system will steer Mandous toward the northwest during the next 48 hours. On its anticipated track, Tropical Cyclone Mandous could be near the coast of southern India near Chennai in 48 hours. Mandous could bring gusty winds and locally heavy rain to Puducherry, northern Tamil Nadu and southern Andhra Pradesh. Heavy rain could cause flash floods in some locations.