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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.

Low Pressure System Forms over Bay of Bengal

A low pressure system formed over the Bay of Bengal on Thursday. The low pressure system was designated as Invest 95B. At 10:00 p.m. EST on Thursday the center of a low pressure system was located at latitude 9.4°N and longitude 86.3°E which put it about 485 miles (780 km) southeast of Chennai, India. The low pressure system was moving toward the northwest at 10 m.p.h. (16 km/h). The maximum sustained wind speed was 25 m.p.h. (40 km/h) and there were wind gusts to 35 m.p.h. (55 km/h). The minimum surface pressure was 1008 mb.

The circulation around a low pressure system over the Bay of Bengal exhibited more organization on Thursday evening. The pattern of clouds began to look more like a developing tropical cyclone. More thunderstorms formed in bands around the low pressure system. The bands started to revolve around the center of circulation. Storms near the center began to generate upper level divergence that pumped mass away from the low pressure system.

The low pressure system will be in an environment favorable for the development of a tropical cyclone during the next 36 hours. Invest 95B will move over water where the Sea Surface Temperatures are near 29°C. It will move under the middle of an upper level ridge over the Bay of Bengal. The upper level winds are weak near the middle of the ridge and there will be little vertical wind shear. The low pressure system will intensify during the next 36 hours. It is likely to develop into a tropical cyclone.

The low pressure system will move around the southwestern part of a high pressure system over East Asia. The high pressure system will steer Invest 95B toward the northwest during the next 36 hours. On its anticipated track, the low pressure system will move toward the coast of southeast India. It could approach the coast as a tropical cyclone by the end of the weekend.

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.

Tropical Cyclone 01B Weakens over Bay of Bengal

Tropical Cyclone 01B weakened over the Bay of Bengal on Saturday. At 4:00 p.m. EST on Saturday the center of Tropical Cyclone 01B was located at latitude 11.2°N and longitude 82.8°E which put it about 160 miles (260 km) east-southeast of Chennai India. It was moving toward the west at 4 m.p.h (6 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 1003 mb.

Tropical Cyclone 01B weakened over the southwest Bay of Bengal on Saturday. The inflow around the western side of the tropical cyclone pulled drier air that was over India into Tropical Cyclone 01B. The drier air circulated around the tropical cyclone and it caused many of the thunderstorms to dissipate. A few thunderstorms persisted in a band northeast of the center of circulation. The other bands consisted primarily of showers and lower clouds. The dissipation of thunderstorms resulted in a circulation that was present only in the lower atmosphere.

Tropical Cyclone 01B will move through an environment unfavorable for intensification during the next 24 hours. The tropical cyclone will move over water where the Sea Surface Temperatures are near 28˚C. However the drier air will continue to inhibit the formation of new thunderstorms. The tropical cyclone will move under the western part of an upper level ridge centered over southeast Asia. The ridge will produce southeast winds that will blow toward the top of the depression. Those winds will cause moderate vertical wind shear and the shear will also inhibit intensification. Tropical Cyclone 01B is likely to continue to weaken as the circulation spins down. It could bring rain showers to southern India early next week.

Depression Forms over Bay of Bengal

A depression formed over the Bay of Bengal on Friday morning. At 10:00 a.m. EST on Friday the center of the depression was located at latitude 9.4°N and longitude 83.4°E which put it about 320 miles (515 km) southeast of Chennai India. It was moving toward the north-northwest at 7 m.p.h (11 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 1000 mb.

The circulation around a low pressure system over the Bay of Bengal strengthened on Friday morning and the system was classified as a depression by the India Meteorological Department. More thunderstorms develop near the enter of the depression. Bands of showers and thunderstorms were revolving around the center of circulation. Storms near the center generated upper level divergence that pumped mass away to the north of the depression.

The depression will move through an environment somewhat favorable for intensification during the next 24 hours. The depression will move over water where the Sea Surface Temperatures are near 28˚C. It will move under the western part of an upper level ridge centered over southeast Asia. The ridge will produce southeast winds that will blow toward the top of the depression. Those winds will cause moderate vertical wind shear and the shear will inhibit intensification. The depression is likely to intensify during the next 24 hours unless the upper level winds get stronger.

The depression will move south of a high pressure system centered over southeast Asia. The high pressure system will steer the depression slowly toward the northwest during the next 24 hours. On its anticipated track the depression will remain northeast of Sri Lanka and it will move closer to southern India.