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Former Tropical Cyclone Mandous Moves over Arabian Sea

The circulation of former Tropical Cyclone Mandous moved over the Arabian Sea on Tuesday. At 1:00 p.m. EST on Tuesday the center of Tropical Cyclone Mandous was located at latitude 12.6°N and longitude 71.8°E which put it about 215 miles (345 km) west of Mangaluru, India. Mandous was moving toward the west at 5 m.p.h. (8 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 1007 mb.

After making landfall on the coast of southeastern India between Puducherry and Chennai on Friday, Tropical Cyclone Mandous moved westward across southern India during the weekend. The circulation of former Tropical Cyclone Mandous emerged over the Arabian Sea west of India on Tuesday. The circulation around Mandous was still well organized. 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 and west of the former tropical cyclone.

Former 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 northwestern part of an upper level ridge over southern Asia and the Arabian Sea. The ridge will produce northwesterly winds will blow toward the top of Mandous’ circulation. Those wind will cause some vertical wind shear, but the wind shear will not be strong enough to prevent intensification. Former Tropical Cyclone Mandous could strengthen during the next 24 hours. Northeasterly winds in the lower levels are transporting drier air from Asia over the western Arabian Sea. Mandous is likely to weaken when it reaches the mass of drier air later this week.

Former Tropical Cyclone Mandous will move south of a high pressure system over southern Asia and the northern Arabian Sea. The high pressure system will steer Mandous toward the west during the next several days. On its anticipated track, former Tropical Cyclone Mandous will move farther away from the coast of southwest India.

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 Sitrang Brings Wind and Rain to Bangladesh

Tropical Cyclone Sitrang brought wind and rain to Bangladesh on Monday. At 5:00 p.m. EDT on Monday the center of Tropical Cyclone Sitrang was located at latitude 24.6°N and longitude 91.2°E which put it about 45 miles (75 km) northeast of Dhaka, Bangladesh. Sitrang was moving toward the north at 35 m.p.h. (55 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.

Tropical Cyclone Sitrang moved quickly across the northern Bay of Bengal and over Bangladesh on Monday. The heaviest rain was falling in bands in the northern side of Sitrang’s circulation. Bands in the southern half of Tropical Cyclone Sitrang consisted primarily of showers and lower clouds. Winds to tropical storm force extended out 60 miles (95 km) from the center of Sitrang.

A high pressure system over Southeast Asia will steer Tropical Cyclone Sitrang quickly toward the north-northeast during the next 24 hours. On its anticipated track Sitrang will move across Bangladesh and over northeastern India. Tropical Cyclone Sitrang will drop locally heavy rain over Bangladesh and northeastern India. Heavy rain could cause flash floods in some locations. Sitrang will weaken steadily as it moves farther inland.

Tropical Cyclone 04B Makes Landfall South-southwest of Kolkata

Tropical Cyclone 04B made landfall on the coast of India south-southwest of Kolkata on Friday. At 11:00 a.m. EDT on Friday the center of Tropical Cyclone 04B was located at latitude 21.9°N and longitude 87.7°E which put it about 65 miles (105 km) south-southwest of Kolkata India. The tropical cyclone was moving toward the west-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 990 mb.

Tropical Cyclone 04B strengthened during the hours prior to landfall. The maximum sustained wind speed was 50 m.p.h. (80 km/h) when Tropical Cyclone 04B made landfall on the coast of India south-southwest of Kolkata. Winds to tropical storm force extended out 85 miles (135 km) from the center of Tropical Cyclone 04B. Bands of showers and thunderstorms were revolving around a broad center of circulation.

Tropical Cyclone 04B will move south of a high pressure system over southern Asia. The high pressure system will steer the tropical cyclone toward the west-northwest during the next 48 hours. On its anticipated track Tropical Cyclone 04B will move farther inland over central India during the weekend. The tropical cyclone will gradually weaken when it moves farther inland. Tropical Cyclone 04B will drop heavy rain over parts of central India. Heavy rain could cause flash floods in some locations.

Tropical Cyclone 04B Forms over Northern Bay of Bengal

Tropical Cyclone 04B formed over the northern Bay of Bengal on Thursday afternoon. At 5:00 p.m. EDT on Thursday the center of Tropical Cyclone 04B was located at latitude 20.7°N and longitude 89.5°E which put it about 175 miles (280 km) southeast of Kolkata India. The tropical cyclone was moving toward the west-northwest at 9 m.p.h. (15 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 992 mb.

Tropical Cyclone 04B developed over the northern Bay of Bengal southeast of Koklata, India on Thursday afternoon. The distribution of thunderstorms around the tropical cyclone was asymmetrical. The strongest thunderstorms were occurring in bands in the southern and western parts of the circulation. Bands in the northern and eastern parts of Tropical Cyclone 04B consisted primarily of showers and lower clouds. An upper level ridge over southern Asia was producing easterly winds that were blowing toward the top of the tropical cyclone’s circulation. Those winds were causing moderate vertical wind shear and the wind shear was contribution to the asymmetrical distribution of thunderstorms. Winds to tropical storm force extended out 40 miles (65 km) from the center of Tropical Cyclone 04B.

Tropical Cyclone 04B will move through an environment somewhat favorable for intensification during the next 12 hours. The tropical cyclone will move over water where the Sea Surface Temperatures are near 29˚C. However, the upper level ridge over southern Asia will continue to cause moderate vertical wind shear. The wind shear will inhibit intensification. Tropical Cyclone 04B could intensify during the next 12 hours, if the upper level winds do not get any stronger.

Tropical Cyclone 04B will move south of a high pressure system over southern Asia. The high pressure system will steer the tropical cyclone toward the west-northwest during the next 24 hours. On its anticipated track the center of Tropical Cyclone 04B could be south of Kolkata in 12 hours. It could make landfall on the coast of India southwest of Kolkata in 18 hours. Tropical Cyclone 04B will bring gusty winds and locally heavy rain to the region of India south and west of Kolkata. Heavy rain could cause flash floods in some locations.

Tropical Cyclone Asani Makes Landfall in Andhra Pradesh

Tropical Cyclone Asani made landfall on the east coast of India in Andhra Pradesh on Tuesday night. At 11:00 p.m. EDT on Tuesday the center of Tropical Cyclone Asani was located at latitude 15.8°N and longitude 80.6°E which put it 25 miles (40 km) south of Tenali, India. Asani was moving toward the west-northwest at 7 m.p.h (11 km/h). The maximum sustained wind speed was 60 m.p.h. (95 km/h) and there were wind gusts to 75 m.p.h. (120 km/h). The minimum surface pressure was 986 mb.

The center of Tropical Cyclone Asani made landfall on the coast of Andhra Pradesh south of Tenali on Tuesday night. Asani was the equivalent of s strong tropical storm at the time of landfall. Winds to tropical storm force extended out 110 miles (175 km) from the center of Tropical Cyclone Asani. Thunderstorms in bands in the western and northern parts of Asani were dropping heavy rain in scattered areas near the coast of Andhra Pradesh.

Tropical Cyclone Asani will weaken steadily as it moves inland over Andhra Pradesh. The rainfall will become lighter when drier air over India is pulled into Asani’s circulation. The circulation around Tropical Cyclone Asani will become shallower when it weakens. Southwesterly winds in the lower levels over India and the Bay of Bengal could steer the weakened circulation of Asani toward the northeast later this week.

Tropical Cyclone Asani Nears East Coast of India

Tropical Cyclone Asani neared the east coast of India on Tuesday morning. At 5:00 a.m. EDT on Tuesday the center of Tropical Cyclone Asani was located at latitude 15.1°N and longitude 82.1°E which put it 90 miles (145 km) southeast of Machilipatnam, India and about about 210 miles (330 km) south-southeast of Visakhapatnam. Asani was moving toward the west at 13 m.p.h (20 km/h). The maximum sustained wind speed was 75 m.p.h. (120 km/h) and there were wind gusts to 90 m.p.h. (145 km/h). The minimum surface pressure was 977 mb.

Tropical Cyclone Asani maintained its intensity as it moved closer to the east coast of India on Tuesday morning. Winds to hurricane/typhoon force were occurring in an area 30 miles (50 km) north of the center of Asani’s circulation. Even though the intensity of Tropical Cyclone Asani was steady, the distribution of thunderstorms was asymmetrical. The strongest thunderstorms were occurring in bands in the southern and western parts of Asani’s circulation. Bands in the northern and eastern parts of Asani consisted primarily of showers and lower clouds. Storms southwest of the center of circulation generated upper level divergence that pumped mass away from the tropical cyclone. The removal of mass allowed Tropical Cyclone Asani to maintain its intensity. Winds to tropical storm force extended out 155 miles (250 km) from the center of Asani.

Tropical Cyclone Asani will move through an environment that will become more unfavorable for intensification during the next 12 hours. Asani will move over water where the Sea Surface Temperatures are near 30˚C. It will move under the southern part of an upper level ridge over South Asia. The upper level ridge will produce easterly winds that will blow toward the top of Tropical Cyclone Asani’s circulation. Those winds will cause moderate vertical wind shear. Asani will move toward a mass of drier air that is sinking over India. The moderate vertical wind shear and the sinking drier air are likely to cause Tropical Cyclone Asani to start to weaken as it approaches the east coast of India during the next 12 hours.

Tropical Cyclone Asani will move around the western side of a high pressure system over Southeast Asia. The high pressure system will steer Asani toward the northwest during the next 24 hours. On its anticipated track Tropical Cyclone Asani will reach the east coast of India near Machilipatnam within 18 hours. Asani will bring strong gusty winds and locally heavy rain to parts of Andhra Pradesh during the next 36 hours. Heavy rain could cause flash floods in some locations.

Tropical Cyclone Asani Moves Northwest across Bay of Bengal

Tropical Cyclone Asani moved northwest across the Bay of Bengal on Monday morning. At 5:00 a.m. EDT on Monday the center of Tropical Cyclone Asani was located at latitude 14.6°N and longitude 85.3°E which put it about 275 miles (445 km) southeast of Visakhapatnam, India and about 595 miles (965 km) south-southwest of Kolkata. Asani was moving toward the northwest at 9 m.p.h (15 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 980 mb.

The distribution of thunderstorms in Tropical Cyclone Asani became more asymmetrical on Monday morning as Asani moved northwest across the western Bay of Bengal. The strongest thunderstorms were occurring in bands in the western half of Asani’s circulation. Bands in the western half of the circulation consisted primarily of showers and lower clouds. Storms just west of the center of circulation generated upper level divergence that pumped mass away from the tropical cyclone. Winds to tropical storm force extended out 130 miles (210 km) from the center of Tropical Cyclone Asani.

Tropical Cyclone Asani will move through an environment that will become more unfavorable for intensification during the next 24 hours. Asani will move over water where the Sea Surface Temperatures are near 30˚C. It will move under the southern part of an upper level ridge over South Asia. The upper level ridge will produce easterly winds that will blow toward the top of Tropical Cyclone Asani’s circulation. Those winds will cause moderate vertical wind shear. Asani will move toward a mass of drier air that is sinking in the ridge over South Asia. The moderate vertical wind shear and the sinking drier air are likely to cause Asani to start to weaken during the next 24 hours.

Tropical Cyclone Asani will move around the western side of a high pressure system over Southeast Asia. The high pressure system will steer Asani toward the northwest during the next 24 hours. On its anticipated track Tropical Cyclone Asani will move toward the east coast of India. Asani could approach of Visakhapatnam in 48 hours.