Tag Archives: 05B

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 Sitrang Develops over Northern Bay of Bengal

Tropical Cyclone Sitrang developed over the northern Bay of Bengal on Sunday. At 11:00 p.m. EDT on Sunday the center of Tropical Cyclone Sitrang was located at latitude 18.3°N and longitude 89.4°E which put it about 360 miles (580 km) south-southwest of Chittagong, Bangladesh. Sitrang was moving toward the north-northeast at 13 m.p.h. (20 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 circulation around a low pressure system over the northern Bay of Bengal strengthened on Sunday and the India Meteorological Department designated the system as Tropical Cyclone Sitrang. The distribution of thunderstorms around Sitrang was asymmetrical. Thunderstorms were occurring in bands in the northern side of Tropical Cyclone Sitrang. Bands near the center of Sitrang’s circulation and in the southern half of the tropical cyclone consisted primarily of showers and lower clouds. Tropical Cyclone Sitrang was moving under the western end of an upper level ridge over Southeast Asia and the Bay of Bengal. The ridge was producing southerly winds that were blowing toward the top of Sitrang’s circulation. Those winds were causing moderate vertical wind shear and they were also causing the asymmetrical distribution of thunderstorms. Winds to tropical storm force extended out 60 miles in the eastern side of Tropical Cyclone Sitrang. The winds in the western half of Sitrang were blowing at less than tropical storm force.

Tropical Cyclone Sitrang will move through an environment somewhat favorable for intensification during the next 18 hours. Sitrang will move over water where the Sea Surface Temperatures are near 30˚C. However, the upper level ridge over Southeast Asia and the Bay of Bengal will continue to cause moderate vertical wind shear. The wind shear will inhibit intensification. Tropical Cyclone Sitrang could strengthen during the next 18 hours before it makes landfall in Bangladesh.

Tropical Cyclone Sitrang will move around the western end of a high pressure system over Southeast Asia. The high pressure system will steer Sitrang toward the north-northeast during the next 24 hours. On its anticipated track Tropical Cyclone Sitrang will reach Bangladesh in less than 24 hours. Sitrang will bring gusty winds and locally heavy rain to Bangladesh. Heavy rain could cause flash floods in some locations. Tropical Cyclone Sitrang could cause a storm surge of five feet (1.5 meters) along the coast of Bangladesh.

Tropical Cyclone Jawad Spins over Bay of Bengal

Tropical Cyclone Jawad was spinning over the Bay of Bengal east of India on Friday night. At 10:00 p.m. EST on Friday the center of Tropical Cyclone Jawad was located at latitude 16.0°N and longitude 85.0°E which put it about 150 miles (240 km) southeast of Visakhapatnam, India. Jawad was moving toward the north 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.

Tropical Cyclone Jawad continued to spin over the Bay of Bengal east of India on Friday night. An upper level ridge over the Bay of Bengal was producing southeasterly winds that were blowing toward the top of Jawad’s circulation. Those winds were causing moderate vertical wind shear and the shear was keeping Tropical Cyclone Jawad from getting stronger. The strongest thunderstorms in Jawad were occurring in the northern half of the circulation because of the vertical wind shear. Bands in the southern half of the circulation consisted primarily of showers and lower clouds. Winds to tropical storm force extended out 100 miles (160 km) from the center of Tropical Cyclone Jawad.

Tropical Cyclone Jawad will move through an environment only marginally favorable for intensification during the next 24 hours. Jawad will move over water where the Sea Surface Temperatures are near 28˚C. It will move under the western end of an upper level ridge over the Bay of Bengal. The ridge will continue to produce southerly winds that will blow toward the top of Jawad’s circulation. Those winds will cause moderate vertical wind shear. The wind shear is likely to remain strong enough to prevent Tropical Cyclone Jawad from strengthening during the next 24 hours.

Tropical Cyclone Jawad will move around the western end of a high pressure system over southeast Asia. The high pressure system will steer Jawad toward the north-northeast during the next several days. On its anticipated track Tropical Cyclone Jawad will move parallel to the east coast of India during the next 36 hours. Jawad could approach Kolkata in 72 hours. Tropical Cyclone Jawad could bring gusty winds and locally heavy rain to the coastal parts of northeastern Andhra Pradesh, Odisha, and West Bengal.

Tropical Cyclone 05B Forms over Bay of Bengal

Tropical Cyclone 05B formed over the Bay of Bengal on Thursday night. At 10:00 p.m. EST on Thursday the center of Tropical Cyclone 05B was located at latitude 14.4°N and longitude 85.8°E which put it about 360 miles (580 km) southeast of Visakhapatnam, India. Tropical Cyclone 05B was moving toward the northwest at 16 m.p.h. (26 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 central Bay of Bengal strengthened on Thursday night into Tropical Cyclone 05B. The distribution of thunderstorms around Tropical Cyclone 05B was asymmetrical. The strongest thunderstorms were occurring in bands in the northern half of the tropical cyclone. Bands in the southern half of the circulation consisted primarily of showers and lower clouds. The thunderstorms in the northern half of the circulation generated upper level divergence that pumped mass away to the north of the tropical cyclone. The distribution of wind speeds was also asymmetrical. Winds to tropical storm force extended out 150 miles (240 km) in the northern half of the tropical cyclone. The winds in the southern half of the circulation were blowing at less than tropical storm force.

Tropical Cyclone 05B will move through an environment favorable for intensification during the next 24 hours. The tropical cyclone will move over water where the Sea Surface Temperatures are near 28˚C. It will move under the western end of an upper level ridge over the Bay of Bengal. The ridge will produce southerly winds that will blow toward the top of the tropical cyclone. Those winds will cause some vertical wind shear, but the wind shear will not be strong enough to prevent intensification. Tropical Cyclone 05B is likely to intensify during the next 24 hours. The India Meteorological Department will likely give the tropical cyclone a name on Friday.

Tropical Cyclone 05B will move around the western end of a high pressure system over southeast Asia. The high pressure system will steer the tropical cyclone toward the northwest during the next 24 hours. On its anticipated track Tropical Cyclone 05B will approach the coast of India northeast of Visakhapatnam in 24 hours. It will bring gusty winds and locally heavy rain to the coastal parts of northeastern Andhra Pradesh and Orissa. Tropical Cyclone 05B will move more slowly after it nears the coast and it could turn toward the northeast during the weekend.

Tropical Cyclone Burevi Stalls over Gulf of Mannar

Tropical Cyclone Burevi stalled over the Gulf of Mannar on Friday. At 4:00 p.m. EST on Friday the center of Tropical Cyclone Burevi was located at latitude 9.0°N and longitude 79.4°E which put it about 80 miles (130 km) east of Toothukudi, India. Burevi was nearly stationary. 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 Burevi stalled over the Gulf of Mannar between Sri Lanka and the southern tip of India on Friday. Although the center of Burevi was over water, the tropical cyclone weakened since some of the circulation passed over Sri Lanka or southern India. The parts of the circulation that were over land experienced increased friction and were unable to extract as much energy from the surface. The wind speeds around Tropical Cyclone Burevi decreased gradually as a result of more friction and less available energy.

Tropical Cyclone Burevi dropped locally heavy rain over parts of southern Tamil Nadu and Kerala in India. Persistent rain fell in some locations because Burevi stalled. If the rain continues to fall over the same locations, then flash floods are likely to occur.

A high pressure system over India could start to push Tropical Cyclone Burevi toward the west during the weekend. Burevi will weaken further if the center moves across southern India. Tropical Cyclone Burevi could strengthen slowly next week, if the circulation is still relatively intact when it reaches the Arabian Sea.

Tropical Cyclone Burevi Rains on Sri Lanka and Southern India

Tropical Cyclone Burevi dropped rain on northern Sri Lanka and southern India on Wednesday night. At 10:00 p.m. EST on Wednesday the center of Tropical Cyclone Burevi was located at latitude 9.1°N and longitude 80.4°E which put it about 50 miles (80 km) south-southeast of Jaffna, Sri Lanka. Burevi was moving toward the west at 8 m.p.h. (13 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 center of Tropical Cyclone Burevi made landfall on the coast of Sri Lanka north of Trincomalee on Wednesday. The center moved westward across northern Sri Lanka after it made landfall. Bands of showers and thunderstorms in the northern and western parts of Burevi dropped rain over northern Sri Lanka, southern Tamil Nadu and southern Kerala. Prolonged rain could cause flash floods in some locations.

Tropical Cyclone Burevi could weaken during the next few hours while the center is over northern Sri Lanka. The center of Burevi will move over the Gulf of Mannar in a few hours. The center of Tropical Cyclone Burevi could make another landfall on the coast of southern India near Thoothukudi in about 18 hours. Burevi will move across the southernmost parts of Tamil Nadu and Kerala. Tropical Cyclone Burevi could move over the Arabian Sea in about 36 hours. Burevi could slowly strengthen when it moves over the Arabian Sea.

Tropical Cyclone Burevi Strengthens East of Sri Lanka

Tropical Cyclone Burevi strengthened over the Bay of Bengal east of Sri Lanka on Tuesday. At 10:00 a.m. EST on Tuesday the center of Tropical Cyclone Burevi was located at latitude 8.0°N and longitude 84.4°E which put it about 220 miles (350 km) east of Trincomalee, Sri Lanka. Burevi was moving toward the 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. (110 km/h). The minimum surface pressure was 1000 mb.

A former tropical depression over the Bay of Bengal east of Sri Lanka strengthened into Tropical Cyclone Burevi on Tuesday. More thunderstorms formed close to the center of circulation. More thunderstorms also formed in bands revolving around the center of Burevi. Storms near the center generated upper level divergence which pumped mass away from the tropical cyclone. Winds to tropical storm force extended out 110 miles from the center of Tropical Cyclone Burevi.

Tropical Cyclone Burevi will move through a region favorable for intensification during the next 24 hours. Burevi will move over water where the Sea Surface Temperature is near 29°C. It will move under the eastern end of an upper level ridge centered over India. The upper winds will be weaker during the next day or so and there will be less vertical wind shear. Tropical Cyclone Burevi will intensify during the next 24 hours.

Tropical Cyclone Burevi will move south of a high pressure system over India and the Bay of Bengal. The high will steer Burevi toward the west-northwest during the next several days. On its anticipated track the center of Tropical Cyclone Burevi will approach northern Sri Lanka in about 24 hours. Burevi will bring gusty winds to the northeast coast of Sri Lanka and the coastal waters around southern India. Tropical Cyclone Burevi will drop heavy rain over parts of Sri Lanka and southern India. Flash floods could occur in portions of Sri Lanka, southern Tamil Nadu and southern Kerala.

Tropical Cyclone Vardah Nears Somalia

Tropical Cyclone Vardah neared landfall in Somalia late on Sunday.  At 7:00 p.m. EST on Sunday the center of Tropical Cyclone Vardah was located at latitude 8.9°N and longitude 51.2°E which put it about 80 miles (130 km) east of Eyl, Somalia.  Vardah was moving toward the west at 17 m.p.h. (27 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. (70 km/h).  The minimum surface pressure was 1005 mb.

Tropical Cyclone Vardah has a small but well organized circulation.  A couple of rainbands wrap tightly near the center of circulation.  The are several other thin bands of showers.  Thunderstorms near the center are generating upper level divergence.  There is a distinct low level circulation, but it only extends about 120 miles (195 km) from the center.

Tropical Cyclone Vardah is being steering a little south of due west by a subtropical ridge north of the cyclone.  That general motion is expected to continue and Vardah could make landfall on the coast of Somalia in about 12 hours.  Tropical Cyclone Vardah could bring gusty winds and locally heavy rain where the center moves into Somalia.

Tropical Cyclone Vardah Moves Closer to Somalia

Tropical Cyclone Vardah moved closer to Somalia on Saturday.  At 7:00 p.m. EST on Saturday  the center of Tropical Cyclone Vardah was located at latitude 9.3°N and longitude 56.9°E which put it about 465 miles (745 km) east of Eyl, Somalia.  Vardah was moving toward the west-southwest at 18 m.p.h. (28 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. (70 km/h).  The minimum surface pressure was 1004 mb.

Tropical Cyclone Vardah has a small but well defined circulation.  Several rainbands wrap close to the center.  However, the rainbands are thin and thunderstorms are scattered along them.  It appears that the circulation is pulling in drier air from the surrounding environment.  The thunderstorms near the core of the circulation are generating some upper level divergence.

Environmental conditions around Tropical Cyclone Vardah contain both positive and negative factors.  Vardah is moving over water where the Sea Surface Temperature is near 27°C.  So, there is enough energy in the upper ocean to support intensification.  The winds in the upper levels are not very strong and there is little vertical wind shear.  Drier air seems to be the primary negative factor that is preventing intensification of Tropical Cyclone Vardah.  The drier air could prevent significant intensification of Vardah, but the low level circulation could be strong enough to persist for several more days.

A strong subtropical ridge north of Vardah is steering the tropical cyclone toward the west-southwest and that general motion is expected to continue for several more days.  On its anticipated track Tropical Storm Vardah could approach the coast of Somalia in a little over 24 hours.

Tropical Cyclone Vardah is small.  It could produce gusty winds when it reaches the coast.  Isolated areas could also receive locally heavy rain.

Tropical Cyclone Vardah Reorganizes Over the Arabian Sea

After moving across southern India and weakening Tropical Cyclone Vardah began to reorganize over the eastern Arabian Sea on Thursday.  At 7:00 p.m. EST on Thursday the center of Tropical Cyclone Vardah was located near latitude 11.0°N and longitude 68.0°E which put it about 1140 miles (1840 km) east of Baargaal, Somalia.  Vardah was moving toward the west at 7 m.p.h. (11 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 1007 mb.

Tropical Cyclone Vardah retained a well organized low level circulation as it moved across southern India and into the eastern Arabian Sea.  However, almost all of the showers and thunderstorms dissipated as the cyclone crossed over land.  A few showers and thunderstorms began to redevelop about 24 hours ago.  There are now several rainbands that are spiraling around the circulation and stronger thunderstorms are forming in some of those bands.  The thunderstorms are beginning to produce upper level divergence.

Tropical Cyclone Vardah will be moving through an environment that is favorable for intensification.  Vardah will be moving over water where the Sea Surface Temperature is near 28°C.  The upper level winds are weak and there is not much vertical wind shear.  Tropical Cyclone Vardah should continue to redevelop during the next 24 hours.

A subtropical ridge to the north of Vardah has been steering the tropical cyclone toward the west and that general motion is expected to continue.  On its anticipated track Tropical Cyclone Vardah will move across the Arabian Sea toward eastern Africa during the next several days.