Tag Archives: 01B

Typhoon Ewiniar Moves Away From Luzon

Typhoon Ewiniar moved away from Luzon on Monday. At 11:00 a.m. EDT on Monday the center of Typhoon Ewiniar was located at latitude 17.4°N and longitude 124.3°E which put it about 185 miles (300 km) east of Tuguegarao, Philippines. Ewiniar was moving toward the northeast at 9 m.p.h. (15 km/h). The maximum sustained wind speed was 100 m.p.h. (160 km/h) and there were wind gusts to 120 m.p.h. (195 km/h). The minimum surface pressure was 966 mb.

After intensifying rapidly on Sunday, Typhoon Ewiniar showed signs of weakening on Monday. A small eye with a diameter of 5 miles (8 km) was still present at the center of Ewiniar’s circulation. However, there were breaks in the ring of thunderstorms surrounding the eye. Storms near the center of Ewiniar still were generating upper level divergence that was pumping mass away from the typhoon. Bands of showers and thunderstorms were revolving around the center of Typhoon Ewiniar.

The circulation around Typhoon Ewiniar was small. Winds to typhoon force extended out 20 miles (30 km) from the center of Ewiniar’s circulation. Winds to tropical storm force extended out 75 miles (120 km) from the center of circulation.

Typhoon Ewiniar will move through an environment that will become less favorable for intensification during the next 24 hours. Ewiniar will move over water where the Sea Surface Temperatures are near 30°C. An upper level trough near the east coast of China will produce southwesterly winds that will blow toward the top of Ewiniar’s circulation. Those winds will cause the vertical wind shear to increase. Since the circulation around Ewiniar is small, an increase in wind shear will have a larger effect on the typhoon. Typhoon Ewiniar is likely to weaken during the next 24 hours when the vertical wind shear increases.

Typhoon Ewiniar will move around the northwestern part of a high pressure system over the Western North Pacific Ocean. The high pressure system and the upper level trough near the east coast of China will steer Ewiniar toward the northeast during the next 24 hours. On its anticipated track, Typhoon Ewiniar will continue to move farther away from Luzon. Ewiniar will pass southeast of the Ryukyu Islands during the next few days.

Elsewhere, Tropical Cyclone Remal continued to drop heavy rain on Bangladesh. There were reports that Remal caused fatalities in Bangladesh. At 5:00 a.m. EDT on Monday the center of Tropical Cyclone Remal was located at latitude 23.1°N and longitude 89.2°E which put it about 85 miles (140 km) southwest of Dhaka, Bangladesh. Remal was moving toward the north-northeast at 5 m.p.h. (8 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 979 mb.

Tropical Cyclone Remal Brings Wind and Rain to West Bengal and Bangladesh

Tropical Cyclone Remal brought wind and rain to West Bengal and Bangladesh on Sunday. At 5:00 p.m. EDT on Sunday the center of Tropical Cyclone Remal was located at latitude 22.0°N and longitude 88.5°E which put it about 65 miles (105 km) south of Kolkata, India. Remal was moving toward the north 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 978 mb.

The center of Tropical Cyclone Remal made landfall on the coast of West Bengal south of Kolkata on Sunday. The circulation around Remal was large at the time of landfall. Winds to tropical storm force extended out 165 miles (265 km) from the center of Remal’s circulation. A weather station at Mongla, Bangladesh reported a sustained wind speed of 47 m.p.h. (76 km/h).

Tropical Cyclone Remal was moving along with the leading edge of a surge of humid air moving north in the monsoonal flow over the Bay of Bengal. The monsoonal flow will steer Remal toward the northeast during the next 24 hours. On its anticipated track Tropical Cyclone Remal will move inland across Bangladesh.

Tropical Cyclone Remal will weaken gradually as it moves farther inland. Remal will continue to bring strong winds and locally heavy rain to Bangladesh and adjacent parts West Bengal. Heavy rain is likely to cause floods in some locations. Remal could also cause a storm surge of up to 7 feet (2 meters) along the coast of Bangladesh. Weather conditions should start to improve gradually on Monday when Tropical Cyclone Remal moves farther inland and weakens.

Tropical Cyclone Remal Approaches Bangladesh

Tropical Cyclone Remal was approaching the coast of Bangladesh and West Bengal on Sunday morning. At 5:00 a.m. EDT on Sunday the center of Tropical Cyclone Remal was located at latitude 20.7°N and longitude 88.9°E which put it about 155 miles (250 km) south-southeast of Kolkata, India. Remal was moving toward the north at 11 m.p.h. (17 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 985 mb.

Tropical Cyclone Remal was strengthening as it approached the coast of Bangladesh and West Bengal on Sunday morning. Even though Remal was getting stronger, the distribution of thunderstorms was asymmetrical. Most of the thunderstorms were occurring in bands in the southern half of Remal’s circulation. Bands in the northern part of Tropical Cyclone Remal consisted primarily of showers and lower clouds. Storms near the center of Remal’s circulation generated upper level divergence that pumped mass away from the tropical cyclone. The removal of mass caused the surface pressure to decrease.

The circulation around Tropical Cyclone Remal was large. Winds to tropical storm force extended out 190 miles (305 km) from the center of Remal’s circulation.

Tropical Cyclone Remal will move through an environment favorable for intensification during the next 12 hours. Remal will move over water where the Sea Surface Temperatures are near 31°C. It will move under the axis of an upper level ridge over South Asia and the Bay of Bengal. The winds are weak near the axis off the ridge and there will be little vertical wind shear. Tropical Cyclone Remal is likely to intensify during the next 12 hours. The large circulation around Remal could cause intensification to occur slowly.

Tropical Cyclone Remal formed along the leading edge of a surge of humid air moving north in the monsoonal flow over the Bay of Bengal. The monsoonal flow will continue to steer Remal north during the next 12 hours. On its anticipated track Tropical Cyclone Remal will reach the northern coast of the Bay of Bengal in 12 hours. The center of Remal is likely to make landfall near the western border between India and Bangladesh.

Tropical Cyclone Remal will bring strong winds and locally heavy rain to Bangladesh and adjacent parts West Bengal. Heavy rain is likely to cause floods in some locations. Remal could also cause a storm surge of up to 7 feet (2 meters) along the coast of Bangladesh.

Tropical Cyclone Remal Forms over Bay of Bengal

Tropical Cyclone Remal formed over the Bay of Bengal on Saturday. At 11:00 a.m. EDT on Saturday the center of Tropical Cyclone Remal was located at latitude 19.1°N and longitude 89.4°E which put it about 110 miles (175 km) south-southeast of Kolkata, India. Remal was moving toward the north 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 993 mb.

A low pressure system over the Bay of Bengal strengthened on Saturday and the India Meteorological Department designated the system as Tropical Cyclone Remal. The distribution of thunderstorms around Tropical Cyclone Remal was asymmetrical. Thunderstorms were occurring in bands in the southern half of Remal’s circulation. Bands in the northern part of Tropical Cyclone Remal consisted primarily of showers and lower clouds. Storms near the center of Remal’s circulation generated upper level divergence that pumped mass away from the tropical cyclone.

The circulation around Tropical Cyclone Remal was large. Winds to tropical storm force extended out 175 miles (280 km) from the center of Remal’s circulation.

Tropical Cyclone Remal will move through an environment favorable for intensification during the next 24 hours. Remal will move over water where the Sea Surface Temperatures are near 31°C. It will move under the axis of an upper level ridge over South Asia and the Bay of Bengal. The winds are weak near the axis off the ridge and there will be little vertical wind shear. Tropical Cyclone Remal will intensify during the next 24 hours. The large circulation around Remal could cause intensification to occur slowly.

Tropical Cyclone Remal formed along the leading edge of a surge of humid air moving north in the monsoonal flow over the Bay of Bengal. The monsoonal flow will continue to steer Remal north during the next 24 hours. On its anticipated track Tropical Cyclone Remal will approach the northern coast of the Bay of Bengal in 24 hours. The center of Remal is likely to make landfall between Kolkata, India and Chittagong, Bangladesh.

Tropical Cyclone Remal will bring strong winds and locally heavy rain to Bangladesh and adjacent parts West Bengal. Heavy rain is likely to cause floods in some locations. Remal could also cause a storm surge of up to 7 feet (2 meters) along the coast of Bangladesh.

Tropical Cyclone Mocha Hits Myanmar

Tropical Cyclone Mocha hits Myanmar on Sunday morning. At 5:00 a.m. EDT on Sunday the center of Tropical Cyclone Mocha was located at latitude 20.5°N and longitude 93.0°E which put it about 20 miles (30 km) north-northeast of Sittwe, Myanmar. Mocha was moving toward the northeast at 16 m.p.h. (26 km/h). The maximum sustained wind speed was 155 m.p.h. (250 km/h) and there were wind gusts to 195 m.p.h. (315 km/h). The minimum surface pressure was 919 mb.

The center of powerful Tropical Cyclone Mocha made landfall on the coast of Myanmar near Sittwe on Sunday morning. Mocha was near its peak intensity at the time of landfall. A circular eye with a diameter of 20 miles (32 km) was present at the center of Mocha’s circulation. A ring of strong thunderstorms surrounded the eye and the strongest winds were occurring in ring of storms. Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Mocha.

Tropical Cyclone Mocha intensified to the equivalent of a Category 4 hurricane on the Saffir-Simpson Scale at the time of landfall. Winds to hurricane/typhoon force extended out 40 miles (65 km) from the center of Mocha’s circulation. Winds to tropical storm force extended out 200 miles (320 km) from the center. The Hurricane Intensity Index (HII) for Tropical Cyclone Mocha was 33.2. The Hurricane Size Index (HSI) was 14.7 and the Hurricane Wind Intensity Size Index (HWISI) was 47.9. Tropical Cyclone Mocha was similar in size and intensity to Hurricane Michael when Michael hit Northwest Florida in 2018. Tropical Cyclone Mocha was capable of causing regional severe damage.

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 northeast during the next 24 hours. Tropical Cyclone Mocha will bring very strong winds and locally heavy rain to Myanmar. The strong winds and heavy rain are likely to cause severe damage. Heavy rain is likely to cause flash floods in some locations. Mocha could also cause a storm surge of up to 13 feet (4 meters) along portions of the coast where the wind blows the water toward the shore. Tropical Cyclone Mocha will also bring gusty winds and heavy rain to eastern Bangladesh.

Powerful Tropical Cyclone Mocha Nears Myanmar and Bangladesh

Powerful Tropical Cyclone Mocha was nearing the coast of the Bay of Bengal near the border between Myanmar and Bangladesh on Saturday afternoon. At 5:00 p.m. EDT on Saturday the center of Tropical Cyclone Mocha was located at latitude 18.4°N and longitude 91.4°E which put it about 150 miles (240 km) south-southwest of Sittwe, Myanmar. Mocha was moving toward the north-northeast at 9 m.p.h. (15 km/h). The maximum sustained wind speed was 150 m.p.h. (240 km/h) and there were wind gusts to 185 m.p.h. (295 km/h). The minimum surface pressure was 926 mb.

Tropical Cyclone Mocha continued to intensify on Saturday. A circular eye with a diameter of 20 miles (32 km) was present at the center of Mocha’s circulation. A ring of strong thunderstorms surrounded the eye and the strongest winds were occurring in that band of storms. Storms near the center of circulation generated strong upper level divergence that pumped a large quantity of mass away from the tropical cyclone. The removal of a large quantity of mass allowed the surface pressure to decrease to 926 mb.

Tropical Cyclone Mocha intensified to the equivalent of a Category 4 hurricane on the Saffir-Simpson Scale on Saturday. Winds to hurricane/typhoon force extended out 35 miles (55 km) from the center of Mocha’s circulation. Winds to tropical storm force extended out 175 miles (280 km) from the center. The Hurricane Intensity Index (HII) for Tropical Cyclone Mocha was 31.6. The Hurricane Size Index (HSI) was 12.0 and the Hurricane Wind Intensity Size Index (HWISI) was 43.6. Tropical Cyclone Mocha was similar in size and intensity to Hurricane Ida when Ida hit southeast Louisiana in 2021. Tropical Cyclone Mocha was capable of causing regional severe damage.

Tropical Cyclone Mocha will move through an environment favorable for a powerful tropical cyclone during the next few 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 is likely to maintain its intensity until it reaches land.

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-northeast during the next 24 hours. Tropical Cyclone Mocha is likely to make landfall between Cox’s Bazar, Bangladesh and Sittwe, Myanmar in less than 12 hours. Mocha will be the equivalent of a major hurricane when it makes landfall. Tropical Cyclone Mocha will bring very strong winds and locally heavy rain to Myanmar and Bangladesh. The strong wind and rain is likely to cause severe damage. Heavy rain is likely to cause flash floods in some locations. Mocha could also cause a storm surge of up to 13 feet (4 meters) along portions of the coast where the wind blows the water toward the shore.

Tropical Cyclone Mocha Strengthens to Equivalent of a Major Hurricane

Tropical Cyclone Mocha strengthened to the equivalent of a major hurricane over the Bay of Bengal on Friday. At 5:00 p.m. EDT on Friday the center of Tropical Cyclone Mocha was located at latitude 15.2°N and longitude 88.9°E which put it about 545 miles (880 km) south-southwest of Cox’s Bazar, Bangladesh. Mocha was moving toward the north-northeast at 5 m.p.h. (8 km/h). The maximum sustained wind speed was 125 m.p.h. (200 km/h) and there were wind gusts to 155 m.p.h. (250 km/h). The minimum surface pressure was 945 mb.

Tropical Cyclone Mocha rapidly intensified to the equivalent of a major hurricane over the Bay of Bengal on Friday. A circular eye was present at the center of Mocha’s circulation. A ring of strong thunderstorms surrounded the eye and the strongest winds were occurring in that band of storms. Storms near the center of circulation generated strong upper level divergence that pumped a large quantity of mass away from the tropical cyclone. The removal of mass allowed the surface pressure to decrease rapidly.

The circulation around Tropical Cyclone Mocha was large. Winds to hurricane/typhoon force extended out 35 miles (55 km) from the center of Mocha’s circulation. Winds to tropical storm force extended out 200 miles (320 km) from the center. The Hurricane Intensity Index (HII) for Tropical Cyclone Mocha was 23.6. The Hurricane Size Index (HSI) was 12.6 and the Hurricane Wind Intensity Size Index (HWISI) was 36.2. Tropical Cyclone Mocha was capable of causing major damage.

Tropical Cyclone Mocha will move through an environment favorable for intensification during the next 24 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 is likely to intensify during the next 24 hours.

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-northeast during the next 48 hours. Tropical Cyclone Mocha is likely to make landfall near the border between Bangladesh and Myanmar during the weekend. Mocha is likely to 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 13 feet (4 meters) along portions of the coast where the wind blows the water toward the shore.

Tropical Cyclone Mocha Intensifies to Equivalent of Hurricane/Typhoon

Tropical Cyclone Mocha intensified to the equivalent of a hurricane/typhoon over the Bay of Bengal on Thursday night. At 11:00 p.m. EDT on Thursday the center of Tropical Cyclone Mocha was located at latitude 13.6°N and longitude 88.3°E which put it about 670 miles (1080 km) south-southwest of Cox’s Bazar, Bangladesh. Mocha was moving toward the north at 7 m.p.h. (11 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 981 mb.

Tropical Cyclone Mocha intensified rapidly to the equivalent of a hurricane/typhoon on Thursday. The inner end of a rainband wrapped around the center of Mocha’s circulation. An eye was evident at the center of Tropical Cyclone Mocha on microwave satellite images. The eye was surrounded by a ring of strong thunderstorms and the strongest winds were occurring in that ring of storms. Bands of showers and thunderstorms were revolving around the core of Mocha’s circulation. Storms near the center of circulation generated strong upper level divergence that pumped mass away from the tropical cyclone. The removal of mass caused the surface pressure to decrease steadily. Winds to hurricane/typhoon force extended out 35 miles (55 km) from the center of Tropical Cyclone Mocha. Winds to tropical storm force extended out 200 miles (320 km) from the center of Mocha’s circulation.

Tropical Cyclone Mocha will move through an environment very favorable for intensification during the next 36 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 36 hours. Mocha could intensify rapidly at times. Mocha is likely to intensify to the equivalent of a major hurricane within 36 hours .

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-northeast during the next 48 hours. Tropical Cyclone Mocha is likely to make landfall near the border between Bangladesh and Myanmar during the weekend. Mocha is likely to 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 13 feet (4 meters) along portions of the coast where the wind blows the water toward the shore.

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 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.