Tag Archives: Pakistan

Tropical Cyclone Gulab Redevelops over the Arabian Sea

Tropical Cyclone Gulab redeveloped over the Arabian Sea on Thursday. At 5:00 p.m. EDT on Thursday the center of Tropical Cyclone Gulab was located at latitude 22.8°N and longitude 65.1°E which put it about 175 miles (280 km) south-southwest of Karachi, Pakistan. Gulab was moving toward the west at 15 m.p.h. (24 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 994 mb.

Tropical Cyclone Gulab redeveloped over the Arabian Sea south of Pakistan on Thursday. Gulab originally formed over the northern Bay of Bengal a few days ago. Gulab made landfall on the coast of India near Tekkali and then it moved westward across India. Even though Tropical Cyclone Gulab weakened after it made landfall, the circulation remained relatively intact because of a favorable upper level environment. There was not a lot of vertical wind shear. In fact, upper level divergence continued to pump away mass and allow the surface low pressure system to persist. The circulation began to intensify as Gulab approached the Arabian Sea and it strengthened once the low level center was back over water.

The circulation around Tropical Cyclone Gulab exhibited more organization on Thursday. More thunderstorms developed in bands revolving around the center of Gulab. The strongest thunderstorms were occurring in bands in the southern half of Tropical Cyclone Gulab. Bands in the northern half of the circulation consisted primarily of showers and lower clouds. The northern half of Gulab appeared to be pulling drier air from Asia into its circulation. Winds to tropical storm force extended out 140 miles (220 km) on the northern side of Tropical Cyclone Gulab. Winds to tropical storm force extended out 60 miles (95 km) on the southern side of the circulation.

Tropical Cyclone Gulab will move through an environment favorable for intensification during the next 36 hours. Gulab 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 Southwest Asia and the northern Arabian Sea. The upper level winds are weak near the middle of the ridge and there will be little vertical wind shear. Dry air from Asia could continue to limit the development of thunderstorms in the northern half of Gulab. Tropical Cyclone Gulab will intensify during the next 36 hours and it could strengthen to the equivalent of a hurricane/typhoon.

Tropical Cyclone Gulab will move around the southern side of a high pressure system over Southwest Asia. The high will steer Gulab toward the west during the next 36 hours. On its anticipated track Tropical Cyclone Gulab could approach the coast of Oman near Muscat in 60 hours.

Tropical Cyclone Forms Southwest of Mumbai

A tropical cyclone formed southwest of Mumbai, India on Thursday.  At 11:00 p.m. EDT on Thursday the center of Tropical Cyclone 04A was located at latitude 15.7°N and longitude 71.3°E which put it about 200 miles (320 km) southwest of Mumbai, India.  It was moving toward the north at 2 m.p.h. (3 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.

A distinct low level center of circulation formed within a broad area of low pressure over the Arabian Sea west of India.  Thunderstorms were developing near the low level center.  Bands of showers and thunderstorms were forming and the bands began to revolve around the center of circulation.  Storms near the center started to generate upper level divergence which was pumping mass away from the tropical cyclone.  Winds to tropical storm force extended out 105 miles (165 km) from the center of circulation.

Tropical Cyclone 04A will move through an environment favorable for intensification during the next 48 to 72 hours.  It will move over water where the Sea Surface Temperature is near 29°C.  The tropical cyclone will move through a region where the upper level wind are weak and there will be little vertical wind shear.  Tropical Cyclone 04A will continue to intensify and it is likely to strengthen into the equivalent of a hurricane/typhoon within 24 to 36 hours.

Tropical Cyclone 04A will move south of a high pressure system that extends from India across the northern Arabian Sea.  The high will steer the tropical cyclone in a west-northwesterly direction.  On its anticipated track Tropical Cyclone 04A should start to move away from India during the next 24 hours.  The tropical cyclone could approach Oman in about five days

Tropical Cyclone Vayu Weakens South of Pakistan

Tropical Cyclone Vayu weakened over the Arabian Sea south of Pakistan on Saturday.  At 11:00 p.m. EDT on Saturday the center of Tropical Cyclone Vayu was located at latitude 24.2°N and longitude 65.3°E which put it about 275 miles (445 km) south-southwest of Karachi, Pakistan.  Vayu was moving toward the northwest at 8 m.p.h. (13 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 985 mb.

The low level circulation around Tropical Cyclone Vayu remained well organized on Saturday, but the distribution of thunderstorms was asymmetrical.  The stronger thunderstorms were occurring in the southern half of the former eyewall and in several rainbands in the southern half of the circulation.  The strongest winds were occurring in the remaining portion of the eyewall.  Bands in the northern half of the circulation consisted primarily of showers and lower clouds.  Winds to tropical storm force extended out about 150 miles (240 km) from the center of circulation.

The circulation around Tropical Cyclone Vayu continued to draw drier air into the northern half of the tropical cyclone on Saturday.  An upper level ridge north of Vayu was producing strong northeasterly winds which were blowing toward the top of the circulation.  Those winds were causing moderate vertical wind shear.  The drier air and wind shear were the primary factors causing the asymmetrical distribution of thunderstorms.

Tropical Cyclone Vayu will move through an environment unfavorable for intensification during the next 24 hours.  Even though Vayu will move over water where the Sea Surface Temperature is near 30°C, the combined effects of the drier air and the wind shear are likely to cause the tropical cyclone to continue to weaken on Sunday.  If the upper level winds get stronger, they could blow the upper half of the circulation southwest of the lower part of Tropical Cyclone Vayu.  In that case Vayu will weaken more quickly.

The future track of Tropical Cyclone Vayu will also depend on the vertical wind shear.  If the wind shear is not too strong and the circulation remains vertically intact, then the ridge north of Vayu will steer the tropical cyclone slowly toward the northwest on Sunday.  If the upper level winds blow the upper half of the circulation away from the lower portion of Tropical Cyclone Vayu, then southwesterly winds in the lower atmosphere will blow the shallower system toward the northeast.  Guidance from numerical models suggest this second scenario is more likely and the anticipated track takes Tropical Cyclone Vayu toward the northeast.

Tropical Cyclone Vayu Stalls, Weakens Southwest of Gujarat

Tropical Storm Vayu stalled and weakened southwest of Gujarat on Friday.  At 11:00 p.m. EDT on Friday the center of Tropical Cyclone Vayu was located at latitude 20.6°N and longitude 67.4°E which put it about 170 miles (275 km) southwest of Dwarka, India.  Vayu was moving toward the west at 4 m.p.h. (6 km/h).  The maximum sustained wind speed was 90 m.p.h. (150 km/h) and there were wind gusts to 115 m.p.h. (185 km/h).  The minimum surface pressure was 969 mb.

The structure of the inner core of Tropical Cyclone Vayu changed significantly on Friday.  The previous small eye disappeared and a large new eye with a diameter of 50 miles (80 km) developed at the center of Vayu.  The eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that ring of storms.  The strongest rainbands were located in the southern half of the circulation.  Bands in the northern half of the circulation consisted primarily of showers and lower clouds.  Winds to hurricane/typhoon force extended out about 35 miles (55 km) from the center of circulation.  Winds to tropical storm extended out about 150 miles (240 km) from the center.

The environment around Tropical Cyclone Vayu will become less favorable for a tropical cyclone on Saturday.  An upper level ridge north of Vayu will strengthen.  The ridge will produce stronger northeasterly winds which will blow toward the top of the circulation.  Those winds will cause more vertical wind shear.  Tropical Cyclone Vayu will also continue to pull drier air into the northern half of the circulation.  Vayu will move over water where the Sea Surface Temperature is near 30°C.  Even though Tropical Cyclone Vayu will be over very warm water, the combined effects of stronger wind shear and drier air are likely to cause it to weaken on Saturday.

The ridge north of Vayu will block the tropical cyclone from moving toward the north on Saturday.  The ridge is likely to continue to steer Tropical Cyclone Vayu slowly toward the west over the northeastern Arabian Sea during the next 24 hours.  On its anticipated track Vayu will move farther away from Gujarat and Pakistan on Saturday.

Tropical Cyclone Vayu Turns West Over Northeast Arabian Sea

Tropical Cyclone Vayu turned west over the northeastern Arabian Sea on Thursday.  At 11:00 p.m. EDT on Thursday the center of Tropical Cyclone Vayu was located at latitude 20.9°N and longitude 68.4°E which put it about 80 miles (130 km) southwest of Porbandar, India.  Vayu was moving toward the west-northwest at 4 m.p.h. (6 km/h).  The maximum sustained wind speed was 105 m.p.h. (170 km/h) and there were wind gusts to 120 m.p.h. (195 km/h).  The minimum surface pressure was 960 mb.

Tropical Cyclone Vayu maintained its intensity on Thursday, but the circulation exhibited slightly less organization.  A small eye continued to mark the center of circulation.  A ring of strong thunderstorms surrounded the eye, but there was a break in the northeastern portion of the ring.  The circulation continued to pull drier air into the northern part of the tropical cyclone.  Many of the stronger thunderstorms were occurring in bands in the southern half of the circulation.  Rainbands in the northern half of the circulation were weaker.  Winds to hurricane/typhoon force extended out about 40 miles (65 km) from the center of circulation.  Winds to tropical storm force extended out about 125 miles (200 km) from the center.

Tropical Cyclone Vayu will continue to move through an environment capable of sustaining a tropical cyclone on Friday.  Vayu will move under the axis of an upper level ridge where the winds are weaker and there will be little vertical wind shear.  The Sea Surface Temperature in the northeastern Arabian Sea is near 30°C.  However, Tropical Cyclone Vayu moved slowly on Thursday and it may have stirred some cooler water to the surface.  In addition, the circulation around Vayu will continue to draw in drier air from over south Asia.  Tropical Cyclone Vayu could start to weaken slowly on Friday, although it could maintain its intensity if it moves away from the upwelled cooler water.

Tropical Cyclone Vayu will be south of a strengthening ridge of high pressure over south Asia.  The ridge will block Vayu and prevent it from moving farther toward the north.  The ridge will steer Vayu slowly toward the west during the next 24 to 48 hours.  On its anticipated track Tropical Cyclone Vayu will remain southwest of Gujarat and south of Pakistan during the next two days.

Tropical Cyclone Vayu Slows Near Gujarat Coast

Tropical Cyclone Vayu slowed near the coast of Gujarat on Wednesday.  At 11:00 p.m. EDT on Wednesday the center of Tropical Cyclone Vayu was located at latitude 20.4°N and longitude 69.1°E which put it about 85 miles (135 km) south-southwest of Porbandar, India.  Vayu was moving toward the north-northwest at 8 m.p.h. (13 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 962 mb.

The circulation around Tropical Cyclone Vayu weakened slightly on Wednesday, although the inner core appeared to remain mostly intact.  The circulation seemed to pull some drier air over India into the eastern and northern portions of Vayu.  Outer rainbands weakened in those parts of the tropical cyclone.  The drier air did not appear to have penetrated the inner core of the circulation.  A tiny eye remained at the center of circulation.  A ring of showers and thunderstorms surrounded the eye and the strongest winds were occurring in that ring of storms.  Bands of strong thunderstorms in the southern half of the circulation were revolving around the core of Tropical Cyclone Vayu.  Winds to hurricane/typhoon force extended out about 35 miles (55 km) from the center of circulation.  Winds to tropical storm force extended out about 120 miles (195 km) from the center.

Tropical Cyclone Vayu will move through an environment that will be mainly favorable for a tropical cyclone during the next 24 to 48 hours.  Vayu will move over water where the Sea Surface Temperature is near 30°C.  It will move near the axis of an upper level ridge where winds are weaker and there will be less vertical wind shear.  The drier air being pulled into the circulation from over India will be a factor that could inhibit any additional strengthening of Tropical Cyclone Vayu.  Vayu could strengthen during the next 24 hours, but it is more likely to maintain its intensity or weaken slightly.  If drier air mixes into the inner core of the circulation, then Tropical Cyclone Vayu could weaken more quickly.

Tropical Cyclone Vayu will move around the western end of a ridge over India during the next 12 to 24 hours.  The ridge will steer Vayu toward the north-northwest on Thursday.  A second ridge will develop north of Tropical Cyclone Vayu.  The second ridge will block the northward movement of Vayu and force the tropical cyclone to move more toward the west.  On its anticipated track the core of Tropical Cyclone Vayu will remain west of the coast of Gujarat.  Bands on the eastern side of the circulation could drop rain over Gujarat but the strongest part of the circulation is likely to remain offshore.

Tropical Cyclone Vayu Strengthens to Equivalent of Hurricane/Typhoon

Tropical Cyclone Vayu strengthened into the equivalent of a hurricane/typhoon over the eastern Arabian Sea on Tuesday.  At 11:00 a.m. EDT on Tuesday the center of Tropical Cyclone Vayu was located at latitude 16.4°N and longitude 70.8°E which put it about 200 miles (320 km) southwest of Mumbai, India.  Vayu was moving toward the north at 10 m.p.h. (16 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. (150 km/h).  The minimum surface pressure was 974 mb.

Microwave satellite imagery indicated that an inner rainband had wrapped completely around the center of circulation and a small eye had formed at the center of Tropical Cyclone Vayu.  The core of Vayu was relatively small.  Winds to hurricane/typhoon force only extended out about 20 miles (30 km) from the center of circulation.  Winds to tropical storm force extended out about 100 miles (160 km) from the center.  Storms around the core of Tropical Cyclone Vayu were generating upper level divergence which was pumping mass to the west of the tropical cyclone.  Additional bands of showers and thunderstorms were revolving around the core of Vayu.

Tropical Cyclone Vayu will move through an environment favorable for intensification during the next 24 to 36 hours.  Vayu will move over water where the Sea Surface Temperature is near 30°C.  Tropical Cyclone Vayu will move near the southwestern portion of an upper level ridge.  The ridge will produce southeasterly winds which will blow toward the top of the circulation.  Those winds will cause some vertical wind shear, but the shear will not be strong enough to prevent intensification.  Tropical Cyclone Vayu will intensify during the next 24 to 36 hours.  It could intensify rapidly once the eye and eyewall are fully formed.  Vayu could strengthen into the equivalent of a major hurricane.

Tropical Cyclone Vayu will move around the western end of a ridge over India.  The ridge will steer Vayu toward the north.  On its anticipated track Tropical Cyclone Vayu could approach the coast of Gujarat within 36 hours.  Vayu could be the equivalent of a major hurricane by that time.  It could bring strong winds and locally heavy rain to Gujarat.  Heavy rain could cause flash floods.  Tropical Cyclone Vayu could also generate a significant storm surge along the coast of Gujarat.

Tropical Cyclone Forms Over Eastern Arabian Sea

A tropical cyclone formed over the eastern Arabian Sea on Monday.  At 11:00 a.m. EDT on Monday the center of Tropical Cyclone 02A was located at latitude 13.7°N and longitude 70.8°E which put it about 400 miles (645 km) south-southwest of Mumbai, India.  It was moving toward the north-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 996 mb.

More thunderstorms formed near the center of a low pressure system over the eastern Arabian Sea on Monday and the system exhibited sufficient organization to be designated a tropical cyclone.  The distribution of thunderstorms around the tropical cyclone was asymmetrical.  Most of the stronger thunderstorms were located in bands developing in the western half of the circulation.  The inner portions of a rainband was wrapping around the southern side of the center of circulation.  Bands in the eastern half of the circulation consisted primarily of lower clouds and showers.  Winds to tropical storm force extended out about 60 miles (95 km) from the center of circulation.

Tropical Cyclone 02A developed southwest of an upper level ridge.  The ridge was producing easterly winds which were blowing toward the top of the circulation.  Those winds were causing moderate vertical wind shear and they were the primary cause for the asymmetrical distribution of thunderstorms.  The tropical cyclone will move over water where the Sea Surface Temperature is near 30°C.   Wind shear will inhibit intensification, but it will not be strong enough to prevent Tropical Cyclone 02A from strengthening.  The tropical cyclone will gradually intensify and it could strengthen to the equivalent of a hurricane/typhoon.  If an eye and eyewall form as part of an inner core and the wind shear decreases, then a period of rapid intensification could occur.

Tropical Cyclone 02A will move around the western end of the upper level ridge.  The ridge will steer the tropical cyclone toward the north-northwest during the next several days.  On its anticipated track Tropical Cyclone 02A could approach the coast of Gujarat within 72 hours.  it could be the equivalent of a hurricane/typhoon by that time.

Tropical Cyclone Ockhi Moves Closer to India

Tropical Cyclone Ockhi moved closer to India on Monday.  At 10:00 p.m. EST on Monday the center to Tropical Cyclone Ockhi was located at latitude 17.9°N and longitude 70.7°E which put it about 170 miles (270 km) west-southwest of Mumbai, India and about 250 miles (400 km) southwest of Surat.  Ockhi was moving toward the northeast at 11 m.p.h. (17 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 983 mb.

An upper level trough over the northern Arabian Sea was producing strong southwesterly winds which were blowing across the top of Tropical Cyclone Ockhi.  Those winds were causing significant vertical wind shear.  Microwave satellite imagery was indicating that the shear may be strong enough to push the upper part of Ockhi’s circulation to the northeast of the lower part of the tropical cyclone’s circulation.  The circulation in the middle and upper levels continued to show evidence of an eye surrounded by a ring of strong storms.  Several bands of strong storms were occurring north of the center of circulation.

The upper level trough is steering Tropical Cyclone Ockhi toward the northeast and that general motion is expected to continue for several more days.  On its anticipated track Ockhi will make landfall in Gujarat along the coast of the Gulf of Khambhat within 24 hours.  Strong vertical wind shear will continue to weaken Tropical Cyclone Ockhi.  Ockhi is likely to make landfall as the equivalent of a tropical storm.  Drier air is wrapping around the southern side of the circulation.  The heavy rain will fall over parts of Gujarat before the center of circulation reaches the coast.  Locally heavy rainfall could create the potential for flash floods in some places.

Tropical Cyclone Ockhi Turns Back Toward India

Tropical Cyclone Ockhi turned back toward India on Sunday night as it moved over the eastern Arabian Sea.  At 10:00 p.m. EST on Sunday the center of Tropical Cyclone Ockhi was located at latitude 14.6°N and longitude 68.9°E which put it about 405 miles (650 km) southwest of Mumbai, India.  Ockhi was moving toward the north-northeast at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 80 m.p.h. (130 km/h) and there were wind gusts to 100 m.p.h. (160 km/h).  The minimum surface pressure was 976 mb.

Tropical Cyclone Ockhi started to weaken on Sunday.  An upper level trough over the northern Arabian Sea was producing southwesterly winds which were causing moderate vertical wind shear.  In spite of the weakening trend, the structure of Tropical Cyclone Ockhi remained well organized.  There was a circular eye at the center of Ockhi.  A ring of strong storms surrounded the eye, but the ring was broken east of the center of circulation.  Several bands of showers and thunderstorms were occurring north of the core of Tropical Cyclone Ockhi.  The bands in the other parts of the circulation consisted primarily of low clouds and showers.  It appeared that some drier air might be wrapping around the southern and western parts of the circulation.  Winds to hurricane/typhoon force extended out about 50 miles (80 km) from the center or circulation.  Winds to tropical storm force extended out about 180 miles (290 km) from the center.

Tropical Cyclone Ockhi is likely to continue to weaken.  The upper level trough will continue to produce significant vertical wind shear over Ockhi.  The wind shear and drier air will weaken Ockhi to the equivalent of a tropical storm on Monday.  Some models dissipate the circulation of Ockhi before it makes a landfall in India, while other models move a weakened Tropical Cyclone inland before it dissipates.

The trough over the northern Arabian Sea will steer tropical cyclone Ockhi toward the northeast during the next several days.  On its anticipated track the center of Tropical Cyclone Ockhi could make a landfall on the coast of India between Mumbai and Veraval in 36 to 48 hours.  Ockhi could bring gusty winds and heavy rain to the Gulf of Khambhat and surrounding land areas in Gujarat.