Tropical Storm Kate Intensifies and Moves Away from the Bahamas

Tropical Depression 12 intensified Monday into Tropical Storm Kate.  Kate continued to intensify on Monday night as it started to move away from the Bahamas.  At 10:00 p.m. EST on Monday the center of Tropical Storm Kate was located at latitude 27.2°N and longitude 76.0°W which put it about 175 miles (280 km) north-northeast of the Northwestern Bahamas.  Kate was moving toward the north at 16 m.p.h. (26 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 1005 mb.

Kate is more organized this evening and it looks more like a tropical storm.  The is a core of thunderstorms at the center of circulation and several rainbands are wrapping around the northeastern side of the storm.  Kate has a small circulation and tropical storm force winds only extend out about 80 miles (130 km) on the eastern side of it.  The thunderstorms in the core of Kate are generating upper level divergence which is spreading northeast of the center.

Tropical Storm Kate is in an environment that is favorable for further intensification.  It is over water where the Sea Surface Temperature is near 28°C.  The combination of a large trough west of Kate and a smaller upper level high east of it are creating some southerly winds over the top of the circulation.  However, the vertical wind shear is moderate at the current time, and Kate could intensify further.  Kate could reach hurricane intensity in the next 24 to 36 hours.  After that time the trough to the west of Kate will cause increased vertical wind shear.

The upper level trough and ridge are steering Kate toward the north.  As Kate moves farther north, stronger westerly winds will begin to push it toward the northeast.  Since Kate is moving toward the northeast away from the Bahamas, the government there has discontinued all tropical storm warnings.

Tropical Cyclone Megh Hits Socotra Island and Brushes Somalia

Tropical Cyclone Megh moved over Socotra Island, Yemen on Sunday and it passed near the northeast coast of Somalia.  At 10:00 p.m. EDT on Sunday the center of Tropical Cyclone Megh was located at latitude 12.3°N and longitude 50.6°E which put it about 375 miles (605 km) east of Aden (Adan), Yemen and about 35 miles (55 km) north of Cape Guardafui, Somalia.  Megh was moving toward the west at 13 m.p.h. (21 km/h).  The maximum sustained wind speed was 105 m.p.h. (170 km/h) and there were wind gusts to 125 m.p.h. (200 km/h).  The minimum surface pressure was 957 mb.

Although Tropical Cyclone Megh weakened as it moved across Socotra Island, it remains a small, well organized storm.  Megh still has an eye surrounded by a ring of strong thunderstorms.  Those storm are generating upper level divergence which is pumping out mass in all direction.

Tropical Cyclone Megh is over warm water and the upper level winds are light.  The only negative factors are the proximity to Somalia and drier air over the Arabian peninsula.  As long as the center of Tropical Cyclone Megh stays north of Somalia, it will likely retain most of its intensity.  When Megh starts to get closer to the coast of Yemen, it will begin to draw in some drier air and weaken more rapidly.  Vertical wind shear could also increase in 24 to 36 hours, which would further speed the weakening process.

A subtropical ridge has been steering Megh toward the west and that general motion is expected to continue for another day or so.  After that time Megh will reach the western end of the ridge and start to move toward the northwest.  On its expected track, Tropical Cyclone Megh could approach the coast of Yemen on Tuesday.  It could still be the equivalent of a hurricane at that time.

Tropical Cyclone Megh may have caused significant damage on Socotra Island.  It will be capable of producing wind damage when it reaches Yemen, but heavy rain and flooding will be the greater risk.

Tropical Depression 12 Forms and Warnings Issued for the Bahamas

A small center of circulation developed within a larger disturbance near the Bahamas and the National Hurricane Center classified it as Tropical Depression 12 (TD12).  At 10:00 p.m. EDT on Sunday the center of Tropical Depression 12 was located at latitude 23.0°N and longitude 73.0°W which put it about 115 miles (185 km) southeast of San Salvador in the Bahamas and about 30 miles (50 km) north of Mayaguana.  TD12 was moving toward the northwest at 14 m.p.h. (22 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 1010 mb.

Tropical Storm Warnings have been issued for the Central and Northwestern Bahamas and for the Acklins, Samana Cays, Crooked Island and Long Cay in the Southeastern Bahamas.

Tropical Depression 12 formed when a tropical wave interacted an upper level low.  Tropical cyclones that develop in that manner tend to be poorly organized in their early stages.  Most of the stronger thunderstorms are located east and south of the center of circulation.  The surface center is located on the western edge of the convection.

Although Tropical Depression 12 is over water where the Sea Surface Temperature is near 28°C, the upper level environment is marginal for intensification.  An upper level low near southwest of the depression is generating southerly upper level winds over the western part of TD12.  A small upper level high is over the eastern part of TD12.  The upper level high is generating some divergence to the east of the depression.  Some further intensification is possible and the depression could become Tropical Storm Kate on Monday.

Tropical Depression 12 could bring rain and squally weather to parts of the Bahamas.  It is near some of the same places that were hit by Hurricane Joaquin last month and it could hinder recovery efforts.

Dangerous Tropical Cyclone Megh Nearing Socotra Island

Megh intensified rapidly Saturday into a dangerous tropical cyclone as it neared Socotra Island, Yemen.  At 10:00 p.m. EDT on Saturday the center of Tropical Cyclone Megh was located at latitude 12.8°N and longitude 55.5°E which put it about 105 miles (170 km) east of Socotra Island, Yemen.  Megh was moving toward the west at 13 m.p.h. (21 km/h).  The maximum sustained wind speed was 130 m.p.h. (210 km/h) and there were wind gusts to 150 m.p.h. (240 km/h).  The minimum surface pressure was 939 mb.

Tropical Cyclone Megh is the equivalent of a major hurricane even though it is a small storm.  Megh is a very symmetrical cyclone.  It has a five mile (8 km) wide eye which is surrounded by a ring of strong thunderstorms.  The convection in the core is generating upper level divergence which in pumping out mass.  Tropical storm force winds extend out 50 miles (80 km) from the center.

Tropical Cyclone Megh will remain in a favorable environment until it reaches Socotra Island.  It is over water where the Sea Surface Temperature is near 28°C.  The upper level winds are light and there is vertical wind shear.  Megh could intensify further until it reaches Socotra.  It should weaken when the core of the circulation interacts with island.

A subtropical ridge north of Megh is steering the tropical cyclone toward the west and that general motion is expected to continue for several more days.  On its anticipated track Tropical Cyclone Megh will reach Socotra Island in a few hours.  it is capable of producing wind damage and flooding.  Since Tropical Cyclone Chapala recently caused damage on Socotra, the impact of Tropical Cyclone Megh could be significant.

Tropical Cyclone Megh Moving Slowly West Over the Arabian Sea

Tropical Cyclone Megh moved slowly westward over the Arabian Sea on Friday.  At 4:00 p.m. EDT on Friday the center of Tropical Cyclone Megh was located at latitude 12.9°N and longitude 60.4°E which put it about 420 miles (680 km) east of Socotra Island, Yemen.  Megh was moving toward the west at 7 m.p.h. (11 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 990 mb.

The convection around Tropical Cyclone Megh diminished earlier today, but more thunderstorms have formed near the center of circulation during the past few hours.  Megh has a well formed, symmetrical circulation with an eyelike feature at the center.  It is a small cyclone and tropical storm force winds only extend out about 50 miles (80 km) from the center.  The new thunderstorms near the center of circulation are starting to generate upper level divergence.

Aside from the possible drier air, the environment surrounding Tropical Cyclone Megh is favorable for intensification,  It is over water where the Sea Surface Temperature is near 28°C.  The winds in the upper levels are light and there is not much vertical wind shear.  Now that thunderstorms are redeveloping near the core of the circulation, Tropical  Cyclone Megh should begin to intensify and it is still likely to reach hurricane intensity in a day or two.

A ridge north of Megh is steering the tropical cyclone toward the west and that general motion is expected to continue during the weekend.  On its anticipated track, Tropical Cyclone Megh could approach Socotra Island, Yemen in about 36 hours.  It could be the equivalent of a hurricane at that time.  Given the prior damage caused by Tropical Cyclone Chapala, Megh could have a significant impact on Socotra Island.

Disturbance Brings Squally Weather to the Northwest Caribbean Sea

A complicated disturbance over the northwestern Caribbean Sea is bringing squally weather to that area.  A tropical wave over the western Caribbean Sea is interacting with an upper level low over eastern Mexico.  The disturbance is causing thunderstorms over a region that extends from the northwestern Caribbean Sea to the southern Gulf of Mexico.  Upper level divergence east of the upper low has led to the formation of a surface low pressure system east of Belize.  At 7:00 p.m. EST on Thursday the center of the surface low was located at latitude 18°N and longitude 86°W which put it about 150 miles (240 km) east-southeast of Chetumal, Mexico.  The surface low was moving toward the west-northwest at 10 m.p.h. (16 m.p.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 1011 mb.

The disturbance is not very well organized, which is normally the case when a tropical wave interacts with an upper level low.  There is a broken area of thunderstorms that extends around the east and northern sides of the disturbance.  However, there are not many thunderstorms close to the center of the surface low.  The upper low is causing vertical wind shear over the western half of the surface low.  Some upper level divergence is occurring over the eastern half of the surface low.

A large high pressure system over the western Atlantic Ocean is steering the disturbance toward the west-northwest.  That general steering pattern is expected to continue for the next two days.  On its anticipated track the disturbance will move over the Yucatan peninsula and over the southern Gulf of Mexico during the next several days.

The disturbance is in an environment that is marginally favorable for tropical development.  The Sea Surface Temperature of the northwestern Caribbean is near 29°C.  There is vertical wind shear, but it may be just small enough to allow for slow development.  On the other hand, the disturbance will move over the Yucatan peninsula which will further inhibit development.  There may also be a chance for development after the disturbance moves over the southern Gulf of Mexico.  The National Hurricane Center is giving a 20% probability of tropical cyclone formation out of the disturbance.

Tropical Cyclone Megh Forms Over the Arabian Sea

A new tropical cyclone, designated with the name Megh, formed Thursday over the same portion of the Arabian Sea where Tropical Cyclone Chapala developed.  At 4:00 p.m. EST on Thursday the center of Tropical Cyclone Megh was located at latitude 13.6°N and longitude 63.0°E which put it about 640 miles (1030 km) east of Socotra Island, Yemen.  Megh was moving toward the west-southwest 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 994 mb.

Tropical Cyclone Megh exhibited increased organization on Thursday.  A core of thunderstorms developed near the center of circulation and a primary rainband spirals around the northern and western sides of the tropical cyclone.  The thunderstorms near the core of Megh are beginning to generate upper level divergence, especially toward the east.

Tropical Cyclone Megh is an environment favorable for intensification.  It is over water where the Sea Surface Temperature is near 28°C.  An upper level ridge north of Megh is generating light northeasterly winds over the top of the tropical cyclone, but the vertical wind shear is modest.  Megh should continue to intensify and it could reach the equivalent of hurricane intensity in a day or two.

The ridge is steering Tropical Cyclone Megh a little south of due west and that general steering motion is expected to continue for several days.  On its anticipated track, Tropical Cyclone Megh could approach Socotra Island, Yemen in 48 to 60 hours.  Since the outer portions of Tropical Cyclone Chapala caused damage on Socotra Island, a direct hit by Tropical Cyclone Megh could have a significant impact there.

Tropical Cyclone Chapala Makes Landfall in Yemen

Tropical Cyclone Chapala made landfall in Yemen just west of Al Mukalla as the equivalent of a hurricane.  At 10:00 p.m. EDT on Monday the center of Tropical Cyclone Chapala was located at latitude 13.9°N and longitude 48.7°E which put it 30 miles (50 km) south of Al Mukalla, Yemen.  Chapala was moving toward the west-northwest at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 85 m.p.h. (135 km/h) and there were wind gusts to 105 m.p.h. (170 km/).  The minimum surface pressure was 979 mb.

Tropical Cyclone Chapala reached the western end of the ridge that was steering it toward the west and it turned north toward the coast of Yemen on Monday.  When Chapala reached the western end of the ridge, southerly winds in the upper levels generated vertical wind shear and the circulation of the tropical cyclone tilted toward the north.  In addition, as the core of the circulation neared the coast, it drew in drier air from the Arabian peninsula.  The combination of more wind shear and drier air started to weaken Chapala, but the tropical cyclone was still the equivalent of a hurricane when it made landfall.

The core of Tropical Cyclone Chapala will bring strong winds and heavy rain to the coast.  Although Chapala will weaken fairly quickly as it moves into the dry interior of the Arabian peninsula, the circulation will be capable of producing locally heavy rainfall and flash floods as the tropical cyclone spins down.

Tropical Cyclone Chapala Poised to Enter Gulf of Aden

Tropical Cyclone Chapala continued to move steadily westward on Sunday and it was poised to enter the Gulf of Aden.  At 11:00 p.m. EDT on Sunday the center of Tropical Cyclone Chapala was located at latitude 13.2°N and longitude 52.2°E which put it about 230 miles (370 km) east-southeast of Al Mukalla, Yemen.  Chapala was moving toward the west at 12 m.p.h. (19 km/h).  The maximum sustained wind speed was 120 m.p.h. (195 km/h) and there were wind gusts to 150 m.p.h. (240 km/h).  The minimum surface pressure was 959 mb.

Chapala is still a very well organized tropical cyclone and it is the equivalent of a major hurricane.  Chapala has a 25 mile (40 km) wide eye, which is surrounded by numerous thunderstorms.  Those storms are generating upper level divergence which is pumping out enough mass to balance the air flowing into the center near the surface.  The balance of inflow and outflow allowed Chapala to maintain its intensity on Sunday.

Tropical Cyclone Chapala is over water where the Sea Surface Temperature is around 28.5°C and the upper level winds are light.  There is little vertical wind shear and most environmental factors support the ability of Tropical Cyclone Chapala to maintain its intensity.  However, once Chapala enters the Gulf of Aden it will have very dry air to its north over the Arabian peninsula and dry air to its south over east Africa.  Chapala will remain a strong tropical cyclone as long as the dry air does not reach its core.  However, as Tropical Cyclone Chapala moves closer to the coast of Yemen, the drier air will probably cause it to start to weaken.

A ridge north of Chapala is steering the tropical cyclone toward the west.  Chapala will reach the western end of the ridge on Monday and the tropical cyclone will turn toward the northwest.  On its anticipated track Chapala will make landfall on the coast of Yemen near Al Mukalla in 24 to 30 hours.  It will bring strong winds and heavy rain to the coast.  Chapala is likely to dissipate quickly as it moves inland over the Arabian peninsula, but it could bring heavy rain and flash floods before it does so.

Strong Tropical Cyclone Chapala on Track for Landfall in Yemen

Strong Tropical Cyclone Chapala moved steadily westward on Saturday and it remains on track for a landfall in Yemen.  At 11:00 p.m. EDT on Saturday the center of Tropical Cyclone Chapala was located at latitude 13.6°N and longitude 56.0°E which put it about 265 miles (425 km) south-southeast of Salalah, Oman and about 465 miles (765 km) east of Al Mukalla, Yemen.  Chapala was moving toward the west at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 135 m.p.h. (215 km) and there were wind gusts to 160 m.p.h. (260 km/h).  The minimum surface pressure was 952 mb.

Chapala continues to be a strong well organized tropical cyclone and it is the equivalent of a major hurricane.  It has a symmetrical circulation with a well formed eye inside a core of thunderstorms.  Multiple rainbands are rotation around the center of circulation.  Upper level divergence is pumping out mass in all directions.

Tropical Cyclone Chapala remains in a favorable environment.  It is over warm Sea Surface Temperatures and the upper level winds are light.  There is not much vertical wind shear and Chapala could maintain its intensity until it approaches the coast of Yemen.  When Chapala gets nearer the coast, it will start to pull in drier air from the Arabian peninsula.  As Chapala ingests the drier air, it will start to weaken.

A ridge north of Chapala is steering the tropical cyclone westward.  As Chapala nears the western end of the ridge, it will start to turn more toward the west-northwest.  On its anticipated track Tropical Cyclone Chapala will approach the central coast of Yemen in 36 to 48 hours.  The core of Chapala will pass north of the island of Socotra on Sunday.