Tag Archives: Arabian Sea

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 Moving Across Southern India

Tropical Cyclone Vardah made landfall near Chennai and moved westward across southern India on Monday.  At 8:00 p.m. EST on Monday the center of Tropical Cyclone Vardah was located at latitude 13.1°N and longitude 77.9°E which put it about 60 miles (100 km) east of Bangalore, India.  Vardah was moving toward the west at 11 m.p.h. (17 km/h).  The maximum sustained wind speed was 30 m.p.h. (50 km/h) and there were gusts to 40 m.p.h. (65 km/h).  The minimum surface pressure was 1005 mb.

Tropical Cyclone Vardah was the equivalent of a hurricane when it made landfall and it brought strong winds and heavy rain to the area around Chennai, India.  Vardah weakened steadily after making landfall and most of the thunderstorms have weakened.  The spiral bands still contains scattered showers, but the winds have diminished.  The low level circulation is still well organized and there is a distinct center of low pressure at the surface.

A subtropical ridge to the north of Vardah continues to steer the tropical cyclone toward the west.  On its anticipated track Tropical Cyclone Vardah is expected to move over the Arabian Sea near Mangalore in about 24 hours.  Some numerical models are suggesting that Tropical Cyclone Vardah could reorganize after the center moves back over the water.

Tropical Cyclone Nada Develops Near Sri Lanka

Tropical Cyclone Nada developed over the Bay of Bengal near Sri Lanka.  At 10:00 a.m. EDT on Wednesday the center of Tropical Cyclone Nada was located at latitude 10.1°N and longitude 83.5°E which put it about 295 miles (475 km) east-southeast of Chennai, India.  Nada was moving toward the west-northwest at 14 m.p.h. (23 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 997 mb.

Microwave satellite imagery indicates that Tropical Cyclone Nada has a well organized, circular low level circulation.  However, most of the thunderstorms are occurring in bands southwest of the center and north of the center.  There are mostly low clouds and showers in the circular bands south and east of the center of circulation.  An upper level ridge over the northern Bay of Bengal is producing easterly winds which are causing moderate vertical wind shear.  The upper level easterly flow is inhibiting the development of thunderstorms east of the center of Tropical Cyclone Nada and those winds may be tilting the circulation toward the west.

The environment surround Tropical Cyclone Nada consists of factors that are favorable for intensification and factors that are unfavorable.  Tropical Cyclone Nada is moving over water where the Sea Surface Temperature is near 29°C.  So, there is sufficient energy in the upper ocean to support intensification.  However the easterly winds in the upper levels are restricting upper level divergence to the east of the tropical cyclone.  Moderate vertical wind shear will limit intensification unless the upper level winds weaken.  If the upper level winds do weaken, then Nada could strengthen given its well developed low level circulation.  Tropical Cyclone Nada only has about 24 to 30 hours before it reaches the coast of India and it will start to weaken once it moves over land.

A subtropical ridge north of Nada is steering the tropical cyclone toward the west-northwest and that general motion is expected to continue.  On its anticipated track the center of Tropical Cyclone Nada will pass north of Sri Lanka and it will approach the southeast coast of India in 24 to 30 hours.  Nada is likely to make a landfall south of Cheannai, India near Pondicherry.  Tropical Cyclone Nada is expected to continue to move to the west and it could emerge over the Arabian Sea in two or three days.

Tropical Cyclone Nada will bring gusty winds and locally heavy rain to northern Sri Lanka and southern India.  Locally heavy rain could cause flooding and mudslides in parts of northern Sri Lanka and Tamil Nadu, Kerala and Karnataka states in India.

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.

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.

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.