Tag Archives: IO05

Tropical Cyclone Vardah Reaches Hurricane Intensity

Tropical Cyclone Vardah intensified into the equivalent of a hurricane on Saturday as it moved across the Bay of Bengal toward India.  At 4:00 p.m. EST on Saturday the center of Tropical Cyclone Vardah was located at latitude 13.0°N and longitude 84.8°E which put it about 290 miles (470 km) east of Chennai, India.  Vardah was moving toward the west at 13 m.p.h. (21 km/h).  The maximum sustained wind speed was 75 m.p.h. (120 km/h) and there were gusts to 90 m.p.h. (145 km/h).  The minimum surface pressure was 974 mb.

The circulation of Tropical Cyclone Vardah is well organized, but the distribution of thunderstorms is asymmetrical.  There is a broken ring of thunderstorms around the center of circulation.  Outside of that ring most of the thunderstorms are forming in the western half of the circulation.  It appears that an upper level ridge to the north of Vardah is producing easterly winds which are causing moderate vertical wind shear.  The wind shear seems to be the primary cause of the asymmetry of the convection.  The thunderstorms are generating upper level divergence which is pumping out mass to the west of the cyclone.

The environment around Tropical Cyclone Vardah is marginal for further intensification.  Vardah is moving over water where the Sea Surface Temperature is near 29°C.  However, the moderate vertical wind shear may be strong enough to inhibit further intensification.  There are some indications that the upper level winds may be getting stronger and the shear could increase.  If the shear increases, then Tropical Cyclone Vardah could start to weaken even though it is over warm water.

The same ridge that is causing the wind shear is also steering Tropical Cyclone Vardah toward the west and that general motion is expected to continue.  On its anticipated track Tropical Cyclone Vardah could make landfall near Chennai, India in about 36 hours.  Tropical Cyclone Vardah will bring gusty winds and locally heavy rain to portions of southern India.  The heavy rain could cause flooding and mudslides.  Vardah will also cause a storm surge along the coast near and to the north of where the center makes landfall.

Tropical Cyclone Vardah Turns Toward India and Strengthens

Tropical Cyclone Vardah turned toward India and strengthened on Friday.  At 4:00 p.m. EDT on Friday the center of Tropical Cyclone Vardah was located at latitude 12.5°N and longitude 88.7°E which put it about 500 miles (800 km) southeast of Visakhapatnam, India.  Vardah was moving toward the west-northwest at 13 m.p.h. (21 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.

Many more thunderstorms formed around the core of Tropical Cyclone Vardah and it exhibited a more symmetrical, circular shape on Friday.  The increasing organization of the circulation include multiple spiral rainbands in the outer portions of the cyclone.  The thunderstorms near the core of Vardah generated strong upper level divergence which pumped out mass and allowed the pressure to decrease more quickly.  An increased pressure gradient force generated stronger winds.

The environment around Tropical Cyclone Vardah has become much more favorable for intensification.  An upper level ridge to the east of Vardah was causing southeasterly winds and was producing moderate vertical wind shear.  Those winds have diminished and the wind shear is much less.  Since Vardah is moving over water where the Sea Surface Temperature is near 29°C, it is efficiently extracting energy from the ocean.  Tropical Cyclone Vardah will continue to intensify during the next 24 hours and it could intensify rapidly.  Vardah is likely to become the equivalent of a hurricane on Saturday.

A subtropical ridge north of Vardah is strengthening and building toward the west.  The ridge is steering Tropical Cyclone Vardah toward the west-northwest and that general motion is expected to continue.  On its anticipated track Tropical Cyclone Vardah could approach the coast of southeast India in two or three days.

Tropical Cyclone Vardah could bring strong winds and heavy rain to parts of southeastern India in three or four days.

Tropical Cyclone Forms Near Andaman Islands

A tropical cyclone formed near the Andaman Islands over the Bay of Bengal on Wednesday.  At 10:00 p.m. EST on Wednesday the center of Tropical Cyclone 05B was located at latitude 11.6°N and longitude 92.1°E which put it about 710 miles (1145 km) southeast of Visakhapatnam, India.  The tropical cyclone was moving toward the north-northeast at 5 m.p.h. (8 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.

An area of thunderstorms moved from the western Pacific Ocean into the southeastern Bay of Bengal.  The area of thunderstorms turned slowly northward near the Nicobar and Andaman Islands.  A distinct center of circulation began to organize inside the area of thunderstorms.  The Indian Meteorological Department classified the low pressure area as a depression and the Joint Typhoon Warning Center designated the system as Tropical Cyclone 05B.

The circulation of Tropical Cyclone 05B is still organizing.  A primary band of thunderstorms wraps around the northern and western side of the center of circulation.  Additional bands of thunderstorms are forming in the eastern half of the circulation.  Microwave satellite imagery suggests that an eye could be developing in the middle levels of the circulation.  The thunderstorms near the center are generating upper level divergence that is pumping out mass toward the northeast of the tropical cyclone.

Tropical Cyclone will be moving through an environment that is favorable for intensification.  It will be moving over water where the Sea Surface Temperature is near 29°C.  An upper level ridge to the west of the cyclone is producing northerly winds which are blowing across the top it.  However, the vertical wind shear is not significantly inhibiting the organization of the tropical cyclone.  Tropical Cyclone 05B could reach hurricane intensity in a couple of days.

A subtropical ridge is currently steering Tropical Cyclone 05B toward the north.  The center is moving just to the west of the Andaman Islands.  The subtropical ridge is forecast to strengthen and build toward the west.  As the ridge strengthens and extends farther west, it will start to steer the tropical cyclone toward the west.  On its anticipated track Tropical Cyclone 05B could approach the east coast of India in three or four days.

Tropical Cyclone 05B will continue to bring gusty winds and heavy rain to parts of the Andaman Islands on Thursday.  The tropical cyclone could bring strong winds, locally heavy rain, a storm surge and mudslides to southern India in a few days.

Weaker Tropical Cyclone Megh Close to Landfall in Yemen

Drier air from the Arabian peninsula finally entered the circulation of Tropical Cyclone Megh and most of the convection weakened on Monday.  At 10:00 p.m. EDT on Monday the center of Tropical Cyclone Megh was located at latitude 13.0°N and longitude 47.0°E which put it about 150 miles (240 km) east of Aden (Adan), Yemen.  Megh was moving toward the west-northwest at 15 m.p.h. (24 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.

As Tropical Cyclone Megh moved closer to the coast of Yemen, it began to draw in drier air from the Arabian peninsula.  As the drier air penetrated the circulation, it cut off the energy from the convection and most of the thunderstorms dissipated.  Without a continuous supply of new energy Megh weakened and the wind speeds decreased.  As the center of circulation approached the coast, friction over land increased low level convergence and new thunderstorms formed near the center.  Those storms are producing winds to tropical storm force over the Gulf of Aden.

Tropical Cyclone Megh is moving around the western end of a subtropical ridge.  The ridge is steering Megh toward the west-northwest.   Tropical Cyclone Megh will make landfall near Ahwar, Yemen in a few hours.  It is still capable of producing locally heavy rain and causing flash flooding.

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.