Tag Archives: Bermuda

Tropical Storm Gaston Forms Southwest of the Cape Verde Islands

A center of circulation quickly organized within a tropical wave on Monday night and the National Hurricane Center designated the system as Tropical Storm Gaston.  At 11:00 p.m. EDT on Monday the center of Tropical Storm Gaston was located at latitude 12.6°N and longitude 30.7°W which put it about 450 miles (725 km) west-southwest of the Cape Verde Islands.  Gaston was moving toward the west-northwest at 18 m.p.h. (30 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 1005 mb.

The circulation consolidated rapidly around the center of Tropical Storm Gaston on Monday.  Several spiral bands of thunderstorms formed close to the center and additional bands formed farther from the center.  The thunderstorms near the center began to generate upper level divergence, which pumped mass away from the center.

Tropical Storm Gaston is moving through an environment that is favorable for intensification.  It is over water where the Sea Surface Temperature is near 28°C.  The upper level winds are light and there is little vertical wind shear.  Gaston is likely continue to intensify steadily during the next several days and it is expected to become a hurricane.  Once a tightly organized core consolidates completely, Gaston could undergo a period of more rapid intensification.

A subtropical ridge is steering Tropical Storm Gaston toward the west-northwest and that general motion is expected to continue for a day or so.  The ridge is expected to weaken northwest of Gaston, and the tropical storm is expected to turn more toward the north during the middle of the week.  Gaston could be moving out into the Central Atlantic Ocean by the end of the week.

Tropical Depression Six Intensifies Into Tropical Storm Fiona

Tropical Depression Six intensified on Wednesday and the National Hurricane Center named it Tropical Storm Fiona.  At 5:00 p.m. EDT on Wednesday the center of Tropical Storm Fiona was located at latitude 15.1°N and longitude 37.8°W which put it about 1545 miles (2490 km) east of the Leeward Islands.  Fiona was moving toward the northwest at 16 m.p.h. (26 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 1006 mb.

Tropical Storm Fiona has a small circulation and winds to tropical storm force only extend out about 25 miles (40 km) from the center circulation.  Most of the thunderstorms are occurring close to the center of circulation.  Those thunderstorms are generating some upper level divergence, but it does not extend very far from the core of Tropical Storm Fiona.  There are bands of lower clouds and showers rotating around the core of Fiona.

Tropical Storm Fiona is moving through an environment that is mostly favorable for intensification.  It is moving over water where the Sea Surface Temperature is near 27°C.  An upper level ridge north of Fiona is generating northeasterly winds which are blowing across the top of the tropical storm.  Those winds are causing some vertical wind shear, but it should only inhibit, but not stop, intensification.  There is drier air northwest of Fiona and that is the main negative factor in the environment.  If the drier air gets pulled into the core of Tropical Storm Fiona, it will reduce the supply of energy and weaken Fiona.  Since the core of Fiona is so small, the tropical storm could intensify or weaken very quickly as the environmental conditions change.

The subtropical high that extends from Africa across the Atlantic Ocean is splitting into an eastern ridge and a western ridge.  Tropical Storm Fiona is moving toward the weakness where the split is occurring.  This is producing a motion toward the northwest and that general motion is expected to continue during the next several days.  On its anticipated track Tropical Storm Fiona could be northeast of the Leeward Islands in a few days.

Tropical Depression Six Forms Over Eastern Atlantic

A center of circulation developed within a tropical wave designated as Invest 98L on Tuesday and the National Hurricane Center classified the system as Tropical Depression Six.  At 11:00 p.m. EDT on Tuesday the center of Tropical Depression Six was located at latitude 12.6°N and longitude 34.1°W which put it about 1800 miles (2900 km) east of the Leeward Islands.  The depression 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. (70 km/h).  The minimum surface pressure was 1008 mb.

The circulation of Tropical Depression Six is still organizing.  A center of circulation exists near the surface and thunderstorms are developing near the center.  Several partial spiral bands are beginning to form.  The thunderstorms near the center are generating a small region of upper level divergence, but the divergence is occurring mainly to the southwest of the depression.

Tropical Depression Six is moving through an environment that favors intensification.  It is moving over water where the Sea Surface Temperature is near 27°C.  An upper level ridge to the north is causing northeasterly winds to blow across the top of the depression.  There is some vertical wind shear, but the shear will only slow the rate of intensification.  The shear is not strong enough to prevent intensification and Tropical Depression Six is expected to become a tropical storm during the next day or two.

The subtropical ridge over Africa and the Atlantic Ocean is splitting into two parts and Tropical Depression Six is moving toward the northwest into the split that is developing.  The depression is expected to continue to move toward the northwest in the short term.  The longer term motion will depend on how strong Tropical Depression Six becomes.  If it intensifies more and develops a taller circulation, then the depression will be steered by the winds higher in the atmosphere.  The winds at those levels are more likely to carry it into the central Atlantic Ocean.  However, if vertical wind shear weakens the depression and the circulation is shallower, then the winds in the lower levels of the atmosphere could carry the depression farther to the west.  In either case Tropical Depression Six is no immediate threat to any land area.

Bonnie Regains Tropical Depression Status Near Cape Hatteras

One time Tropical Storm Bonnie regained tropical depression status near Cape Hatteras on Thursday morning.  The National Hurricane Center (NHC) will resume issuing advisories on Tropical Depression Bonnie at 11:00 a.m. EDT on Thursday.  At 5:00 a.m. EDT on Thursday the center of Tropical Depression Bonnie was located at latitude 35.0°N and longitude 75.7°W which put it about 15 miles (25 km) south of Hatteras,, North Carolina.  Bonnie was moving toward the east-northeast at 9 m.p.h. (15 km/h).  The maximum sustained wind speed was 25 m.p.h. (40 km/h) and there were wind gusts to 35 m.p.h. (55 km/h).  The minimum surface pressure was 1010 mb.

After making landfall in South Carolina during the weekend, the center of Bonnie made a counterclockwise loop over land and then drifted east of Charleston.   The center drifted back over water on Tuesday and more thunderstorms formed near the center of circulation.  However, the vertical wind shear was still significant and the tops of the thunderstorms were periodically blown away from the lower part of the circulation.  As a result the circulation of Post Tropical Depression Bonnie was relatively shallow and existed primarily in the lower troposphere below 700 mb (about 3 km above the surface).  The low level circulation of Bonnie has move slowly east-northeast since that time and more thunderstorms developed in several spiral bands around the circulation.

During the past 24 hours Bonnie drifted under the axis of an upper level trough where the upper level winds are lighter.  As a result thunderstorms have persisted and a well formed band wraps around the northern and western sides of the center of circulation.  The circulation also extends higher into the atmosphere and a small area of upper level divergence has developed over the center of circulation.  Bonnie again has the appearance of a tropical cyclone on both satellite and radar images, which is why NHC is resuming advisories on the system.

Tropical Depression Bonnie could intensify further in the short term.  The Sea Surface Temperature (SST) reported by a buoy at Diamond Shoals, which is near the center of Bonnie, is near 26°C.  So, there is enough energy in the upper ocean to support some strengthening.  The upper level winds are light and vertical wind shear is not significant at this time.  If the surface pressures start to decrease, then Bonnie has a chance to become a tropical storm again.  Eventually, Bonnie will move into an environment where the SSTs are cooler and there is more vertical wind shear.

Tropical Depression Bonnie is between a subtropical high pressure system to its southeast and mid-latitude westerly flow to its north.  That combination is steering Bonnie slowly toward the east-northeast.  A general easterly motion is expected to continue during the next few days.  On its anticipated track Bonnie will gradually move away from the east coast of the U.S.

Strong Low Spins Up Off Southeast Coast

A strong non-tropical low pressure system spun up off the Southeast Coast of the U.S. on Thursday and there is some possibility that it could eventually develop subtropical or tropical characteristics.   At 4:00 p.m. EST on Thursday the low pressure system was centered near latitude 29.0°N and longitude 74.0°W which put it about 425 miles (685 km) west-southwest of Bermuda.  The low was moving toward the east-northeast at 18 m.p.h. (29 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 994 mb.

The low pressure system exhibits the structure of an occluded extratropical cyclone.  An occluded front coils away from the low until it splits into a warm front and a cold front.  Drier air is being pulled around the western and southern sides of the low and a dry slot has formed in the southeastern quadrant of the storm.  However, upper level divergence is pumping mass away from the center of the low and the surface pressure decreased quickly on Thursday afternoon.

The low is in an environment that is not favorable for the classical scenario of formation of a tropical cyclone.  It is moving over water where the Sea Surface Temperature (SST) is near 25°C and strong upper level winds are creating significant vertical wind shear.  However, research has shown that it is possible to get a transition to a subtropical or tropical cyclone over cooler SSTs, when a low pressure system moves into an area where the wind shear is less.

A trough over the southeastern U.S. is steering the low pressure system toward the east-northeast and that general motion is expected to continue during the next day or two.  An upper level ridge is forecast to move north of the low pressure system in a couple of days.  The upper level ridge is expected to steer the low pressure system toward the east-southeast early next week.

If the low pressure system takes the expected track, it could eventually move over slightly warmer SSTs and into an area where there is less vertical wind shear.  The more favorable environment could cause the structure of the low to change into a more subtropical or tropical form.  The National Hurricane Center is giving the low a 10% chance of transitioning into a subtropical cyclone during the next 48 hours and a 30% chance that it makes that transition during the next five days.

Kate Becomes a Hurricane As It Races Northeast

Kate intensified into the fourth Atlantic hurricane of 2015 as it raced northeastward.  At 10:00 a.m. EST on Wednesday the center of Hurricane Kate was located at latitude 36.8°N and longitude 60.5°W which put it about 395 miles (635 km) northeast of Bermuda and about 780 miles (1160 km) south-southwest of Cape Race, Newfoundland.  Kate was moving toward the northeast at 45 m.p.h. (72 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 985 mb.

The organization of Hurricane Kate improved on Wednesday when a partial eyewall wrapped around the northern and western sides of the center of circulation.  The structure of Kate is somewhat tilted toward the northeast by stronger southwesterly wind in the upper levels of the atmosphere.  However, Kate currently has a warm core and it is still a tropical cyclone.  Kate is moving over water where the Sea Surface Temperature (SST) is near 25°C.  In a day or so the effects of strong vertical wind shear and cooler SSTs will cause Hurricane Kate to begin a transition to an extratropical cyclone.

Strong westerly winds are steering Kate rapidly toward the northeast and that general motion is expected to continue during the next few days.  Kate could approach the United Kingdom as a strong extratropical cyclone during the weekend.

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 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.

Hurricane Joaquin Passing Northwest of Bermuda

Hurricane Joaquin is bringing tropical storm force winds to Bermuda as the core of the hurricane moves northwest of that island.  Wind gusts to 64 m.p.h. have been reported in recent hours in Bermuda.  At 11:00 p.m. EDT on Sunday the center of Hurricane Joaquin was located at latitude 33.1°N and longitude 65.5°W which put it about 70 miles (110 km) northwest of Bermuda.  Joaquin was moving toward the north-northeast at 13 m.p.h. (20 km/h).  The maximum sustained wind speed was 85 m.p.h. (140 km/h) and there were wind gusts to 100 m.p.h. (160 km/h).  The minimum surface pressure was 961 mb.  A Hurricane Warning remains in effect for Bermuda.

Hurricane Joaquin is gradually moving over cooler water, but it is still over water where the Sea Surface Temperature is around 28°C.  It appears that a combination of drier air and vertical wind shear caused Joaquin to weaken on Sunday.  Thunderstorms are not rising as far up into the atmosphere and gaps have appeared in the eyewall.  Southwesterly winds in the upper levels are inhibiting upper level divergence in that portion of the hurricane and the pressure rose 17 mb on Sunday.  The wind shear could lessen for a time on Monday and the rate of weakening could slow.

Hurricane Joaquin is moving toward the north-northeast.  When it moves farther north, it will encounter the upper level westerlies in the middle latitudes.  Those westerly winds will carry Joaquin toward the east.  Joaquin could make a transition to a strong extratropical storm and affect western Europe in a few days.

Hurricane Joaquin Heading Toward Bermuda

After intensifying to almost Category 5 on the Saffir-Simpson Scale on Saturday, Hurricane Joaquin headed toward Bermuda.  The Bermuda Weather Service has issued a Hurricane Warning for Bermuda.  At 11:00 p.m. EDT on Saturday the center of Hurricane Joaquin was located at latitude 28.0°N and longitude 68.9°W which put it about 385 miles (620 km) southwest of Bermuda.  Joaquin was moving toward the northeast at 20 m.p.h. (32 km/h).  The maximum sustained wind speed was 130 m.p.h. (215 km/h) and there were wind gusts to 160 m.p.h. (260 km/h).  The minimum surface pressure was 944 mb.  Joaquin was a Category 4 hurricane on the Saffir-Simpson Scale.  The Hurricane Intensity Index (HII) was 25.1.  The Hurricane Size Index (HSI) was 20.0 and the Hurricane Wind Intensity Size Index (HWISI) was 45.1.

Joaquin is moving over water where the Sea Surface Temperature is near 29°C.  However, a large upper level trough over the southeastern U.S. and an upper level low northwest of Joaquin are combining to generate westerly winds over the hurricane.  The vertical wind shear is causing the circulation to become more asymmetrical and the strongest convection is occurring in the eastern half of the circulation.  The flow of air is also pushing drier air toward the core of Hurricane Joaquin.  If Joaquin can move fast enough to outrun the drier air, it could weaken slowly.  However, if the drier air gets into the core of the circulation, then Joaquin will weaken faster.

The trough and upper level low are steering Hurricane Joaquin quickly toward the northeast and that motion is expected to continue on Sunday.  On its anticipated track Joaquin will pass near Bermuda on Sunday night.  It could bring strong winds and a storm surge as it moves past the island.