Category Archives: Atlantic, Caribbean, and Gulf of Mexico

Atlantic TCs

Joaquin Almost a Hurricane, Watch Issued for Central Bahamas

Tropical Storm Joaquin is on the verge of reaching hurricane intensity.  At 11:00 p.m. EDT on Tuesday the center of Tropical Storm Joaquin was located at latitude 25.8°N and longitude 71.7°W which put it about 360 miles (580 km) east of the Northwestern Bahamas and about 680 miles (1100 km) south-southeast of Cape Hatteras, North Carolina.  Joaquin was moving toward the west-southwest at 5 m.p.h. (8 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 988 mb.  The government of the Bahamas has issued a Hurricane Watch for the Central Bahamas.

The organization of the circulation of Tropical Storm Joaquin increased on Tuesday in spite of moderate amounts of vertical wind shear.  More thunderstorms developed near the core of circulation and a partial eyewall formed around the southern and eastern parts of the center.  Although it is more organized, the circulation is still asymmetrical and the stronger winds were found in the eastern side of the tropical storm.

A thin upper level ridge is east of Florida and clockwise flow around the ridge is producing northerly winds over the top of Joaquin.  Those winds produced moderate vertical wind shear on Tuesday but the shear appears to be decreasing with time.  Joaquin is over water where the Sea Surface Temperature is near 30°C.  As the upper level winds diminish, the environment favors intensification and Joaquin is likely to become a hurricane on Wednesday.  Joaquin will continue to be in an environment that favors intensification during the next several days.

A ridge of high pressure north of Joaquin is blocking it from moving north and the ridge is forcing the tropical storm to move toward the west-southwest.  That general motion is expected to continue for another 24 to 48 hours and it could bring Joaquin near the Central and Northwestern Bahamas.  When Joaquin reaches the western end of the ridge it will turn toward the north.  An upper level trough over the eastern U.S. will cause Joaquin to move more quickly toward the north at the end of the week.  On its anticipated track, Joaquin could be approaching the Mid-Atlantic Coast of the U.S. by the weekend.

TD11 Becomes Tropical Storm Joaquin

The circulation in Tropical Depression 11 exhibited more organization on Monday night and the National Hurricane Center upgraded it to Tropical Storm Joaquin.  At 11:00 p.m. EDT on Monday the center of Tropical Storm Joaquin was located at latitude 26.7°N and longitude 70.4°W which put it about 400 miles (640 km) northeast of the Central Bahamas and about 670 miles (1080 km) south-southeast of Cape Hatteras, North Carolina.  Joaquin was moving toward the southwest at 5 m.p.h. (8 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 1002 mb.

Tropical Storm Joaquin formed when an upper level low sat in place over warm Sea Surface Temperatures for a few days.  Transfers of momentum slowly increased the rotation in the lower atmosphere until a distinct center of circulation developed.  However, northwesterly winds in the upper levels created vertical wind shear that inhibited the development of the system.  Eventually, the wind shear decreased enough to allow more thunderstorms to develop near the center of circulation.  Condensation in those storms created a warm core in the middle and upper atmosphere and Joaquin began to intensify.  Now, upper level divergence is beginning to develop and the environment is becoming more favorable for intensification.

A ridge north of Joaquin is steering it slowly toward the west and that steering pattern is expected to continue for the next day or two.  An upper level trough approaching from the west is expected to turn Joaquin toward the north.  Guidance from numerical models is divergent.  Some models bring Joaquin to the Mid-Atlantic Coast while other models forecast Joaquin to move toward Long Island.  The future track of Joaquin will depend on how far west it moves before it turns northward and how strong it gets.

Tropical Storm Ida Forms West of the Cape Verde Islands

The circulation within a tropical disturbance west of the Cape Verde Islands organized on Friday and it was classified as Tropical Storm Ida by the National Hurricane Center.  At 11:00 p.m. EDT on Friday the center of Tropical Storm Ida was located at latitude 13.7°N and longitude 37.5°W which put it about 915 miles (1470 km) west of the Cape Verde Islands.  Ida was moving toward the northwest at 7 m.p.h. (11 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 Ida has a much larger circulation than many of the tropical storms that have formed over the eastern Atlantic Ocean in 2015.  It has a well formed spiral rainband that curls around the southern and eastern side of the center of circulation.  The upper level winds over Ida are not very strong and upper level divergence is beginning to occur in all directions.  Ida is over water where the Sea Surface Temperature is near 28°C.  There is little vertical wind shear and the environment favors intensification.   A period of rapid intensification is possible if the inner core organizes and an eye and eyewall develop.  Ida has a chance to become a hurricane during the next several days.

A subtropical ridge north of Ida is steering the tropical storm toward the northwest and that general steering pattern is expected to continue for the next day or two.  The guidance from the numerical models is less consistent for early next week and that means there is more uncertainty about the longer term track for Ida.

 

Tropical Storm Henri Forms East of Bermuda

An instrument on a satellite indicated that there could be surface winds to tropical storm force in an area of thunderstorms east of the center of Tropical Depression Eight and the National Hurricane Center designated the system as Tropical Storm Henri.  At 11:00 p.m. EDT on Wednesday the center of Tropical Storm Henri was located latitude 31.3°N and longitude 60.7°W which put it about 250 miles (405 km) east-southeast of Bermuda.  Henri was moving toward the north at 5 m.p.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 1008 mb.

Henri is not a very well organized tropical storm.  An upper level low centered north of Bermuda is causing brisk southwesterly winds over the top of Henri.  The vertical wind shear is blowing the tops off of thunderstorms that start to form near the center of circulation.  As a result of the wind shear, the stronger thunderstorms are all located well to the east of the center of the tropical storm.  Henri is over warm Sea Surface Temperatures (SSTs) which are above normal in that part of the western Atlantic Ocean.  So, there is plenty of energy to support intensification.  However, as long as the upper level low creates significant vertical wind shear, intensification will be minimal.  It is possible that as Henri moves toward the north that the wind shear could decrease.  In that case Henri could intensify during the next day or two before it moves over cooler SSTs.

An upper level trough over the eastern U.S. should steer Henri toward the north during the next several day.  On its anticipated track, Henri could pass near Newfoundland during the weekend.  Henri could be in the process of transitioning from a tropical storm to an extratropical cyclone at that time, but it could still bring strong winds and rain to parts of extreme eastern Canada.

Tropical Storm Grace Forms Southwest of Cape Verde

Enough organization developed in the center of an area of low pressure that moved off the coast of Africa several days ago for the National Hurricane Center to classify it as Tropical Storm Grace.  At 5:00 p.m. EDT on Saturday the center of Tropical Storm Grace was located at latitude 12.6°N and longitude 26.4°W which put it about 285 miles (460 km) southwest of the Cape Verde Islands.  Grace was moving toward the west at 14 m.p.h. (22 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 1007 mb.

The area of low pressure that became Tropical Storm Grace had a large area of thunderstorms when it moved off the coast of West Africa.  A few thunderstorms developed closer to the center of circulation and there are signs that a couple of spiral bands could be forming near the core of Grace.  The strongest thunderstorms are occurring in the southwestern quadrant of the circulation.  Some of the thunderstorms appear to be getting taller, but the core of the circulation is still organizing.

Tropical Storm Grace is moving over water where the Sea Surface Temperature is near 29°C.  Although there are stronger upper level westerly winds north of the tropical storm, the vertical wind shear over Tropical Storm Grace is relatively modest.  It has a day or two for the core of the circulation to organize and to intensify.  When Grace moves farther west it could move into a region where there is drier air.  An upper level trough could produce more vertical wind shear when the tropical storm gets closer to the Caribbean Sea.

A subtropical ridge is steering Grace toward the west and that steering pattern is expected to continue for the next few days.  If Grace gets stronger and the convection taller, it would take a track a little farther to the north.  If it remains weaker and shallower, lower level winds will steer it more to the west.  On its anticipated track, Grace could approach the Lesser Antilles in five or six days.

Hurricane Fred Bringing Wind and Rain to Cape Verde Islands

Hurricane Fred brought strong winds and heavy rain to many places in the Cape Verde Islands on Monday.  At 5:00 p.m. EDT on Monday the center of Hurricane Fred was located at latitude 17.2°N and longitude 24.6°W which put it about 20 miles (30 km) east of Santo Antao in the Cape Verde Islands.  Fred was moving toward the northwest at 12 m.p.h. (19km/h).  The maximum sustained wind speed was 80 m.p.h. (130 km/h) and there were wind gusts to 95 m.p.h. (155 km/h).  The minimum surface pressure was 989 mb.  A Hurricane Warning was in effect for the Cape Verde Islands.  It is unusual for a tropical cyclone of with sustained winds to hurricane force to move through the Cape Verde Islands.

Hurricane Fred has probably already gotten as strong as it is going to get.  It is moving over water where the Sea Surface Temperature (SST) is around 27°C.  However, an upper level trough located northwest of Fred is generating southwesterly winds that are blowing across the top of the hurricane.  The resulting vertical wind shear is beginning to affect the circulation in Fred and the eyewall is not as intact as it was earlier today.  As Fred moves farther north, the SSTs will decrease and the vertical wind shear will increase.  Those negative environmental factors should caused a steady weakening of Fred.

Hurricane Fred is moving toward a weaker portion of the subtropical ridge.  The ridge is expected to strengthen this week.  In addition, as the hurricane gets weaker, its circulation will become shallower.  That will mean it will be steered by winds lower in the atmosphere.  Those winds are likely to turn Fred toward the west in a day or two.

Fred will continue to bring wind and heavy rain to the Cape Verde Islands on Monday night, but conditions should start to improve on Tuesday when the hurricane moves farther west and weakens.

Rapidly Intensifying Tropical Storm Fred Threatens Cape Verde Islands

An area of low pressure organized quickly after it moved off the coast of West Africa and the National Hurricane Center designated it as Tropical Storm Fred.  At 2:00 p.m. EDT on Sunday the center of Tropical Storm Fred was located at latitude 14.1°N and longitude 20.7°W which put it about 195 miles (315 km) east-southeast of Praia in the Cape Verde Islands.  Fred was moving toward the northwest 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 1000 mb.  A Hurricane Warning has been issued for the Cape Verde Islands.

Tropical Storm Fred was a well organized low pressure system when it moved over the eastern Atlantic Ocean from West Africa.  The input of energy from the ocean enhanced the existing thunderstorms and the low pressure system quickly reached the intensity necessary to be classified as a tropical storm.  The circulation continued to organize further on Sunday.  A primary rainband has wrapped almost entirely around the center of circulation.  A small eye and an eyewall may be forming and other spiral bands of thunderstorms are developing.  The thunderstorms are generating upper level divergence which is pumping out mass.  Fred is moving over water where the Sea Surface Temperatures (SSTs) are near 27°C to 28°C.  The winds in the upper levels are relatively light and there is not much vertical wind shear.  The favorable environmental conditions are allowing Fred to intensify rapidly and it could become a hurricane tonight.  As Fred moves farther toward the northwest, it will start to move over cooler SSTs and into a region where there is more vertical wind shear.  As a result, Fred is likely to weaken back to tropical storm intensity later this week.

There is a weaker area in the subtropical ridge over the Atlantic Ocean and Fred is moving northwest toward that area.  The ridge is expected to strengthen during the week and as it strengthens it will cause Fred to move more toward the west.  On its anticipated track Fred will reach the Cape Verde Islands in about 12 hours.  It could bring strong winds and heavy rain when it move across those islands.

Tropical Storm Erika Bringing Heavy Rain to Hispaniola

Tropical Storm Erika is moving across Hispaniola and it is bringing heavy rain to parts of that island.  At 5:00 p.m. EDT the center of Tropical Storm Erika was located at latitude 17.9°N and longitude 71.2°W which put it about 95 miles (155 km) west-southwest of Santo Domingo, Dominican Republic and about 745 miles (1200 km) southeast of Miami, Florida.  Erika was moving toward the west at 21 m.p.h. (33 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 1009 mb.  Tropical Storm Warnings have been issued for the southeastern Bahamas, the Turks and Caicos, for the Dominican Republic, Haiti, for the Central Bahamas including Cat Island, the Exumas, Long Island, Rum Cay and San Salvador.  Tropical Storm Watches have been issued for the northwestern Bahamas including the Abacos, Andros Island, Berry Island, Bimini, Eleuthera, Grand Bahama Island and New Providence, the Cuban provinces of Ciego de Avila, Camaguey, Las Tunas, Holguin and Guantanamo.

The circulation around Tropical Storm Erika is even less well organized today.  At times a small cyclonic rotation appeared on visible satellite images, while at other times Erika looked a lot like a very strong tropical wave.  Vertical wind shear caused by an upper level trough over the western Caribbean Sea has prevented thunderstorms from forming near the core of the circulation.  The lower part of the circulation will be significantly disrupted by the mountains of Hispaniola, but the middle portion may make it across the island.  If the middle level circulation is disrupted as well, then Erika will degenerate into a disorganized area of thunderstorms.  If the middle level circulation is still intact when it emerges west of Hispaniola, then it is possible that momentum could be transferred to the surface and a new low level center spun up.  Erika would most likely be a tropical depression at most at that time.  The water north of Cuba is very warm and if Erika still exists, it could intensify somewhat as it moves toward Florida.

The winds in the lower levels continued to push Erika toward the west-northwest on Friday and that general motion is likely continue for the next 12 to 12 hours.  Erika is getting closer to the western end of the subtropical high and it could turn more toward the north during the weekend.  On its anticipated track Erika or its remnants could be approaching the Florida Keys on Sunday afternoon.  At this time it is almost impossible to know how strong it will be at that time.  If Erika does start to reorganize when it gets west of Hispaniola, watches and/or warnings could be issued for parts of Florida.

Erika Bringing Heavy Rain to the Northeastern Caribbean

Although it is not very well organized, Tropical Storm Erika brought heavy rains to parts of the northeastern Caribbean Sea on Thursday and it caused flooding on Dominica.  At 11:00 p.m. EDT on Thursday the center of Tropical Storm Erika was located at latitude 16.6°N and longitude 65.3°W which put it about 135 miles (215 km) south-southeast of San Juan, Puerto Rico and about 1145 miles (1850 km) east-southeast of Miami, Florida.  Erika was moving toward the west at 17 m.p.h. (28 km/h).  The maximum sustained wind speed was 45 m.p.h. (70 km/h) and there were wind gusts to 60 m.p.h. (95 km/h).  The minimum surface pressure was 1008 mb.  Tropical Storm Warnings have been issued for Puerto Rico, Vieques, Culebra, the U.S. Virgin Islands, the British Virgin Islands, the southeastern Bahamas, the Turks and Caicos, the coast of the Dominican Republic from Isla Saona to the border with Haiti, St. Barthelemy and St. Martin.  Tropical Storm Watches have been issued for the Central Bahamas and the coast of the Dominican Republic from Isla Saona to Punta Palenque.

The circulation around Tropical Storm Erika is poorly organized to due persistent upper level winds from the west which are causing vertical wind shear.  The low level circulation consists of a large diffuse center with at least once smaller mesoscale center rotating around inside the larger diffuse center.  The mesoscale center could have been produced by one of the thunderstorm clusters that form nightly in the southeastern portion of the circulation.  Again on Thursday the strongest thunderstorms occurred east of the center of circulation.  Those thunderstorms produced a lot of upper level divergence but the upper level westerly winds pushed that divergence east of the low level center.  As a result, the surface pressure actually rose a couple of millibars on Thursday.  Stronger thunderstorms are forming southeast of the center of Erika again tonight.  So, the pattern of the past several nights appears to be repeating itself again.

An upper level trough over the western Caribbean Sea is causing the westerly winds that are the source of vertical wind shear over Erika.  That trough is expected to drift west and slowly weaken.  If it does weaken in a couple of days, then the upper level wind pattern could be more favorable for intensification.  However, the center of Erika could pass over or very near Hispaniola.  It is likely that the mountains on that island would significantly disrupt the low level circulation.  If the low level circulation maintains its integrity, the Sea Surface Temperatures around the Bahamas and south Florida are very warm.  If Erika still has a coherent circulation at that time it could organize quickly.

A subtropical ridge is steering Erika toward the west.  Erika is nearing the western end of the ridge and a turn toward the west-northwest is possible.  If Erika gets stronger and the circulation is taller, then the upper level trough could push it more toward the north.  On the other hand, if the circulation of Erika stays weaker and shorter, then lower level flow could push it farther west.  Erika is likely to pass near or over Hispaniola on Friday and on its anticipated track it could be approaching south Florida in about 72 hours.

Even if Erika is a disorganized tropical storm it is capable of producing heavy rains and flooding on any island it crosses.

Tropical Storm Erika Approaches the Leeward Islands

Tropical Storm Erika moved steadily toward the Leeward Islands on Wednesday.  At 11:00 p.m. EDT on Wednesday the center of Tropical Storm Erika was located at latitude 16.7°N and longitude 60.2°W which put it about 110 miles (175 km) east-southeast of Antigua and about 1400 miles east-southeast of Miami, Florida.  Erika was moving toward the west at 16 m.p.h. (26 km/h).  The maximum sustained wind speed was 45 m.p.h. (70 km/h) and there were wind gusts to 60 m.p.h. (95 km/h).  The minimum surface pressure was 1006 mb.  Tropical Storm Warnings have been issued for Anguilla, Saba, St. Eustatius and St. Maarten, Puerto Rico, U.S. Virgin Islands, British Virgin Islands, Montserrat, Antigua, Barbuda, St. Kitts, Nevis, St. Martin and St. Barthelemy.  Tropical Storm Watches have been issued for the coast of the Dominican Republic from Cabo Engano to Cabo Frances Viejo, the southeastern Bahamas and the Turks and Caicos, and Guadeloupe.

Although Erika looks very impressive on infrared satellite images with a large area of cold cloud tops, it is in reality very poorly organized.  The thunderstorms generating those cold clouds are located southeast of the low level center of circulation.  There are not really any thunderstorms in other parts of Erika.  There could be a mid-level center of circulation within the cluster of thunderstorms southeast of the surface center.  Well organized tropical cyclones are vertically stacked with the mid-level center directly above the surface center.  This is certainly not the case with Erika.  Upper level winds from the west appear to be causing vertical wind shear over Erika and that is contributing to the poor organization.

Erika is moving over water where the Sea Surface temperature is almost 29°C.  So, there is sufficient energy in the upper ocean to support intensification.  However, an upper level trough over the central Caribbean Sea could continue to cause wind shear over Erika.  The intensity guidance is inconsistent.  Some guidance strengthens Erika to a hurricane during the next few days, while other guidance weakens it.  Until the circulation become more well organized and thunderstorms develop near the center of circulation, significant intensification is unlikely.  If the vertical wind shear gets any stronger it could weaken Erika to a tropical depression.

The track forecast is also challenging.  The numerical guidance shifted the track toward the east on Wednesday evening, but that was due to the fact that the models were predicting that Erika would become a stronger hurricane.  If it become a stronger storm with a taller, vertically coherent circulation, then the upper trough over the Caribbean could push Erika farther east.  However, if Erika remains weaker, then the winds in the lower levels of the atmosphere could push it farther to the west.  On its anticipated track Erika could approach southeastern Florida in about four days.