Category Archives: Atlantic, Caribbean, and Gulf of Mexico

Atlantic TCs

Tropical Storm Earl Nearing Southern Bay of Campeche

Tropical Storm Earl was maintaining its intensity as it approached the southern Bay of Campeche on Thursday night.  At 11:00 p.m. EDT on Thursday the center of Tropical Storm Earl was located at latitude 18.1°N and longitude 91.7°W which put it about 40 miles (65 km/h) south-southeast of Ciudad del Carmen, Mexico.  Earl was moving toward the west-northwest at 10 m.p.h. (16 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 1000 mb.

The government of Mexico has issued a Tropical Storm Warning for the portion of the coast from Ciudad del Carmen to Laguna Verde.

Despite moving over land for almost 24 hours the structure of Tropical Storm Earl retained much of its integrity.  A primary rainband wrapped around three quarters of the way around the southern and eastern portions of the center center.  A weather station at Ciudad del Carmen reported wind gusts to tropical storm force.  The circulation of Tropical Storm Earl is still generating upper level divergence, especially to the east of Earl.  The upper level divergence pumped out enough mass to allow the surface pressure to remain near 1000 mb.

The center of Tropical Storm Earl could move near the southern Bay of Campeche on Friday morning.  The Sea Surface Temperature is near 30°C in that part of the Bay of Campeche.  If Earl moves along the coast, it is likely to maintain tropical storm intensity for another 24 to 36 hours.  If the center of Earl moves out over the southern Bay of Campeche it could intensify given the organization that still exists in the tropical storm.

A ridge of high pressure is steering Tropical Storm Earl toward the west-northwest and that general motion is expected to continue.  On its anticipated track Tropical Storm Earl could be near Veracruz, Mexico in another 24 hours.  The primary risk associated with Tropical Storm Earl is heavy rain and flooding.  Tropical Storm Earl is still causing heavy rain over parts of Mexico, Honduras and Belize.  However, Earl could also generate some storm surge along portions of the southern Bay of Campeche.

Earl Becomes a Hurricane As It Moves Toward Belize

A NOAA aircraft investigating Tropical Storm Earl found that there were sustained winds to hurricane force and the National Hurricane Center upgrade it to Hurricane Earl at 5:00 p.m. EDT on Wednesday.  At 5:00 p.m EDT the center of Hurricane Earl was located at latitude 17.1°N and longitude 86.0°W which put it about 150 miles (240 km) east of Belize City, Belize.  Earl was moving slightly north of due west at 14 m.p.h. (22 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 988 mb.

A Hurricane Warning is in effect for the Bay Islands of Honduras and the portion of the coast from Puerto Costa Mayo, Mexico to the Belize/Guatemala border.  A Tropical Storm Warning is in effect for the coast of Honduras from Cabo Gracias a Dios to the Honduras/Guatemala border and from Punta Allen, Mexico to Puerto Costa Mayo.

The Hurricane Intensity Index (HII) for Earl is 10.4.  The Hurricane Size Index (HSI) is 8.0 and the Hurricane Intensity Size Index (HWISI) is 18.4.  Those indices mean that Earl is capable of causing localized minor wind damage.

The structure of Hurricane Earl improved significantly on Wednesday as it moved farther from the northern coast of Honduras.  An eye developed at the center of circulation and a band of thunderstorms wrapped about two thirds of the way around the eye.  The eyewall is broken southwest of the center.  Additional bands of thunderstorms are rotating around the periphery of the circulation.  The core of strongest winds is relatively small and only extends about 60 miles (95 km) from the center.  However, outer rainbands extend at least 250 miles (400 km) from the center of circulation and the overall size of Hurricane Earl is much larger than it was yesterday.

Hurricane Earl is moving through an environment that is favorable for further intensification.  It is moving over water where the Sea Surface Temperature is near 30°C.  It is located beneath an upper level ridge and the upper level winds are weak.  So, there is little vertical wind shear and the ridge is enhancing the upper level divergence.  Hurricane Earl has another 10 – 15 hours to intensify before it reaches the coast.  Earl will weaken as it moves inland, but it could re-intensify after it moves over the Bay of Campeche.  The amount of re-intensification will depend on how long Hurricane Earl remains over land and where it enters the Bay of Campeche.

A subtropical high pressure system is steering Hurricane Earl on a track that is a little north of due west and that general motion is expected to continue for several more days.  On its anticipated track the center of Hurricane Earl will reach the coast near the border between Mexico and Belize in about 10 – 15 hours.

Since it is a hurricane, Earl will be capable of causing some wind damage.  Hurricane Earl will also create a storm surge near and to the north of where the center makes landfall because the winds will be pushing water toward the coast.  The size and number of the rainbands in Hurricane Earl will create the potential for very heavy rainfall and serious flooding as it moves inland over Belize and Mexico.

Tropical Storm Earl Forms over the Western Caribbean

Based on data collected by an Air Force Reserve Hurricane Hunter reconnaissance plane, the National Hurricane Center designated a system previously known as Invest 97L as Tropical Storm Earl.  At 12:00 p.m. EDT on Tuesday the center of Tropical Storm Earl was located at latitude 16.3°N and longitude 80.2°W which put it about 535 miles (860 km) east of Belize City, Belize.  Earl was moving toward the west at 22 m.p.h. (35 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 1001 mb.

A Hurricane Watch and a Tropical Storm Warning has been issued for the portion of the coast from Punta Allen, Mexico to the Belize/Guatemala border.  A Tropical Storm Warning has been issued for the portion of the coast from Cabo Gracias a Dios to the Honduras/Guatemala border.

The recon plane found a small closed low level center of circulation on the western edge of a cluster of thunderstorms.  The circulation around Tropical Storm Earl is very small.  Winds to tropical storm force only extend out about 80 miles (130 km) from the center of circulation.  Most of the thunderstorms are occurring in the eastern half of the tropical storm.  Those thunderstorms are generating upper level divergence which has pumped out enough mass to allow the surface pressure to decrease a few millibars during the past 12 hours.

The environment around Tropical Storm Earl is somewhat favorable for intensification.  It is moving over water where the Sea Surface Temperature is near 29°C.  An upper level low centered near the western tip of Cuba is producing southwesterly winds which are blowing over the western side of Tropical Storm Earl.  Those westerly winds are producing some vertical wind shear, which is why most of the thunderstorms are in the eastern half of Earl.  The wind shear is inhibiting intensification, but the upper low is forecast to move farther from Earl, which would reduce the shear.  If Earl move north of the coast of Honduras, it should intensify.  However, if the center of circulation moves over Honduras, then Earl could weaken fairly quickly because of its small size.

The subtropical high over the Atlantic Ocean is steering Tropical Storm Earl toward the west at a fairly rapid speed.  The high is expected to continue to steer Earl toward the west during the next several days, but the tropical storm is expected to move a little more slowly on Wednesday.  On its anticipated track the center of Tropical Storm Earl is expected to pass just north of the coast of Belize.  Earl could be very close to Belize in about 36 hours.

Earl is a small tropical storm and the greatest risks are locally heavy rainfall and flash flooding.

Possible Tropical Development

The National Hurricane Center (NHC) is monitoring two tropical disturbances which are designated Invest 96L and Invest 97L for possible development into tropical cyclones.

At 8:00 p.m. EDT on Thursday the center of Invest 97L was located at latitude 13.4°N and longitude 37.0°W which put it about 1525 miles (2460 km) east-southeast of the Leeward Islands.  Invest 97L was moving toward the west at 21 m.p.h. (34 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 1011 mb.

At 8:00 p.m. EDT on Thursday the center of Invest 96L was located at latitude 11.2°N and longitude 20.9°W which put it about 320 miles (515 km) south-southeast of the Cape Verde Islands.  Invest 96L was moving toward the west-northwest at 9 m.p.h. (15 km/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 1010 mb.

Invest 97L consists of a fast moving tropical wave over the central Atlantic Ocean.  The circulation of Invest 97L is not well organized.  A few thunderstorms are occurring near the northern part of the axis of the tropical wave, but convection is scattered.  The rapid forward motion of the wave is preventing the thunderstorms from consolidating around a center of circulation.

If the forward speed of Invest 97L slows, then it may move into an environment that is more favorable for the development of a tropical cyclone.  It is over water where the Sea Surface Temperature (SST) is near 27°C and it will move over warmer water as it gets closer to the Caribbean Sea.  There is not much vertical wind shear except for the low level shear created by the rapid forward motion of the wave.  There is drier air to the north of Invest 97L, but it is embedded in the moister air closer to the Equator.  NHC has a 30% probability that Invest 97L will develop into a tropical cyclone during the next five days.  As a result, NHC has tentatively tasked a plane to fly reconnaissance into Invest 97L on Saturday if it shows signs of developing as it approaches the Caribbean Sea.

Invest 96L also consists of a tropical wave, but it is more well organized than Invest 97L  There are numerous thunderstorms west of the center of circulation and some rainbands are developing south of the center of circulation.  The thunderstorms west of the center are starting to generate some upper level divergence to the west of Invest 96L.  There are some indications that a low level center of circulation may be forming.

Invest 96L is currently in an environment that is mostly favorable for further development.  It is moving over water where the SSTs are near 28°C.  An upper level ridge north of Invest 96L is causing easterly winds to blow over the top of it.  The vertical wind shear is moderate and shear is the primary factor slowing the organization of the Invest 96L.  NHC has a 40% probability that Invest 96L will develop into a tropical cyclone during the next five days.

Because it is more well organized and it is moving more slowly, Invest 96L has a better chance for developing into a tropical cyclone during the next two days.  However, Invest 96L could move into a less favorable environment after that time.  Invest 97L will be moving into a more favorable environment during the weekend.  If Invest 97L holds together until its forward speed slows, then it could have a better chance of developing in several days.  If Invest 97L becomes a tropical cyclone it could threaten portions of the Caribbean Sea.

TD 4 Intensifies to Tropical Storm Danielle As It Nears Mexico

A large area of thunderstorms developed near the center of Tropical Depression 4 during during the overnight hours.  An Air Force Reserve Hurricane Hunter reconnaissance aircraft found sustained winds to tropical storm force and at 8:00 a.m. EDT on Monday the National Hurricane Center classified the system as Tropical Storm Danielle.

At 8:00 a.m. EDT on Monday the center of Tropical Storm Danielle was located at latitude 20.6°N and longitude 96.0°W which put it about 95 miles (150 km) east-southeast of Tuxpan, Mexico.  Danielle was moving toward the west-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 1008 mb.  The government of Mexico has issued a Tropical Storm warning for the portion of the coast from Laguna Verde to Rio Panuco.

The center of an upper level ridge moved near the center of Danielle on Sunday night, which caused the upper level winds to be weaker over the core of the circulation.  As a result, a large area of thunderstorms was able to develop and persist around the center of circulation.  Since Danielle was over water where the Sea Surface Temperature was near 30°C, the circulation was able to extract energy from the ocean and Danielle intensified into a tropical storm.

The thunderstorms at the core of Danielle are generating upper level divergence that is pumping mass out in all direction.  The pressure at the surface is likely to decrease which should produce an additional increase in the wind speed.  Danielle will be over very warm water until it makes landfall on the coast of Mexico later today.  It is likely to intensify further before it reaches the coast.

An ridge of high pressure extends from the Atlantic Ocean into the Gulf of Mexico.  The ridge is steering Danielle toward the west-northwest and that general motion is expected to continue.  On its anticipated track the center of Danielle could be very near Tuxpan on the coast of Mexico in about 12 hours.  Danielle could produce a storm surge of several feet along the coast.  It could also cause some wind damage, although that should be minimal.  The increase in thunderstorms near the center of circulation means that Danielle will produce locally heavy rain when it moves inland.  The heavy rain will create the risk of flash floods and mudslides on steeper slopes.

Danielle was designated a tropical storm on June 20, which makes it the fourth Atlantic tropical storm of 2016.  June 20th is the earliest date on record on which the fourth Atlantic tropical storm has formed.  The previous record was June 23, which was the date when Tropical Storm Debbie was named in 2012.   During the record setting year of 2005, the fourth Atlantic tropical storm was not named until July 5.

Tropical Depression 4 Forms Over Bay of Campeche

An Air Force Reserve Hurricane Hunter aircraft investigated an area of low pressure over the Bay of Campeche on Sunday afternoon and found that there was sufficient organization for the National Hurricane Center to designate the system Tropical Depression 4.  At 11:00 p.m. EDT on Sunday the center of Tropical Depression 4 (TD4) was located at latitude 20.1°N and longitude 95.4°W which put it about 145 miles (230 km) east-southeast of Tuxpan, Mexico.  TD4 was moving toward the west at 7 m.p.h. (11 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 1009 mb.  The government of Mexico has issued a Tropical Storm Warning for the portion of the coast from Laguna Verde to Rio Panuco.

Although the reconnaissance aircraft found that the circulation was better organized than it was on Saturday, it still is not well organized.  There is a distinct center of circulation, but the thunderstorms near the center have been developing and then weakening.  The circulation appears to be somewhat elongated and stretches from the southeast toward the northwest.  A persistent rain band is east and north of the center of circulation and some of the stronger winds are occurring in the rainband.  A new cluster of thunderstorms appears to be developing near the center, and it could represent an improvement in the organization of the depression.

The environment is marginally favorable for intensification.  Tropical Depression 4 is over water where the Sea Surface Temperature is near 30°C.  An upper level ridge is producing some vertical wind shear, but the upper level ridge is also enhancing upper level divergence to the east of the depression.  The depression is close to tropical storm intensity and it has another 12-18 hours to intensify before it makes landfall in Mexico.

A ridge of high pressure that extends from the Atlantic Ocean over the Gulf of Mexico is steering the depression toward the west and that general steering motion is expected to continue.  On its anticipated track, Tropical Depression 4 will make landfall in Mexico on Monday.  The depression could produce locally heavy rainfall and flash flooding will be the primary risk when it makes landfall.

Invest 94L Moves Over Southern Bay of Campeche

A tropical disturbance designated as Invest 94L moved out over the southern Bay of Campeche on Saturday morning.  At 2:00 p.m. EDT on Saturday the center of Invest 94L was located at latitude 19.0°N and longitude 91.8°W which put it about 20 miles (35 km) northeast of Ciudad del Carmen, Mexico.  Invest 94L was moving toward the west-northwest at 8 m.p.h. (13 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.  The National Hurricane Center is putting the probability of development of a tropical cyclone at 50%.  A reconnaissance plane has tentatively been tasked to investigate the system on Sunday afternoon, if necessary.

There is a broad area of lower pressure centered over the extreme southern Bay of Campeche.  However, there is no well formed core at the center of the circulation.  In addition there are only thin fragmented lines of showers and thunderstorms instead of well formed spiral bands.  The circulation seems to exist primarily in the lower portion of the atmosphere.  An upper level ridge east of Invest 94L is providing some upper level divergence.

The center of Invest 94L has moved over water and the Sea Surface Temperatures in the southern Bay of Campeche are 30°C – 31°C.  So there is plenty of energy in the upper ocean to support tropical development.  However, the western side of the upper level ridge is causing southerly winds to blow over the top of Invest 94L which is creating vertical wind shear.  The southern portion of the circulation is still over land, which is also an inhibiting factor.  The combination of positive and negative environmental factors are contributing to the uncertainty over the possible development of Invest 94L.

Invest 94L is being steered toward the west-northwest by a ridge of high pressure to its northeast.  On its anticipated track, the center of Invest 94L will remain over water for another 24 to 48 hours.  That time period represents the window during which Invest 94L could develop into a tropical depression or a tropical storm.  Invest 94L is likely to reach the coast of Mexico in about two days and when it moves inland, the chance for development will end.

Tropical Storm Colin Near Landfall in Florida

Tropical Storm Colin accelerated toward the northeast on Monday afternoon and the center of circulation is about to make landfall near Steinhatchee, Florida.  At 11:00 p.m. EDT on Monday the center of Tropical Storm Colin was located at latitude 29.8°N and longitude 83.8°W which put it about 65 miles (105 km) northwest of Cedar Key, Florida.  Colin was moving toward the northeast at 22 m.p.h. (35 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 1001 mb.

A Tropical Storm Warning is in effect for the portion of the coast from Indian Pass to Englewood, Florida.  A Tropical Storm Warning is also in effect for the East Coast from Sebastian Inlet, Florida to Oregon Inlet, North Carolina.

Although Tropical Storm Colin looked ragged on satellite and radar imagery, the pressure did drop to 1001 mb on Monday.  Colin is a very asymmetric tropical storm.  Almost all of the rain and stronger winds are in the eastern half of the circulation.  Most of the heavier rain is falling in bands southeast and northeast of the center.  An upper level trough over Mexico is producing strong southwesterly winds which are blowing over the western half of Colin.  Despite significant vertical wind shear, the center of circulation became more well defined on Monday.  There are few thunderstorms near the center and Colin is clearly a sheared tropical cyclone.

Tropical Storm Colin did produce minor storm surges along the west coast of Florida where the winds pushed the water toward the coast.  Local coastal flooding occurred, especially in the most surge prone areas.  In addition Tropical Storm Colin produced heavy rainfall over the peninsula of Florida.

Normally, a tropical storm weakens when it moves over land because there is more friction and it is removed from its energy source.  However, Tropical Storm Colin could move into a region where there is more upper level divergence.  If the upper level divergence pumps out more mass, the surface pressure could fall and the wind speeds could increase a little bit.  In addition, if Colin moves toward the northeast more quickly then the effect of vertical wind shear will be less.  The wind speed in Tropical Storm Colin is forecast to increase a little on Tuesday, even though it could start to lose its tropical characteristics.

The upper level trough should continue to steer Tropical Storm Colin toward the northeast on Tuesday.  It is expected to move rapidly across northeast Florida and the center of Colin could emerge over the Atlantic Ocean by Tuesday morning.  The center of Colin is expected to move close to the coast of the Carolinas and it could be east of Cape Hatteras by Tuesday night.

On its anticipated track, the strongest winds should occur over the Atlantic Ocean.  Tropical Storm Colin could contribute to locally heavy rainfall in northeast Florida, extreme southeast Georgia and coastal portions of South Carolina and North Carolina.  Wave action could cause some beach erosion.  Wind damage should be minimal, although some power outages could occur.

Tropical Storm Colin Forms Over Gulf of Mexico and Heads for Florida

A broad area of low pressure over the southern Gulf of Mexico became more organized on Sunday and a U.S. Air Force Reserve Hurricane Hunter reconnaissance aircraft found sustained winds of 40 m.p.h. (65 km/h).  As a result, the National Hurricane Center classified the system as Tropical Storm Colin.  At 11:00 p.m. EDT on Sunday the center of Tropical Storm Colin was located at latitude 23.6°N and longitude 87.8°W which put it about 450 miles (720 km) southwest of Tampa, Florida.  Colin was moving toward the north at 9 m.p.h. (15 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 1003 mb.

A Tropical Storm Warning has been issued for the portion of the coast from Indian Pass to Englewood, Florida.  A Tropical Storm Warning has also been issued for the East Coast from Sebastian Inlet, Florida to Altamaha Sound, Georgia.  A Tropical Storm Watch has been issued for the portion of the coast from Altamaha Sound, Georgia to South Santee River, South Carolina.

The circulation of Tropical Storm Colin is very asymmetrical.  The stronger winds and most of the thunderstorms are east of the center of circulation.  Some rotation in the middle levels in the primary band on the east side of Colin is apparent on satellite imagery.  Winds to tropical storm force are occurring up to 185 miles (295 km) from the center of circulation.  However, the winds are much weaker in the western half of the circulation.

The environment around Tropical Storm Colin is marginal for intensification.  Colin is moving over water where the Sea Surface Temperature is near 28°C to 29°C.  So, there is sufficient energy in the upper ocean to support intensification.  An upper level low near Texas and an upper level ridge east of Colin are combining to produce southwesterly winds that are blowing over the western half of the storm.  Those winds are causing strong vertical wind shear which is preventing the development of thunderstorms in that part of the storm.  Part of the upper level ridge is over the eastern half of the circulation.  The upper level winds are weaker there and there is less vertical wind shear, which is allowing strong thunderstorms to persist in that part of Colin.  The upper level ridge is also enhancing upper level divergence to the east of Tropical Storm Colin.  If a new center of circulation were to form closer to the upper level ridge, then more intensification would be possible.  Colin is likely to intensify somewhat on Monday.

The upper low and upper level ridge are also steering Tropical Storm Colin toward the north.  Those features are expected to turn Colin toward the northeast on Monday.  On its anticipated track Tropical Storm Colin will approach the coast of Florida between Tampa and Apalachicola on Monday evening.  However, if a new center of circulation develops farther east, Colin could make landfall farther south along the coast and earlier on Monday.

Heavy rainfall is the greatest risk with Tropical Storm Colin.  It is pulling very humid air from the Caribbean Sea northward over the eastern Gulf of Mexico.  Tropical Storm Colin could also generate a storm surge of 1-6 feet near where the center makes landfall.  The coast along the northeastern Gulf of Mexico is very susceptible to storm surges and water rises will occur in that area.  Wind damage is likely to be minimal, although power outages may occur.  Some tornadoes could be generated when Colin moves over land.  Locally heavy rain could also fall in portions of the Mid-Atlantic states as the circulation of Tropical Storm Colin interacts with a cold front.

Tropical Storm Colin was named on June 5, which is the earliest date on record on which the third Atlantic Tropical Storm has formed.  During the record setting year of 2005 Tropical Storm (later to become Hurricane) Cindy was named on July 5.

Disturbance Near Yucatan Could Develop Over Gulf of Mexico

A tropical disturbance over the northwestern Caribbean Sea near the Yucatan peninsula is moving northwest and it could develop into a tropical cyclone when it moves over the southern Gulf of Mexico.  The National Hurricane Center (NHC) has designated the disturbance as Invest 93L and NHC is putting the probability of development into a tropical cyclone during the next two days at 80%.  At 8:00 p.m. EDT the center of Invest 93L was located at latitude 18.5°N and longitude 87.5°W which put it about 170 miles (270 km) south of Cancun, Mexico.  Invest 93L was moving toward the northwest at 11 m.p.h. (17 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.

Invest 93L consists of a broad area of low pressure at the surface.  Several bands of thunderstorms are occurring in the eastern and northern parts of the circulation.  There is no well defined center of circulation and there are fewer thunderstorms in the inner portion of the circulation.  The strongest winds are occurring in the bands of thunderstorms north and east of the center.  There is some upper level divergence to the east of Invest 93L.

The environment around Invest 93L is not totally favorable for development.  The Sea Surface Temperature in northwest Caribbean Sea is near 30°C, which means there is plenty of energy in the upper ocean.  However, an upper level low near Texas and an upper level ridge east of Invest 93L are combining to generate strong southwesterly winds that are blowing over the top of the disturbance.  Those winds are creating significant vertical wind shear which is inhibiting the development of Invest 93L.  The upper level ridge is enhancing the upper level divergence to the east of the disturbance which allowed the pressure to fall several millibars on Saturday.  The upper winds are lighter near the axis of the ridge which is why the stronger bands of thunderstorms are persisting in that area.

Invest 93L is forecast to move toward the Yucatan peninsula on Sunday.  If the broad area over low pressure moves over land that will prevent it from developing until it moves back over water.  Numerical models are guiding that the disturbance will develop into a tropical cyclone when the area of low pressure moves over the southern Gulf of Mexico.  The upper level ridge is forecast to extend over the southeastern Gulf and if that happens the wind shear could decrease enough to allow development to occur.  Invest 93L could become a tropical depression or a tropical storm over the Gulf of Mexico.

The southwesterly flow over the Gulf of Mexico is forecast to turn Invest 93L toward the northeast.  On its anticipated track the system could reach the west coast of Florida near Cedar Key late Monday or early Tuesday.  The primary risk is likely to be locally heavy rain.  However, the coast in that area is very susceptible to storm surge and there could be some rise in the water level.  The National Hurricane Center has tentatively tasked a reconnaissance plane to investigate Invest 93L on Sunday, if necessary.