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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.

Bonnie Brings Heavy Rain and Flooding to South Carolina

Even though Bonnie weakened to a tropical depression before it made landfall near Charleston, it brought locally heavy rain and flooding to parts of South Carolina and eastern Georgia.  A portion of Interstate 95 was closed due to high water.  At 11:00 p.m. EDT on Sunday the center of Tropical Depression Bonnie was located at latitude 32.8°N and longitude 80.1°W which put it about 5 miles (10 km) west of Charleston, South Carolina.  Bonnie was slowly meandering near the coast.  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 1012 mb.

Strong southeasterly winds in the upper levels generated significant vertical wind shear that weakened Tropical Storm Bonnie to a tropical depression on Sunday morning.  However, the lower level circulation remained relatively intact as Bonnie moved onto the coast near Charleston, South Carolina.  Thunderstorms in a band west of the center of circulation dropped heavy rain in parts of southwestern South Carolina and eastern Georgia.  The heavy rain produced some flooding.

Most of the rain has tapered off to a few narrow bands of showers, which is normal at night when weaker tropical cyclones move inland.  However, daytime heating could destabilize the atmosphere and new thunderstorms could redevelop over land on Monday.  Some of those storms could also produce locally heavy rainfall and cause additional flooding.

The center of Tropical Depression Bonnie has drifted back to near the Atlantic Ocean.  Strong southeasterly winds are still blowing in the upper levels and the vertical wind shear should prevent significant redevelopment even if the center moves back over water.  Proximity to the ocean will make it easier for the circulation to pull in more moisture, which could contribute to heavier rainfall.

A high pressure system over the Atlantic and an approaching cold front will combine to produce southwesterly winds in the lower levels of the atmosphere.  Those low level winds are forecast to steer Tropical Depression Bonnie slowly toward the northeast during the next several days.  On its anticipated track Tropical Depression Bonnie is expected to move slowly along the coast of South Carolina and North Carolina.  The primary risks will be locally heavy rain, flooding and rip currents.

TD 2 Intensifies Into Tropical Storm Bonnie

Tropical Depression 2 intensified into Tropical Storm Bonnie as it passed over the warm waters of the Gulf Stream on Saturday.  At 5:00 p.m. EDT on Saturday the center of Tropical Storm Bonnie was located at latitude 31.1°N and longitude 79.4°W which put it about 120 miles (195 km) south-southeast of Charleston, South Carolina.  Bonnie was moving toward the 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 1008 mb.  A Tropical Storm Warning remains in effect for the coast of South Carolina from the Savannah River to Little River Inlet.

Although the convection in Tropical Depression 2 dissipated when it passed over a region of slightly cooler Sea Surface Temperatures (SSTs) on Friday night, thunderstorms redeveloped and persisted when the system crossed the warmer SSTs in the Gulf Stream on Saturday.  Persistent thunderstorms produced enough increase in the wind speed to intensify Tropical Depression 2 into Tropical Storm Bonnie.

The circulation around Tropical Storm Bonnie is very asymmetrical.  Almost all of the thunderstorms are occurring in the northwestern quadrant of the storm and the strongest winds are being generated in that part of the circulation.  There are mainly thin bands of showers in the rest of the storm.  Winds to tropical storm force extend out about 60 miles (95 km) from the center in the northwest quadrant of Bonnie.

An upper level low over Florida and an upper level ridge over the western Atlantic Ocean are combining to generate southeasterly winds which are blowing over the top of Tropical Storm Bonnie.  Moderate vertical wind shear is contributing to the asymmetrical structure by tilting the circulation toward the northwest.  The wind shear is strong enough to inhibit intensification, but Tropical Storm Bonnie is extracting more energy as it passes over the Gulf Stream.  Bonnie could possibly intensify a little more while it is over the Gulf Stream.

The ridge east of Bonnie is steering the tropical storm toward the northwest and that general motion is expected to continue for another 12 to 24 hours.  An upper level trough approaching the ridge from west and the trough is expected to cause the ridge to weaken.  When the ridge weakens, the steering currents will also weaken.  Tropical Storm Bonnie could stall or meander for several days when that happens.

On its anticipated track the center of Tropical Storm Bonnie will approach the coast of South Carolina on Sunday.  The primary threats are coastal erosion, rip currents and locally heavy rainfall.  Persistent rain could create the potential for fresh water flooding.  Wind damage is likely to be minimal.  However, where the winds blow onshore, they could push water toward the coast and contribute to some coastal flooding.

Tropical Depression 2 Forms, Warning Issued for South Carolina

A reconnaissance plane investigated the system that was formerly designated Invest 91L on Friday afternoon and the plane found that the system had enough tropical characteristics to be classified as Tropical Depression 2 by the National Hurricane Center (NHC).  At 5:00 p.m. EDT on Friday the center of Tropical Depression 2 (TD2) was located at latitude 28.5°N and longitude 74.7°W which put it about 435 miles (695 km) southeast of Charleston, South Carolina.  TD2 was moving toward the west-northwest at 13 m.p.h. (20 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.  A Tropical Storm Warning has been issued for the coast of South Carolina from the Savannah River to Little River Inlet.

The circulation in Tropical Depression 2 became better organized on Friday, but it would not yet be considered well organized.  More thunderstorms formed near the center of circulation and a primary rainband now curls around the the northern and western sides of the center.  However, there are only thin bands of showers in much of the eastern half of the circulation.  With persistent thunderstorms near the core of TD2, it possess enough tropical characteristics to be considered a tropical cyclone.

An upper level low near Cuba and an upper level ridge northeast of TD2 are combining to generate northerly winds over the top of the circulation.  Those winds are causing moderate vertical wind shear.  TD2 will also be moving over slightly cooler Sear Surface Temperatures (SSTs) during the next 12 to 18 hours.  The combination of the vertical wind shear and cooler SSTs could keep TD2 from intensifying much during that time period.  TD2 will move over the warmer SSTs of the Gulf Stream later on Saturday.  The vertical wind shear could also decrease somewhat.  Warmer SSTs and less wind shear could allow TD2 to intensify into Tropical Storm Bonnie later on Saturday.

A ridge northeast of TD2 is steering the tropical depression toward the west-northwest and a general motion in that direction is expected for another 36 to 48 hours.  After about two days the steering currents could weaken.  On its anticipated track TD2/Tropical Storm Bonnie is expected to approach the coast of South Carolina on Sunday.  Coastal erosion, rip currents and locally heavy rain are the primary risks.  Wind damage is likely to be minimal.

 

Invest 91L Slightly Stronger, Moving Toward U.S.

The circulation of the low pressure system designated as Invest 91L strengthened slightly on Thursday.  At 8:00 p.m. EDT on Thursday the center of Invest 91L was located at latitude 27.4°N and longitude 70.9°W which put it about 410 miles (660 km) east-northeast of Great Abaco Island, Bahamas and about 675 miles (1090 km) south-southeast of Charleston, South Carolina.  Invest 91L was moving toward the west-northwest at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 35 m.p.h. (55 km/h) and there were wind gusts to near 45 m.p.h. (70 km/h).  The minimum surface pressure was 1013 mb.  The center of Invest 91L was near NOAA buoy 41047 which reported observations consistent with those numbers.

The organization of Invest 91L improved slightly on Thursday.  A few thunderstorms formed northeast of the center of circulation and they persisted throughout the day.  However, there are few thunderstorms in other parts of Invest 91L.  The circulation became slightly more circular although it is still elongated.  The surface pressure decreased slowly, but steadily throughout the day.

The environment around Invest 91L is only marginal for intensification.  It is over water where the Sea Surface Temperature is near 26°C to 27°C.  However, an upper level low near Cuba and an upper level ridge near the east coast of the U.S. are combining to create southerly winds over the top of Invest 91L.  Those winds are causing moderate levels over vertical wind shear which is inhibiting the development of the system.  The magnitude of the wind shear decreased during the past 24 hours and it could decrease a little more on Friday as the upper level ridge moves farther east.

If more thunderstorms develop near the center of circulation, the system could be classified as a tropical depression or tropical storm.  The National Hurricane Center (NHC) is indicating that there is an 80% probability that the Invest 91L will become a tropical cyclone or subtropical cyclone within 48 hours.  NHC has tentatively tasked a reconnaissance plane to investigate the system on Friday.

The vertical wind shear is limiting the strongest part of the circulation of Invest 91L to the lower half of the troposphere.  Thus, the system is being steered toward the west-northwest by a surface pressure system over the western Atlantic Ocean.  That general motion is expected to continue with a slow northward turn.  On its anticipated track Invest 91L could approach the southeast coast of the U.S. in 48 to 72 hours.

The primary risks with Invest 91L remain coastal erosion, rip currents and locally heavy rainfall.  Some wind damage will be possible, but it is likely to be minimal.

Low Pressure Forms East of the Bahamas

A small area of low pressure developed east of the Bahamas on Wednesday afternoon and the National Hurricane Center designated the system as Invest 91L,  At 8:00 p.m. EDT on Wednesday the center of Invest 91L was located at latitude 26.6°N and longitude 67.7°W which put it about 625 miles (1005 km) east of Great Abaco Island in the Bahamas and about 895 miles (1445 km) south-southeast of Charleston, South Carolina.  Invest 91L was moving toward the north at 8 m.p.h. (13 km/h).  The maximum sustained wind speed was he 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 1015 mb.

The circulation of Invest 91L is not well organized at the current time.  A small center of circulation was evident on late afternoon visible satellite imagery.  Several thin bands of showers are on the eastern side of the center of circulation.  However, there are very few taller thunderstorms and the circulation probably does not have a warm core at the moment.

Although Invest 91L is over water where the Sea Surface Temperature is between 26°C and 27°C, the atmospheric environment is currently unfavorable for further development.  An upper level trough near Florida is causing strong southwesterly winds to blow over the top of Invest 91L and there is significant vertical wind shear.  The wind shear is quickly dissipating any thunderstorms that start to form.  Invest 91L is forecast to move west-northwest into a more favorable environment in about a day or two.  If the system moves west, it will move into an area where the upper level winds are not as strong.  If the surface circulation is still intact at that time, less vertical wind shear could allow for the system to intensify.  The National Hurricane Center places the probability of development of a tropical cyclone or subtropical cyclone within the next five days at 60%.

Since Invest 91L primarily exists in the lower levels, it will be steered by winds in the lower troposphere.  A surface high pressure system centered off the southeast coast of the U.S. is forecast to move north of Invest 91L and the high will steer the system west-northwest toward the coast of the U.S.  On its anticipated track Invest 91L could move near the southeast coast of the U.S. during the weekend.

If Invest 91L intensifies, the highest probability is that it could become a tropical depression or tropical storm as it approaches the U.S.  It could generate coastal erosion, rip currents and locally heavy rainfall.  The threat for wind damage appears to be minimal at the current time.  People near the coast should monitor trusted sources of weather information.

Possible Development Off Southeast U.S. Coast

Even though the official start to Atlantic hurricane season is not until June 1, the atmosphere doesn’t always wait for the calendar to change to June.  Several numerical models have been predicting that a low pressure system will develop somewhere near the Bahamas later this week.  The models are also predicting that the low pressure system will move toward the southeast coast of the U.S.

A frontal boundary is over the western Atlantic Ocean.  The front runs from east of the Mid-Atlantic States to near the northern Bahamas.  Low pressure systems can develop along the southern end of frontal boundaries.  The low pressure system could start as an extratropical (non-tropical) cyclone or a subtropical (hybrid) cyclone.  The exact type of cyclone will be partly determined by the vertical wind shear later this week.  The structure of a low pressure system can change, if the environment changes and the low can be placed in a different category.

An upper level low over the western Atlantic could cause enough vertical wind shear, so that the low pressure system could be initially classified as extratropical or subtropical.  The Sea Surface Temperatures (SSTs) in the area where the low is most likely to develop are near 26° to 27°C.  There will be enough energy in the upper ocean to support the development of a tropical cyclone.  An upper level ridge could move north of the developing surface low later in the week, which could reduce the vertical wind shear.  If the shear decreases and the low pressure system extracts enough energy from the ocean to develop a warm core, it could eventually be classified as a tropical cyclone.

After the low pressure system forms, a high pressure system over the Atlantic Ocean is expected to steer the low northwest toward southeast coast of the U.S.  The low pressure system could make landfall in Georgia, South Carolina or North Carolina during the weekend or early next week.

The primary threats from the low pressure system will be coastal erosion, rip currents and potentially heavy rainfall.  The wind threat appears to be minimal, since even if the low pressure system becomes tropical, the highest probability is that it would be a tropical depression or tropical storm.

There is a great deal of uncertainty about the future of this system.  The timing of the formation of the low, the type of cyclone, the possible track of the cyclone and its intensity should become clearer later this week.  People near the southeast coast should monitor trusted sources of weather information.

Ana Transitions to a Tropical Storm

As Subtropical Storm Ana sat over the relatively warm Sea Surface Temperatures of the Gulf Stream, it drew energy from the upper ocean.  More thunderstorms developed near the center of circulation and condensation released latent energy which warmed the middle and upper levels.  As a result, the circulation became more circularly symmetrical and eventually some upper level outflow developed at the top of the system. As a result of the structural changes, Ana made a transition from a subtropical storm to a tropical storm.

At 11:00 a.m. EDT on Saturday the center of Tropical Storm Ana was located at latitude 32.7°N and longitude 77.9°W which put it about 90 miles southeast of Myrtle Beach, South Carolina and about 105 miles south of Wilmington, North Carolina.  Ana was moving toward the northwest at 3 m.p.h.  The maximum sustained wind speed was 60 m.p.h. and there were gusts to 70 m.p.h.  The minimum surface pressure was 1001 mb.

A Tropical Storm Warning remains in effect from South Santee River, South Carolina to Cape Lookout, North Carolina.  A Tropical Storm Watch is in effect from Edisto Beach to South Santee River, South Carolina.

As the high pressure system that has been blocking the forward progress of Ana moves eastward, the tropical storm will move toward the coast.  It is likely to make landfall near the border of South Carolina and North Carolina on Sunday morning.  An upper level trough approaching from the west will turn Ana toward the northeast and sweep it out to sea after it makes landfall.

Ana is still over the relatively warm water of the Gulf Stream and it is likely to maintain its intensity on Saturday.  When Ana moves north of the Gulf Stream, it will cross over cooler water.  In addition, the approaching upper level trough will begin to generate some vertical wind shear over Ana.  The effects of cooler water and more wind shear mean that Ana will likely be weakening as it approaches the coast.  It will bring some wind, locally heavy rain and beach erosion, but the impacts should be minor in most locations.

Tropical Storm Warning Issued for Ana

The National Hurricane Center has issued a Tropical Storm Warning for the portion of the coast from South Santee River, South Carolina to Surf City, North Carolina.  A Tropical Storm Watch remains in effect from Edisto Beach to South Santee River, South Carolina and from Surf City to Cape Lookout, North Carolina.

At 11:00 a.m. EDT on Friday the center of Subtropical Storm Ana was located at latitude 31.5°N north and longitude 77.3°W which put it about 250 miles east of Savannah, Georgia, about 190 miles east-southeast of Charleston, South Carolina and about 180 miles south-southeast of Wilmington, North Carolina.  Ana was nearly stationary.  The maximum sustained wind speed was 45 m.p.h. and there were gusts to 60 m.p.h.  The minimum surface pressure was 1001 mb.

Thunderstorms are forming on the southern and eastern sides of the circulation and Ana is beginning to look more like a tropical cyclone on satellite images.  It could slowly make a transition to a tropical storm during the next several days.

A high pressure system north of Ana is expected to move slowly eastward and steer Ana toward the coast during the next two or three days.  After that time an upper level trough approaching from the west is expected to steer Ana to the northeast and out to sea.

A combination of marginal Sea Surface Temperatures, drier air and some vertical wind shear is expected to limit the potential for intensification.  However, some modest intensification is possible and the surface pressure has decreased slightly in recent hours.