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Blas Intensifies Into a Hurricane

Tropical Storm Blas intensified into the first Eastern North Pacific hurricane of 2016 on Monday.  At 5:00 p.m. EDT on Monday the center of Hurricane Blas was located at latitude 13.7°N and longitude 115.7°W which put it about 740 miles (1190 km) southwest of the southern tip of Baja California.  Blas was moving toward the west-northwest at 14 m.p.h. (22 km/h).  The maximum sustained wind speed was 75 m.p.h. (120 km/h) and there were gusts  to 90 m.p.h. (145 km/h).  The minimum surface pressure was 994 mb.

The Hurricane Intensity Index (HII) for Blas was 10.4.  The Hurricane Size Index (HSI) was 6.1.  The Hurricane Wind Intensity Size Index (HWISI) was 16.5.

The large circulation of Hurricane Blas is still organizing.  A primary rainband wrapped around the center of circulation and an eye may be forming in the center of Blas.  Additional bands of thunderstorms are spiraling around the core of Hurricane Blas.  The thunderstorms near the center of circulation are generating upper level divergence which is pumping out mass.  Despite the improved organization the wind field around Hurricane Blas is asymmetrical.  Winds to hurricane force are occurring primarily in the eastern half of the circulation.  The strongest winds extend out about 25 miles (40 km) east of the center of Hurricane Blas.  Winds to tropical storm force extend out about 150 miles (240 km) east of the center, but only about 80 miles (130 km) west of the center.

Hurricane Blas is in an environment that is favorable for further intensification.  It is moving over water where the Sea Surface Temperature is near 29°C.  An upper level ridge north of Blas is generating some northeasterly winds which are blowing over the top of the circulation.  The vertical wind shear is moderate.  It is slowing the rate of intensification, but the shear is unlikely to prevent Hurricane Blas from intensifying during the next several days.  Blas does have a chance to become a major hurricane later this week.

A ridge of high pressure is steering Hurricane Blas toward the west-northwest and that general motion is expect to continue for several more days.  Hurricane Blas is moving farther away from Mexico.

Tropical Storm Blas Forms West of Mexico

After having no tropical storms during the first month and a half of the Eastern North Pacific hurricane season, Blas became the second tropical storm to form in the past two days.  At 11:00 p.m. EDT on Sunday the center of Tropical Storm Blas was located at latitude 12.4°N and longitude 112.2°W which put it about 740 miles (1190 km) south-southwest of the southern tip of Baja California.  Blas was moving toward the west-northwest at 12 m.p.h. (19 km/h).  The maximum sustained wind speed was 65 m.p.h. (105 km/h) and there were wind gusts to 80 m.p.h. (130 km/h).  The minimum surface pressure was 1001 mb.

The circulation of Tropical Storm Blas organized quickly on Sunday.  A primary rainband wrapped around the western and southern portions of the center of circulation.  Additional rainbands spiraled around the core of the storm.  The intensity of the thunderstorms weakened for a few hours, but storms east of the center of the circulation are intensifying again.  Winds to tropical storm force extend out about 70 miles (115 km) from the center of circulation.

An upper level ridge northeast of Blas is causing some northeasterly winds to blow over the top of the tropical storm.  The winds are responsible for vertical wind shear and they are inhibiting upper level divergence to the east of the circulation.  Tropical Storm Blas is moving over water where the Sea Surface Temperature is near 29°C.  In spite of the vertical wind shear the environment is favorable for intensification and Blas could become a hurricane on Monday.

A ridge of high pressure north of Blas is steering the tropical storm toward the west-northwest and that general motion is expected to continue for the next several days.  Tropical Storm Blas is moving away from Mexico.

Tropical Storm Nepartak Develops South of Guam

A center of circulation organized within an area of thunderstorms south of Guam and the system was designated Tropical Storm Nepartak.  At 11:00 p.m. EDT on Sunday the center of Tropical Storm Nepartak was located at latitude 12.2°N and longitude 141.4°E which put it about 215 miles (345 km) west-southwest of Guam.  Nepartak was moving northwest at 16 m.p.h. (26 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 989 mb.

The circulation of Tropical Storm Nepartak is still organizing.  A primary rainband wrapped around the center and a circular area of thunderstorms formed at the core of the circulation.  The area of thunderstorms is generating upper level divergence which is pumping out mass and allowing the surface pressure to decrease.  Winds to tropical storm force extend our about 100 miles (160 km) from the center of circulation.

An upper level low located north of Nepartak is producing southwesterly winds which area blowing over the top of the tropical storm.  Those winds are creating some vertical wind shear, which is slowing the intensification of Nepartak.  However, the upper low is also enhancing upper level divergence to the northeast of the tropical storm.  Nepartak is moving over water where the Sea Surface Temperature is near 30°C.  The environment is favorable for intensification and Nepartak could become a hurricane during the next several days.

A subtropical ridge located northeast of Nepartak is steering the tropical storm toward the northwest.  That general motion is expected to continue during the next few days.  On its anticipated track, Nepartak could be approaching the southernmost islands of Japan in three or four days.  It is likely to be a typhoon at that time.

Tropical Depression 2E Intensifies Into Tropical Storm Agatha

Tropical Depression 2E intensified into Tropical Storm Agatha on Saturday morning.  At 11:00 a.m. EDT on Saturday the center of Tropical Storm Agatha was located at latitude 15.6°N and longitude 118.9°W which put it about 775 miles (1245 km) southwest of the southern tip of Baja California.  Agatha was moving toward the west-northwest at 12 m.p.h. (19 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 upper level winds blowing over the top to Tropical Depression 2E weakened and the vertical wind shear decreased.  Less vertical wind shear allowed thunderstorms on the northwestern side of the circulation to wrap around the southern side of the center.  With the center of circulation embedded near the main area of thunderstorms the National Hurricane Center named the system Tropical Storm Agatha.  Agatha is a small system and tropical storm force winds only extend out about 45 miles (75 km) from the center.

Agatha has a limited period in which to intensify further.  It is currently moving over water where the Sea Surface Temperature (SST) is near 28°C.  However, Agatha is moving toward cooler SSTs where there will be less energy to drive the circulation.  In addition, there is much drier air north and west of the tropical storm.  Since there is little vertical wind shear, Agatha could intensify during the next 12 to 24 hours.  It will start to weaken when it moves over the cooler SSTs.

A ridge of high pressure north of Agatha is steering the tropical storm toward the east-northwest and that general motion is expected to continue for another day or two.  Agatha currently poses no threat to land.

Agatha was named on July 2.  This is the latest date for the naming of the first tropical storm over the Eastern North Pacific since Ava was named in 1969.

Tropical Depression 2E Forms Southwest of Baja California

After a prolonged period of relatively quiet weather over the Eastern North Pacific Ocean, a tropical depression formed southwest of Baja California.  At 11:00 p.m. EDT on Friday the center of Tropical Depression 2E (TD2E) was located at latitude 14.7°N and longitude 116.7°W which put it about 730 miles (1170 km) southwest of the southern tip of Baja California.  TD2E 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 gusts to 40 m.p.h. (65 km/h).  The minimum surface pressure was 1007 mb.

A tropical wave over the Eastern North Pacific Ocean developed a well defined low level circulation and the National Hurricane Center classified the system as Tropical Depression 2E on Friday night.  Although the structure of the low level wind field is symmetrical, most of the thunderstorms are located northwest of the center of circulation.  An upper level ridge north of the depression is generating easterly winds over the top of the circulation.  The vertical wind shear is causing the asymmetrical distribution of the thunderstorms.

The environment around Tropical Depression 2E is marginal for intensification because there are both positive and negative factors.  TD2E is moving over water where the Sea Surface Temperature is near 29°C.  So, there is plenty of energy in the upper ocean to support intensification.  However, the air to the west of the tropical depression is very dry, which will limit the growth of thunderstorms and the formation of rain bands in that part of the system.  In addition moderate vertical wind shear will also inhibit intensification.  Tropical Depression 2E could intensify during the weekend and it has a chance to become the first named storm of the 2016 Eastern Pacific hurricane season.  However, the potential for intensification is limited.

The ridge to the north of TD2E is expected to continue to steer it toward the west-northwest during the next several days.  Tropical Depression 2E poses no threat to land during the next five days.

Possible Hurricane Formation Southwest of Mexico

Guidance from recent runs of the Global Forecasting System (GFS) model indicate that a tropical cyclone could form southwest of Mexico during the next few days.  A tropical wave will move into the Eastern North Pacific Ocean south of Mexico.  The wave will move over water where the Sea Surface Temperature is between 29°C and 30°C.  Vertical wind shear caused by an upper low near the west coast of Mexico will initially inhibit development of the wave.  The GFS model is forecasting that the tropical wave will move into a region where the upper level winds are light and there will not be much vertical wind shear.  If that scenario occurs then a tropical cyclone could develop during the weekend near latitude 10°N and longitude 105°W.

If a tropical cyclone forms, a ridge of high pressure to the north of the cyclone would likely steer it in a generally west-northwesterly direction which would move it away from Mexico.  The environment would be favorable for intensification.  Rapid intensification may be possible and the system could become a major hurricane next week.

The development of this tropical wave could also be a signal that the Eastern North Pacific is getting active.  Although it has been a bit of a slow start to the hurricane season in that basin, the formation of a hurricane during the next week or so would be consistent with the long term climatology for that region.

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.