Tag Archives: Mexico

Dolores Becomes a Major Hurricane

Hurricane Dolores intensified rapidly on Tuesday night and it has reached Major Hurricane status.  At 11:00 a.m. EDT on Wednesday the center of Hurricane Dolores was located at latitude 18.4°N and longitude 110.2°W which put it about 310 miles (500 km) south of Cabo San Lucas, Mexico.  The maximum sustained wind speed was 130 m.p.h. (215 km/h) which made Dolores a Category 3 hurricane on the Saffir-Simpson Scale.  There were wind gusts to 160 m.p.h. (260 km/h) and the minimum surface pressure was 946 mb.

Dolores is currently over water where the Sea Surface Temperature (SST) is around 29°C.  It is generating well developed upper level outflow which is pumping out mass and there is not much vertical wind shear.  Dolores could strengthen some more during the next 24 hours, although eyewall replacement cycles could produce fluctuations in intensity.  When Dolores moves north of latitude 20°N, it will move over cooler SSTs and it should start to weaken.  Given its size and intensity, it could take several days for the circulation around Dolores to spin down.

A ridge in the middle levels is steering Dolores toward the west-northwest.  That general steering pattern is expected to continue during the next few days and Dolores poses no current threat to land.

Tropical Storm Dolores Forms South of Mexico

A low level circulation organized in a large area of thunderstorms south of Acapulco, Mexico on Sunday and the system was classified as Tropical Storm Dolores.  At 2:00 p.m. EDT on Sunday the center of Tropical Storm Dolores was located at latitude 15.6°N and longitude 102.1°W which put it about 145 miles (230 km) south-southwest of Zihuatanejo, Mexico and about 295 miles (475 km) southeast of Manzanillo, Mexico.  Dolores was moving toward the northwest at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 45 m.p.h. (75 km/h) and there were wind gusts to 55 m.p.h. (90 km/h).  The minimum surface pressure was 1002 mb.  The government of Mexico has issued a Tropical Storm Watch for the portion of the coast from Lazaro Cardenas to Cabo Corrientes.

The circulation around Dolores is not particularly well organized.  Most of the strong thunderstorms are occurring in the eastern half of the circulation.  There are few thunderstorms in the southwestern part of the tropical storm.  Upper level winds are light over Dolores and the tropical storm is producing strong upper level divergence which is pumping out mass.  Dolores is over water where the Sea Surface Temperatures are near 30°C and there is plenty of energy in the upper ocean to support intensification.  Dolores is close enough to Mexico that it could be pulling in some drier air from land, which may be inhibiting intensification at this time.  The environmental factors would support intensification and rapid intensification may be possible if Dolores moves farther away from the coast of Mexico.

A strong mid-level ridge over Texas and Mexico is steering Dolores toward the west-northwest.  That general steering pattern is expected to continue for the next few days.  On its anticipated track the center of Dolores is forecast to stay west of the coast of Mexico.  However, the proximity of Dolores to the coast prompted the issuance of a Tropical Storm Watch for a portion of the coast.

Hurricane Carlos Weakening Quickly

It appears from satellite imagery that vertical wind shear quickly weakened Hurricane Carlos on Tuesday night.  At 11:00 p.m. EDT on Tuesday the center of Hurricane Carlos was located at latitude 18.2°N and longitude 104.5°W which put it about 55 miles (90 km) south-southwest of Manzanillo, Mexico.  Carlos was moving toward the northwest at 5 m.p.h. (7 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 Watch was in effect for the portion of the coast from Playa Perula to Punta San Telmo, Mexico and a Tropical Storm Warning was in effect for the portion of the coast from Cabo Corrientes to Punta San Telmo, Mexico.

After intensifying on Tuesday afternoon and exhibiting well developed upper level divergence, the structure of Hurricane Carlos degenerated quickly on Tuesday night.  Most of the strong thunderstorms dissipated.  Satellite imagery showed an exposed low level center near the Mexican coast, while the upper level canopy was moving westward away from the low level center.  The decoupling of the upper and low parts of the circulation, usually leads to quick weakening of a hurricane.  The small size of Carlos could allow it to weaken even more quickly than an average hurricane.  The most recent satellite images showed a few thunderstorms forming south of the center of circulation.  However, wind shear caused by an upper level ridge north of Carlos may be too strong to allow for the system to regain its vertical integrity.  Tropical cyclones that are sheared apart sometimes have one chance to redevelop.  The low level center is moving closer to the coast of Mexico and interaction with land may prevent any chance for redevelopment.

If the low level center remains separated from the rest of the system and it does not extend higher into the atmosphere, it will be steered by the winds in the lower levels.  Those winds appear to be taking it north-northwest toward the coast.  Carlos could dissipate quickly if it makes landfall, or the circulation could linger for a day or two if it stays farther offshore.

Very Small Hurricane Carlos Moving Just West of Mexico

Hurricane Carlos has a very small circulation and the tropical storm force winds extend out less than 50 miles (80 km) from the center.  At 8:00 p.m. EDT on Monday the center of Hurricane Carlos was located at latitude 17.2°N and longitude 103.3°W which put it about 90 miles (145 km) southwest of Lazaro Cardenas, Mexico and about 140 miles (225 km) south-southeast of Manzanillo.  Carlos was moving toward the west-northwest at 6 m.p.h. (9 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 989 mb.  A Hurricane Watch and a Tropical Storm Warning is in effect for the portion of the coast from Playa Perula to Punta San Telmo.

The small circulation of Hurricane Carlos continues to move over the Pacific Ocean west of Mexico.  It is moving over water where the Sea Surface Temperature is about 29°C.  An upper level ridge north of the hurricane is generating northeasterly winds that are impinging on the northern side of Carlos.  Those winds are inhibiting upper level divergence from the northern side of Carlos.  The small circulation means than any thunderstorms form near the center and the strongest storms are south of the center.  The small circulation also means that wind shear can have a very big effect on Carlos.  Even moderate winds in the upper levels would be strong enough to disrupt the vertical coherence of the hurricane and blow away the upper part of Carlos.  The vertical wind shear is expected to be modest in the short term, and Carlos is forecast to maintain its intensity for a day or two.  However, it would not take much increase in the wind shear to blow the top off Carlos.

The upper level ridge is expected to continue to steer Carlos toward the west-northwest for 24 to 36 hours.  After that time two scenarios are possible.  In one scenario the upper level ridge weakens and Carlos turns northward and moves very close the coast of Mexico near Cabo Corientes.  In an alternative scenario the ridge maintains its intensity and it steers Carlos toward the west-northwest for the next few days.  A third scenario, which could occur at any time, would happen if wind shear blows the top off of Carlos.  In that case the surface circulation would be steered westward by the lower level flow until it dissipated.  These three possible scenarios make the future track of Carlos very uncertain.

Small Tropical Storm Carlos Moving West of Acapulco

Carlos weakened to a tropical storm as it moved west of Acapulco, Mexico on Sunday.  At 11:00 p.m. EDT on Sunday the center of Tropical Storm Carlos was located at latitude 16.7°N and longitude 101.3°W which put it about 95 miles (150 km) west of Acapulco and about 110 miles (175 km) southeast of Lazaro Cardenas.  Carlos was moving toward the northwest at 6 m.p.h. (9 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 998 mb.  Carlos is a small tropical cyclone.  The tropical storm force winds only extend out about 50 miles (80 km) from the center and it has a Hurricane Size Index (HSI) of 1.7.  The government of Mexico has issued a Hurricane Warning for the portion of the coast that extends from Punta San Telmo to Tecpan de Galeana.  A Hurricane Watch has been issued for the portion of the coast from Playa Perula to Punta San Telmo.

Carlos was nearly stationary for several days and its winds mixed cooler water to the surface.  In addition the circulation pulled in drier air from Mexico as it got closer to the coast.  The combined effects of cooler water and drier resulted in less energy to drive the circulation and Carlos weakened to a tropical storm on Sunday.  Late in the day it started to move toward the northwest and get away from the cooler water.  Carlos is moving over an area where the Sea Surface Temperature (SST) is near 30°C.  Recent satellite images indicate that stronger thunderstorms are forming near the center of circulation.  The flow around Carlos is still pulling in drier air from Mexico and there are fewer thunderstorms in the northern half of the tropical storm.  The small size of Carlos means that it can strengthen or weaken more quickly than a larger storm because there is less mass to accelerate.  The upper level winds over Carlos have lessened and there is not as much vertical wind shear.  If Carlos remains over water, it is likely to intensify back to a hurricane on Monday.

An upper level ridge over Mexico is moving slowly toward the east and it is starting to steer Carlos toward the northwest.  The ridge is expected to continue to steer the tropical storm toward the northwest or west-northwest on Monday.  As Carlos approaches the western end of the ridge is expected to turn more toward the west-northwest.  There is some uncertainty about where the turn will occur.  Guidance from some models have Carlos turning farther east and making a landfall between Manzanillo and Cabo Corientes, while some other models have the tropical storm moving farther west before turning.  Either scenario is plausible and hence, the high degree of uncertainty about the future track of Carlos.

Possible Tropical Development in Western Gulf of Mexico

An area of showers and thunderstorms near the Yucatan Peninsula has shown signs of a cyclonic circulation, although the rotation may be in the middle troposphere and not at the surface.  The formal designation of this system is Invest 91L.  At 2:00 p.m EDT on Saturday the center of Invest 91L was located at latitude 20.0°N and longitude 88.4°W which put it about 100 miles (165 km) southeast of Merida, Mexico and about 760 miles (1220 km) south-southeast of Galveston, Texas.  Invest 91L was moving toward the northwest at 5 m.p.h. (8 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 National Hurricane Center is now giving Invest 91L a 50% chance of developing into a tropical depression or tropical storm in the next five days.  An additional reconnaissance plane has been scheduled to investigate it on Sunday afternoon.

The circulation of Invest 91L is not very well organized.  Almost all of the showers and thunderstorms are occurring in the eastern half of the circulation.  Visible satellite images indicate a possible center of cyclonic rotation over the Yucatan peninsula, but it is not clear if the rotation extends all of the way down to the surface.  Counterclockwise winds around an upper level low over the Gulf of Mexico are generating significant vertical wind shear over Invest 91L.  However, the upper level winds east of the upper low are diverging, which is enhancing rising motion and is supporting the development of the showers and thunderstorms in that area.  The upper level divergence is also causing the surface pressure to decrease slowly, which could lead to the formation of a surface center of low pressure.

When Invest 91L moves into the southern Gulf of Mexico, it will move over water where the Sea Surface Temperature is near 27°C to 28°C.  So, there is sufficient energy in the upper ocean to support the development of a tropical cyclone.  The key factor will be the interaction between the upper low and any surface center that forms.  If the surface center forms too close to the upper low, then vertical wind shear will likely inhibit development and the system will remain fairly weak.  If the surface low develops a little farther southeast of the upper low, then there will be less shear and more upper level divergence.  That could allow for more intensification.

Invest 91L is expected to move with the upper low as the upper low moves northward.  Most guidance from numerical models moves the system toward the north-northwest toward the Upper Texas Coast.  However, there will be above normal uncertainty in the track until a well defined center of circulation forms at the surface.

Interests in the western Gulf of Mexico should monitor the progress of Invest 91L.

Carlos Strengthens to a Hurricane

An eye developed in the center of Carlos and the National Hurricane Center upgraded it to a hurricane.  At 5:00 p.m. EDT on Saturday the center of Hurricane Carlos was located at latitude 15.2°N and longitude 100.0°W which put it about 120 miles (190 km) south of Acapulco, Mexico and about 240 miles (390 km) southeast of Lazaro Cardenas, Mexico.  Carlos was moving toward the north at 2 m.p.h. (4 km/h).  The maximum sustained wind speed was 85 m.p.h. (140 km/h) and there were gusts to 105 m.p.h. (170 km/h).  The minimum surface pressure was 986 mb.  The Hurricane Intensity Index (HII) is 12.7.  The Hurricane Size Index (HSI) is 10.3.  The Hurricane Wind Intensity Size Index (HWISI) is 23.0.  These indices suggest that Carlos is capable of producing regional serious wind damage.  The government of Mexico has issued a Hurricane Warning for the portion of the coast from Lazaro Cardenas to Tucpan de Galeana.  A Hurricane Watch is in effect for the portion of the coast from Punta San Telmo to Lazaro Cardenas.  A Tropical Storm Warning has been issued for the portion of the coast from Tecpan de Galeana to Punta Maldonado.

The circulation near the center of Carlos is more well organized than it was 12 hours ago and an eye is clearly apparent on visible satellite imagery.  The hurricane appears to still be pulling in some drier air from Mexico because there is a gap on the northern side of the eyewall.  However, the drier air is less of a factor than it was on Friday.  Carlos is over water where the Sea Surface Temperature (SST) is near 30°C.  At some point it’s lack of movement will cause its winds to mix cooler water to the surface but that has not happened yet.  An upper level ridge located to the north of Carlos is generating some easterly winds near the top of the hurricane, but upper level divergence has increased since yesterday.  The upper level divergence is pumping out mass, which is allowing the surface pressure to decrease and Carlos to strengthen.  Drier air and modest vertical wind shear will slow the intensification of Carlos, but the hurricane should get stronger in the short term while it remains over warm SSTs.

A combination of the upper level ridge north of Carlos and an upper low over the Gulf of Mexico is creating a zone of weak steering winds near Carlos, which is why it has moved so little.  Later this weekend the upper level low is forecast to move away and the ridge will move northeast of the hurricane.  The change in position will cause Carlos to move toward the northwest.  Most of the guidance from numerical models keep the center of Carlos west of the coast of Mexico, but some models are now bringing it much closer to land.  The change in the guidance prompted the issuance of new watches and warnings for portions of the Mexican coast.

Tropical Storm Carlos Stationary South of Acapulco

Tropical Storm Carlos moved very little on Friday.  At 5:00 p.m. EDT on Friday the center of Tropical Storm Carlos was located at latitude 14.7°N and longitude 100.6°W which put it about 160 miles (255 km) south-southwest of Acapulco and about 250 miles (405 km) south-southeast of Lazaro Cardenas, Mexico.  Carlos was stationary.  The maximum sustained wind speed was 60 m.p.h. (95 km/h) and there were gusts to 70 m.p.h. (115 km/h).  The minimum surface pressure was 997 mb.

The intensity of Carlos changed little on Friday and the organization of the circulation fluctuated during the day.  The core of the circulation exhibited greater organization during the afternoon when more thunderstorms developed near the center.  Carlos remains over water where the Sea Surface Temperature (SST) is near 30°C.  At times it appears as though Carlos may be pulling in some sinking drier air from Mexico, because most of the thunderstorms are developing in the southern portion of the circulation.  An upper level ridge north of Carlos is generating some northeasterly winds that are affecting the outflow on the northern side of the tropical storm.  However, an upper level low over the Gulf of Mexico may be enhancing some upper level divergence on the eastern side of the storm.  If Carlos were to remain stationary for several more days, its winds would mix up cooler water.  Carlos should not have as big an effect on the SSTs as Blanca did when it was stationary, because Carlos is weaker than Blanca was.  The intensity forecast is highly uncertain because the SSTs are favorable for intensification, but drier air and vertical wind shear would tend to inhibit strengthening.  The most likely outcome is modest intensification during the weekend.

The interaction of the upper ridge over Mexico and the upper low over the Gulf of Mexico is creating a zone of weak steering winds near Carlos, which is the reason it has been stationary.  Eventually, during the weekend, the upper ridge is expected to move eastward and begin to steer Carlos toward the northwest.  On its anticipated track the center of Carlos is expected to remain off the coast of Mexico, but it is expected to move parallel to the coast.  Any deviation of the track to the east could bring the center very near the coast of Mexico.

TD Three-E Intensifies and Is Now Tropical Storm Carlos

A tight center of circulation consolidated in Tropical Depression Three-E and it intensified on Thursday.  It is now designated as Tropical Storm Carlos.  At 11:00 p.m. EDT on Thursday the center of Tropical Storm Carlos was located at latitude 14.5°N and longitude 100.4°W which put it about 170 miles (270 km) south of Acapulco, Mexico and about 235 miles (380 km) south-southeast of Zihuatanejo.  Carlos was moving toward the north-northwest at 2 m.p.h. (4 km/h).  The maximum sustained wind speed was 60 m.p.h. (95 km/h) and there were gusts to 70 m.p.h. (115 km/h).  The minimum surface pressure was 997 mb.  The government of Mexico has issued a Tropical Storm Watch for the portion of the coast from Acapulco to Zihuatanejo.

Although a tight circulation developed at the center of Carlos, it is still not fully organized.  Thunderstorms are developing mainly to the south of the core of the circulation.  Some spiral bands are beginning to form in the outer part of Carlos.  However, there are not as many thunderstorms in the northern half of the circulation which may be an indication that some drier air from Mexico could be getting pulled into the circulation.   Carlos is moving over water where the Sea Surface Temperature is near 30°C and there is sufficient energy in the upper ocean to support intensification.  An upper level ridge over Mexico is generating northeasterly winds over the top of Carlos and the vertical wind shear is inhibiting the development of the tropical storm.  An upper level trough moving southward over the Gulf of Mexico could weaken the ridge for a day or two.  That could reduce the wind shear and allow Carlos to intensify into a hurricane.

As the upper level trough weakens the ridge, the steering currents will remain weak and Carlos could move slowly toward the coast of Mexico.  The ridge is forecast to strengthen over the weekend and if that happens it will steer Carlos toward the northwest.  On its anticipated track, Carlos will approach and then move parallel to the coast of Mexico.  Most of the guidance from numerical models keeps Carlos off the coast during the next few days, but it could get close enough to bring some wind to the coast.  That is the reason why the government of Mexico issued a Tropical Storm Watch for a portion of the coast.

Tropical Depression Three-E Forms South of Mexico

A low level circulation in a large area of thunderstorms south of Mexico showed evidence of more organization and the National Hurricane Center classified it as Tropical Depression Three-E on Wednesday.  At 11:00 p.m. EDT on Wednesday the center of Tropical Depression Three-E (TD3E) was located at latitude 12.9°N and longitude 99.7°W which put it about 275 miles (445 km) south of Acapulco, Mexico.  TD3E was moving toward the northwest at 10 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 1003 mb.

The circulation of TD3E is still organizing and there could be multiple smaller centers of circulation rotating around inside a larger, broader center of low pressure.  The tropical depression is moving over water where the Sea Surface Temperature is near 30°C, which means there is plenty of energy in the upper ocean to support intensification.  An upper level high ridge over Mexico is generating modest amounts of vertical wind shear over TD3E.  The wind shear could slow the organization and intensification of the depression, but it should not prevent it.  The rate of intensification could quicken after the circulation becomes more well organized.

The ridge over Mexico is currently steering TD3E toward the northwest.  Guidance from numerical models is inconsistent about the future track of the depression.  Some models predict the ridge over Mexico will weaken and that TD3E will move northward toward the coast.  Other models maintain the ridge and forecast the depression will move northwest and stay west of the coast of Mexico.  The current motion of TD3E may suggest that the latter scenario has a higher probability of being correct, but there is still significant uncertainty about its future track.