Category Archives: Eastern and Central Pacific

TCs between Mexico and Hawaii

Guillermo Intensifies Into a Hurricane

Guillermo intensified rapidly during the past 24 hours and it is now a hurricane.  At 5:00 p.m. EDT on Friday the center of Hurricane Guillermo was located at latitude 12.7°N and longitude 134.8°W which put it about 1430 miles (2300 km) east of Hilo, Hawaii.  Guillermo was moving toward the west-northwest at 18 m.p.h. (30 km/h).  The maximum sustained wind speed was 105 m.p.h. (165 km/h) and there were wind gusts to 125 m.p.h. (205 km/h).  The minimum surface pressure was 970 mb.

Guillermo moved through a very favorable environment of warm Sea Surface Temperatures and little vertical wind shear which allowed it to intensify rapidly from a tropical storm into a hurricane.  An eye was visible earlier today on satellite images, but it is either obscured or has filled with clouds on the most recent images.  The hurricane is moving over water where the Sea Surface Temperature (SST) is near 29°C.  The upper level winds are light, but the rapid movement toward the west-northwest may be generating some vertical wind shear.  If Guillermo moves more slowly, it has about another 24 hours before it starts to move over cooler SSTs.  Once Guillermo gets west of longitude 140°W, it will gradually move over cooler SSTs.  As it moves farther north, it will also get closer to stronger upper level winds blowing from the west.  The combination of cooler SSTs and more vertical wind shear are likely to weaken Guillermo as it approaches Hawaii.

A subtropical ridge north of Guillermo is steering the hurricane toward the west-northwest and that steering is likely to continue for several more days,  In a few days a trough approaching from the west will turn Guillermo toward the northwest.  On its anticipated track Guillermo could approach Hawaii in about five days.  The higher probability is that a weaker Guillermo will move north of Hawaii, but the guidance from numerical models has been changing today.

Tropical Storm Guillermo Forms East- Southeast of Hawaii

An area of low pressure organized on Wednesday well east-southeast of Hawaii and it has been classified as Tropical Storm Guillermo.  At 5:00 a.m. EDT on Thursday the center of Tropical Storm Guillermo was located at latitude 8.5°N and longitude 126.3°W which put it about 2070 miles (3340 km) east-southeast of Hilo, Hawaii and about 1475 miles (2370 km) southwest of the southern tip of Baja California.  Guillermo was moving toward the northwest at 15 m.p.h. (24 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.

Guillermo formed at an unusually low latitude over the eastern North Pacific.  It is over an area where the Sea Surface Temperatures (SSTs) are near 29°C.  The upper level winds are light over the circulation and there is not much vertical wind shear.  Guillermo will be moving through an environment favorable for intensification during the next two or three days and a period of rapid intensification will be possible when it nears hurricane intensity.  Guillermo will move over cooler SSTs when it gets closer to Hawaii and the wind shear may also increase.

A subtropical ridge north of Guillermo is steering the tropical storm toward the northwest and the ridge is expected to continue to steer the tropical storm toward the west-northwest during the next 48 to 72 hours.  Later in the weekend an upper level trough approaching from the west could turn Guillermo more toward the northwest.

Tropical Storm Felicia Forms Southwest of Baja California

A center of circulation finally developed in an area of thunderstorms southwest of Baja California and the system has been designated as Tropical Storm Felicia.  At 11:00 a.m. EDT on Thursday the center of Tropical Storm Felicia was located at latitude 19.1°N and longitude 114.9°W which put it about 415 miles (670 km) southwest of the southern tip of Baja California.  The maximum sustained wind speed was 40 m.p.h. (60 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 1004 mb.

Felicia is not a particularly well organized tropical storm.  Most of the thunderstorms are forming in the southern half of the circulation and it does not have many spiral bands.  Recent satellite images seem to indicate that upper level divergence is beginning to occur.  Felicia is over water where the Sea Surface Temperature (SST) is near 27°C and the upper level winds do not appear to be too strong.  The potential for some intensification will exist for about another 24 hours.  In a day or so, Felicia will start to move over cooler SSTs and it will likely weaken by the weekend.

A subtropical ridge is steering Felicia toward the northwest and that general steering pattern is expected to continue as long as the vertical integrity of the circulation remains intact.  When Felicia moves over cooler SSTs, the height of the circulation will decrease and the storm will be steered by winds in the lower levels.  Those winds are expected to turn Felicia more toward the west in a day or two.  Felicia poses no threat to land at this time.

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.

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.