A combination of upwelling of cooler water and a possible eyewall replacement weakened Hurricane Blanca on Thursday.  At 11:00 p.m. EDT on Thursday the center of Hurricane Blanca was located at latitude 13.7°N and longitude 105.7°W which put it about 690 (1115 km) miles south-southeast of Cabo San Lucas, Mexico and about 380 (610 km) miles south-southwest of Manzanillo, Mexico.  Blanca was moving toward the north-northwest at 8 m.p.h. (13 km/h).  The maximum sustained wind speed was 100 m.p.h. (160 km/h) and there were gusts to 120 m.p.h. (195 km/h).  The minimum surface pressure was 975 mb.  The Hurricane Intensity Index (HII) was 16.5, the Hurricane Size Index (HSI) was 16.1 and the Hurricane Wind Intensity Size Index was 32.6.

The structure of Hurricane Blanca underwent a significant transformation on Thursday.  After being nearly stationary for approximately three days, the winds of Blanca stirred up the water in the upper ocean and mixed cooler water to the surface.  The cooler water reduced the energy available to drive the circulation of Blanca.  In addition, Blanca may have undergone an eyewall replacement cycle on Wednesday night and Thursday morning.  When a rainband wraps around an existing eyewall, it produces dissipation of the original eyewall.  The result is often a larger hurricane with a bigger eye, which is the appearance of Blanca on satellite imagery.  The combination of cooler water and a possible eyewall replacement changed the structure of the hurricane from a small intense circulation to a weaker and larger circulation.  However, Blanca is still a 100 m.p.h. (160 km/h).  Blanca is moving again and it will start to move away from the region of cooler water.  The upper level winds are relatively light and the environment is favorable for some intensification during the next day or two.  Since Blanca is larger and less well organized, it will respond more slowly to the favorable environment.  As the hurricane nears latitude 20°N, it will start to encounter cooler water and weaken will be likely.

A ridge to the northeast of Blanca and a trough west of Baja California are combining to steer it toward the north-northwest.  That steering pattern is likely to continue for the next several days.  On its anticipated track Blanca would approach the southern portion of Baja California in about three days.  A reconnaissance aircraft is scheduled to investigate the hurricane on Friday.

Hurricane Blanca intensified very rapidly on Wednesday into a Category 4 hurricane on the Saffir-Simpson Scale.  At 5:00 p.m. EDT on Wednesday the center of Hurricane Blanca was located at latitude 12.3°N and longitude 104.7°W which put it about 810 miles (1300 km) south-southeast of Cabo San Lucas, Mexico and about 465 miles (745 km) south of Manzanillo, Mexico.  Blanca drifted slowly southward during the day, but it is essentially stationary.  The maximum sustained wind speed was 140 m.p.h. (220 km/h) and there were gusts to 165 m.p.h. (270 km/h).  The minimum surface pressure was 945 mb.  Blanca had a Hurricane Intensity Index (HII) of 28.3, a Hurricane Size Index (HSI) of 8.6 and a Hurricane Wind Intensity Size Index (HWISI) of 36.9.  Blanca is almost as strong and slightly larger than Hurricane Charley was when it hit southwest Florida in 2004.  At that time Charley had a HII of 29.9, a HSI of 7.7 and a HWISI of 37.6.

Blanca intensified from 75 m.p.h. (120 km/h) to 140 m.p.h. (220 km/h) during the past 24 hours which is a very rapid rate of intensification.  However, it is nowhere near the record for rapid intensification over the Eastern North Pacific.  In 1997 the maximum sustained wind speed in Hurricane Linda increased from 75 m.p.h. (120 km/h) to 175 m.p.h. (290 km/h) in a 24 hour period.  Blanca’s relatively small size means that there is less mass to accelerate in order to increase the wind speed.  It has efficiently extracted energy from the upper ocean and the wind speed in the small inner core increased rapidly today.  It is over water where the Sea Surface Temperature (SST) is near 30°C.  If Blanca were to remain stationary long enough, its winds would mix some cooler water to the surface.  Some subsidence and drier air is approaching the northwestern periphery of Blanca, but that air appears to have not had an effect on the core of the hurricane today.  Upper level winds are light right over the center of Blanca and there is little vertical wind shear over its inner core.  As long as Blanca can extract sufficient energy from the upper ocean, the potential for further intensification exists.  Much of the guidance suggests that Blanca could intensify for another 12 to 24 hours.  However, eyewall replacement cycles can occur in strong hurricanes and cause fluctuations in intensity.  Changes in intensity in small hurricanes can occur rapidly as we have seen today.  Eventually, when Blanca starts to move northward, it will encounter cooler SSTs and more wind shear which will cause it to weaken.

A ridge over Baja California is preventing Blanca from moving toward the north.  The hurricane is in an area where the steering currents are weak, which resulted in a slow southward drift today.  The ridge is forecast to shift to the east during the next several days and it will start to steer Blanca toward the northwest.  On its anticipated track Blanca could approach the southern tip of Baja California late in the weekend.  Because of a possible threat to Baja California a reconnaissance plane has been scheduled to investigate Blanca on Friday.  Blanca will weaken before it approaches that area, but it may still posed a significant risk.

The structure of Tropical Storm Blanca continued to improve on Tuesday and it intensified into a hurricane.  At 5:00 p.m. EDT on Tuesday the center of Hurricane Blanca was located at latitude 13.1°N and longitude 104.6°W which put it about 375 miles (605 km) south-southwest of Zihuatanejo, Mexico and about 410 miles (655 km) south of Manzanillo, Mexico.  Blanca was stationary.  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 960 mb.  The Hurricane Intensity Index (HII) was 10.4, the Hurricane Size Index (HSI) was 5.8 and the Hurricane Wind Intensity Size Index (HWISI) was 16.2.  Since Blanca and Andres both became hurricanes this year, June 2 becomes the earliest date on record by which time two hurricanes formed over the Eastern North Pacific Ocean.  However, it should be noted that the most reliable records only go back to 1971.

Hurricane Blanca is sitting over water where the Sea Surface Temperature (SST) is near 30°C.  It is efficiently extracting energy from the upper ocean and that energy is fueling its intensification.  Spiral bands of thunderstorms are well organized and the strongest storms are near the center of circulation.  The thermodynamic environment is very favorable for further intensification and rapid intensification is possible.  There are a several of factors that could slow the rate of intensification at times.  Upper level outflow from Hurricane Andres, which is about a thousand miles west of Blanca, appears to be generating some vertical wind shear on the northern and western sides of Blanca.  Thunderstorms in Blanca are producing upper level divergence, but some of the divergence may be reduced in the northwestern quadrant of the hurricane.  Andres is slowly spinning down and the wind shear is likely to lessen during the next several days.  A second potential inhibiting factor is the fact that Blanca is not moving much.  The warm water underneath Blanca is relatively deep, but if it sits in one location long enough, its winds will eventually begin  to mix some cooler water to the surface.  For the time being Blanca has sufficient energy in the upper ocean to support further intensification.  Once Blanca starts moving, then it will be over warm SSTs until it approaches latitude 20°N.  Finally, if Blanca gets as strong as some guidance suggest it could, then eyewall replacement cycles also could produce fluctuations in intensity.  As I mentioned above, Blanca is likely to intensify further and it could intensify rapidly at times.

A ridge in the middle levels centered near Baja California is blocking the northward progress of Blanca and the hurricane is in an area where the steering currents are weak.  The ridge is forecast to move slowly eastward toward a position over northern Mexico and Texas.  As the ridge moves eastward it will initially steer Blanca toward the northwest.  In several days the ridge will cause Blanca to turn more toward the north.  On its anticipated track, Blanca could approach the southern tip of Baja California in a few days.  It is too early to know how strong Blanca might be at that time or how much of a risk it might pose to that area.

After an extended period when drier air and wind shear inhibited the organizational processes in Tropical Storm Vance, it has intensified rapidly in recent hours and it is now a hurricane.  At 10:00 a.m. EST on Sunday the center of Hurricane Vance was located at latitude 11.9°N and longitude 107.5°W which put it about 535 miles south-southwest of Manzanillo, Mexico.  Vance was moving toward the northwest at 15 m.p.h.  The maximum sustained wind speed was 80 m.p.h. and the minimum surface pressure was 990 mb.

Vance is moving around the western end of a ridge of high pressure over Mexico.  A large upper level trough west of California will begin to affect Vance as it moves farther north.  The trough is expected to turn Vance toward the northeast early next week.  The track forecast becomes more challenging for the period when Vance could be approaching the coast of Mexico.  Much of the guidance from the numerical models suggests that the upper level winds could be strong enough to separate the upper portion of Vance’s circulation from the lower level rotation.  If that happens, then the middle and upper portions of the circulation could be transported across Mexico, while the surface low gets left behind and meanders southeast of Baja California.

Vance is over water where the Sea Surface Temperature is near 29°C and the upper level winds are relatively light.  So, the period of rapid intensification could continue for another 12-24 hours.  When the upper level trough approaches Vance from the northwest on Monday, the wind shear will increase and Vance will start to weaken and it could weaken quickly.  Even if the low level center of Vance does not make landfall, moisture in the middle and upper portions of the circulation could enhance precipitation over Mexico next week.

Hurricane Simon intensified rapidly on Saturday and it is now a Major Hurricane.  At 5:00 p.m. EDT the center of Hurricane Simon was located at latitude 20.6°N and longitude 115.0°W which put it about 365 miles west-southwest of the southern tip of Baja California and about 495 miles south of Punta Eugenia, Mexico.  Simon was moving toward the west-northwest at 14 m.p.h.  The maximum sustained wind speed was 120 m.p.h. and the minimum surface pressure was 950 mb.

Simon is the 8th hurricane to reach Major Hurricane intensity over the Eastern North Pacific during 2014.  This ties the record for the most Major Hurricanes in one year in that basin, which was set previously in 1983, 1992 and 1993.

Simon is moving around the western edge of a ridge centered over northern Mexico.  It should turn more toward the north on Sunday.  As Simon moves farther north, it will eventually move toward the northeast.  It could approach Baja California by the middle of next week.

Simon may be on the threshold of an eyewall replacement cycle.  If it goes through one of those cycles, there will be some fluctuations in intensity.  When Simon moves west of Baja California it will move over cooler Sea Surface Temperatures and begin to weaken.  Simon is likely to be a weakening tropical cyclone when it nears Baja California.

Tropical Depression 18-E which formed earlier today has intensified into Tropical Storm Rachel.  At 11:00 p.m. EDT on Wednesday the center of Tropical Storm Rachel was located at latitude 15.3°N and longitude 107.4°W which put it about 325 miles southwest of Manzanillo, Mexico and about 550 miles south-southeast of the southern tip of Baja California.  Rachel was moving toward the west at 12 m.p.h.  The maximum sustained wind speed was 40 m.p.h. and the minimum surface pressure was 1004 mb.

A strong upper level ridge over northern Mexico has been producing northeasterly winds and wind shear over the circulation of Rachel.  The wind shear has been the reason why most of the thunderstorms have been located west of the center of circulation.  The northeasterly winds diminished slightly during recent hours and more thunderstorms developed closer to the center.  The improved organization allowed the wind speed at the surface to increase and Rachel became a tropical storm.  The upper level winds could decrease further and some additional intensification is possible.

A ridge in the middle levels is likely to steer Rachel to the west-northwest during the next day or two.  As Rachel moves farther north, it could be affected by a mid-level trough (i.e. a shortwave trough) in the westerly flow in about 72 hours.  If Rachel is strong enough and tall enough, then the mid-level trough could turn Rachel back to the northeast, which could move it toward Baja California.  If Rachel is weaker and the circulation does not extend as high into the atmosphere, then the mid-level trough may not affect the movement of Rachel.  In that case, it would probably continue to move west and dissipate over cooler Sea Surface Temperatures.

Tropical Storm Polo continues to move northwestward parallel to the west coast of Mexico.  At 11:00 p.m. EDT on Thursday the center of Polo was located at latitude 18.4°N and longitude 106.6°W which put it about 150 miles south-southwest of Cabo Corrientes, Mexico and about 375 miles southeast of the southern tip of Baja California.  Polo was moving toward the northwest at 9 m.p.h.  The maximum sustained wind speed was 70 m.p.h. and the minimum surface pressure was 981 mb.

An upper level ridge over northwestern Mexico is producing northeasterly winds that are creating wind shear over Polo.  The wind shear is limiting thunderstorm activity on the northern side of the storm.  It is also possible that Polo is close enough to Mexico that it may be pulling some drier air into the northern half of the circulation.  Both of those factors are inhibiting intensification of Polo.

A high pressure system in the middle levels over Mexico is steering Polo toward the northwest.  The tropical storm is starting to move a little more quickly.  Numerical models are suggesting that the mid-level high will strengthen and eventually turn Polo more toward the west.  Most guidance predicts that Polo will move southwest of Baja California.  However, based on the faster motion the government of Mexico has issued a Tropical Storm Watch for a portion of southern Baja California from Santa Fe to La Paz.  A Tropical Storm Warning remains in effect for a portion of the coast from Punta San Telmo to Playa Perula.  A Tropical Storm Watch continues for the portion of the coast from Playa Perula to Cabo Corrientes.

The circulation around Polo continues to exhibit increasing signs of intensification and it was upgraded to hurricane status on Wednesday night.  Polo is the sixteenth named tropical cyclone to form over the Eastern North Pacific Ocean during 2014 and it is the eleventh to reach hurricane intensity.

At 11:00 p.m. EDT on Wednesday the center of Hurricane Polo was located at latitude 16.4°N and longitude 104.6°W which put it about 180 miles south of Manzanillo, Mexico.  Polo was moving toward the west-northwest at 10 m.p.h.  The maximum sustained wind speed was 75 m.p.h. and the minimum surface pressure was 988 mb.

The movement of Polo has varied as the circulation has tightened around the core and more well defined spiral bands have developed.  In recent hours it has exhibited a more west-northwesterly motion after moving more toward the northwest earlier in the day.  Polo appears to be being steered mostly by an upper level high over Mexico.  The upper level high should steer Polo on a track that is roughly parallel to the west coast of Mexico.  Many of the numerical models are predicting that Polo will pass southwest of Baja California, but as Hurricane Odile showed, it could take a track closer to the coast.

Polo is moving over warm Sea Surface Temperatures and further intensification is likely.  As the organization of the circulation increases and an eye forms, a period of more rapid intensification is possible.

The government of Mexico has issued a Tropical Storm Warning for the portion of the coast from Punta San Telmo to Playa Perula.  A Tropical Storm Watch has been issued for the portion of the coast from Playa Perula to Cabo Corrientes.