Category Archives: Eastern and Central Pacific

TCs between Mexico and Hawaii

Olaf Becomes a Cat. 4 Hurricane

Hurricane Olaf intensified rapidly on Monday and it reached Category 4 on the Saffir-Simpson Scale.  At 11:00 p.m. EDT on Monday the center of Hurricane Olaf was located at latitude 10.1°N and longitude 139.5°W which put it about 1235 miles (1985 km) east-southeast of Hilo, Hawaii.  Olaf was moving toward the west at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 140 m.p.h. (220 km/h) and there were wind gusts to 165 m.p.h. (270 km/h).  The minimum surface pressure was 949 mb.

Olaf is a small but well organized hurricane.  The core is very symmetrical.  Hurricane Olaf has a clear eye with a diameter of about 12 miles (19 km/h) and the eye is surrounded by a ring of strong thunderstorms.  Several spiral rainbands are rotating around the inner core of the hurricane.  Upper level outflow channels to the northeast and southwest of Olaf are carrying mass away from the center of circulation, which is allowing the surface pressure to decrease.

Hurricane Olaf is moving just south of a band of stronger upper level westerly winds.  It is in an area of modest vertical wind shear.  The ocean beneath Hurricane Olaf has Sea Surface Temperatures  near 29°C.  The compact structure of Olaf allowed the hurricane to efficiently convert energy it extracted from the ocean to kinetic energy associated with higher wind speeds.  Olaf could remain in a favorable environment for another day or two, which may allow for further intensification.  However, if eyewall replacement cycles begin to occur, they will cause fluctuations in the intensity of Hurricane Olaf.

A subtropical ridge north of Olaf is steering the hurricane toward the west and that general steering motion is expected to continue for another day or two.  The western end of the subtropical ridge is expected to weaken later this week and that should allow Olaf to turn toward the north.  On its anticipated track, Olaf would turn toward the north before it reaches the Hawaiian Islands.

Olaf Becomes a Hurricane Between Baja and Hawaii

The core of the circulation of Olaf consolidated on Sunday and the National Hurricane Center upgraded it to a hurricane.  At 11:00 a.m. EDT on Sunday the center of Hurricane Olaf was located at latitude 9.5°N and longitude 133.2°W which put it about 1620 miles (2610 km) east-southeast of Hilo, Hawaii.  Olaf was moving toward the west at 12 m.p.h. (19 km/h).  The maximum sustained wind speed was 80 m.p.h. (130 km/h) and there were wind gusts to 95 m.p.h. (155 km/h).  The minimum surface pressure was 989 mb.

The circulation of Hurricane Olaf consists of a small core of thunderstorms around the center of circulation and a primary rainband that spirals around the western and southern sides of the hurricane.  The core of thunderstorms is producing some upper level divergence, but upper level winds are inhibiting the outflow on the western side of the center.

Hurricane Olaf is moving over water where the Sea Surface Temperature is near 30°C and there is plenty of energy in the upper ocean to support intensification.  However, an upper level trough north of Olaf is producing westerly winds which are blowing over the top of the hurricane.  The upper level winds are blocking upper level outflow on the western side of Olaf and the vertical wind shear is inhibiting the intensification of Olaf.  If the wind shear decreases, then further intensification will be possible.

A subtropical ridge is steering Hurricane Olaf toward the west and that general motion is expected to continue for another day or two.  When Olaf reaches the western end of the ridge, it will start to turn more toward the north.

Tropical Storm Nora Moves Into the Central Pacific

Tropical Storm Nora moved west of longitude 140°W on Sunday which meant that it officially crossed from the Eastern North Pacific into the Central North Pacific Ocean.  At 11:00 p.m. EDT on Sunday the center of Tropical Storm Nora was located at latitude 13.5°N and longitude 143.8°W which put it about 860 miles (1385 km) east-southeast of Hilo, Hawaii.  Nora was moving toward the west-northwest at 9 m.p.h. (15 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 m.p.h.).  The minimum surface pressure was 993 mb.

Nora is a small tropical storm.  Wind to tropical storm force only extend out about 70 miles (110 km) from the center of circulation.  Most of the stronger thunderstorms are located northwest of the center of circulation and there is not much deep convection in the other parts of Nora.  Although Nora is over water where the Sea Surface Temperature is near 29°C, southerly winds in the upper levels appear to be causing vertical wind shear.  The wind shear is likely to increase as an upper level trough north of Hawaii gets closer to Nora.

Tropical Storm Nora is nearing the western end of a subtropical ridge which has been steering it toward the west.  If the vertical structure of Nora remains intact, the tropical storm should turn toward the north during the next day or two.  After that time the upper level trough north of Hawaii could sweep Nora toward the northeast.  An alternate and possibly more likely scenario, given the small size of Tropical Storm Nora, is that the vertical wind shear blows the upper portion of the circulation north of the surface circulation.  If that happens, then the surface circulation will be steered westward until it dissipates by the winds in the lower atmosphere.

Tropical Storm Nora Form Far East of Hawaii

Another Tropical Cyclone has formed over the Eastern North Pacific Ocean well east of Hawaii and the National Hurricane Center has upgraded Tropical Depression 18-E to Tropical Storm Nora.  At 11:00 p.m. EDT on Friday the center of Tropical Storm Nora was located at latitude 11.3°N and longitude 135.1°W which put it about 1470 miles (2365 km) east-southeast of South Point Hawaii.  Nora was moving toward the west at 16 m.p.h. (26 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 1006 mb.

The circulation inside Tropical Storm Nora is still in the process of organizing.  There is one primary rainband that wraps around the western and southern side of the tropical storm.  More thunderstorms are forming near the center, but a clearly defined core of convection has not yet developed.  The storms close to the center of circulation are producing more upper level divergence which is pumping out mass.

Tropical Storm Nora is in an environment that favors intensification,   The Sea Surface Temperature is warmer than 29°C,  The upper level winds are light and there is not much upper level divergence.  Nora is expected to intensify gradually into a hurricane.  Once a tight, well organized inner core develops, it could intensify more quickly.

A subtropical ridge north of Nora is steering the tropical storm westward.  That general steering pattern is expected to continue for another day or two.  When Nora reaches the western end of the subtropical ridge, it is expected to turn toward the north.

Oho Becomes a Hurricane Southeast of Hawaii

The circulation around Tropical Storm Oho became much more organized on Tuesday and it intensified into a hurricane.  At 5:00 p.m. EDT on Tuesday the center of Hurricane Oho was located at latitude 16.6°N and longitude 150.2°W which put it about 385 miles (620 km) east-southeast of Hilo, Hawaii.  Oho was moving toward the northeast at 18 m.p.h. (30 km/h).  The maximum sustained wind speed was 85 m.p.h. (140 km/h) and there were wind gusts to 100 m.p.h. (160 km/h).  The minimum surface pressure was 975 mb.

A primary rainband wrapped tightly around the center of circulation and created a banded eye feature.  In addition other rainbands developed around the core of the circulation and Oho looks much more like a tropical cyclone today.  Thunderstorms near the center of circulation are generating upper level divergence, especially northeast of the center.  The upper level divergence caused the surface pressure to decrease and the wind speeds to increase.

Hurricane Oho is moving over water where the Sea Surface Temperature (SST) is near 28°C.  The upper level winds are currently fairly light and there is not much vertical wind shear.  The conditions are favorable for intensification and Oho could get stronger during the next 24 hours.  After that time Oho will move over cooler SSTs and the vertical wind shear will increase.  Oho should start to weaken and begin a transition to an an extratropical cyclone.

A large upper level trough north of Hawaii will steer Hurricane Oho toward the northeast during the next few days.  On its anticipated track Oho will pass about 400 miles east of Hawaii.  The extratropical stage of Hurricane Oho could approach the Pacific Northwest in three or four days.

Tropical Storm Oho Passing Southeast of Hawaii

Tropical Storm Oho moved slowly southeast of Hawaii on Monday.  At 11:00 p.m. EDT on Monday the center of Tropical Storm Oho was located at latitude 15.0°N and longitude 153.6°W which put it about 340 miles (545 km) south-southeast of Hilo, Hawaii.  Oho was moving toward the northeast at 6 m.p.h. (10 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 984 mb.

Tropical Storm Oho is only partially organized.  A partial eyewall wrapped around the western and southern sides of the center of circulation.  However, most of the stronger thunderstorms are located southwest of the center.  A weak upper level ridge south of Hawaii appears to be generating some northeasterly winds over the top of Oho, which is causing some vertical wind shear.  The wind shear is inhibiting the organization of the circulation of the tropical storm.

Tropical Storm Oho is over water where the Sea Surface Temperature (SST) is near 28.5°C.  The wind shear could decrease on Tuesday and that could allow Oho to increase to hurricane intensity.  Oho will move northward over cooler SSTs later this week.  A combination of cooler water and more vertical wind shear will cause Oho to weaken and make a transition to an extratropical cyclone.

A large upper level trough northwest of Hawaii is expected to move eastward and begin to steer Oho toward the northeast.  On its expected track, Oho will pass southeast of Hawaii.  The extratropical cyclone that is currently Tropical Storm Oho could be approaching the west coast of the U.S. by the weekend.

Recon Finds Marty a Hurricane, Mexico Issues Warnings

A reconnaissance plane investigated Marty on Monday afternoon and the data showed that Marty was a hurricane.  At 5:00 p.m. EDT on Monday the center of Hurricane Marty was located at latitude 16.7°N and longitude 102.1°W which put it about 75 miles (125 km) south-southwest of Zihuatanejo, Mexico.  Marty was moving toward the northeast at 6 m.p.h. (10 km/h).  The maximum sustained wind speed was 80 m.p.h. (130 km/h) and there were wind gusts to 95 m.p.h. (155 km/h).  The minimum surface pressure was 986 mb.

The government of Mexico has issued a Hurricane Warning for the portion of the coast from Tecpan de Galeana to Lazaro Cardenas.  A Tropical Storm Warning has been issued for the coast from Tecpan de Galeana to Acapulco.  A Tropical Storm Watch has been issued for the portion of the coast from Lazaro Cardenas to Punta San Telmo.

Although an upper level trough over Mexico has been producing southwesterly flow and causing moderate vertical wind shear over Marty, the vertical integrity of the circulation has been maintained.  So, instead of blowing the top off the circulation, the southwesterly winds have pushed the entire circulation toward the northeast.  As Marty moved over water where the Sea Surface Temperature was near 30°C, it extracted enough energy from the water to intensify into a hurricane.  The southwesterly winds inhibited upper level divergence on the western side of the circulation, but the upper level divergence east of Marty pumped out mass and the pressure decreased.

The environment is not favorable for much more intensification.  The upper level trough is expected to continue to cause vertical wind shear.  In addition, Marty is close enough to the coast of Mexico that the hurricane will begin to pull in some drier air from land.  Marty could intensify a little more, but it is likely to weaken on Tuesday.  If Marty makes landfall, it will weaken quickly.

The upper level trough is pushing Marty northeastward toward the coast of Mexico.  Unless the shear blows the upper part of the circulation away from the lower portion, it will continue to move toward the coast.  Marty could make landfall in 12 to 24 hours, which is why the government of Mexico issued warnings for the coast.  Hurricane Marty could bring strong winds and locally heavy rainfall when it moves inland.

Marty Intensifies and Mexico Issues a Tropical Storm Watch

Tropical Storm Marty intensified on Sunday and the government of Mexico issued a Tropical Storm Watch for a portion of the west coast.  At 2:00 p.m. EDT on Sunday the center of Tropical Storm Marty was located at latitude 15.0°N and longitude 102.8°W which put it about 235 miles (380 km) southwest of Acapulco, Mexico.  Marty was moving toward the north-northeast at 6 m.p.h.  The maximum sustained wind speed was 60 m.p.h. (95 km/h) and there were wind gusts to 75 m.p.h. (120 km/h).  The minimum surface pressure was 997 mb.  A Tropical Storm Watch has been issued for the portion of the coast from Acapulco to Lazaro Cardenas, Mexico.

The structure of Tropical Storm Marty improved on Sunday morning.  A long rainband stretched around the southern and eastern sides of the circulation and more thunderstorms developed near the center or circulation.  Marty is over water where the Sea Surface Temperature (SST) is near 30°C, which means there is a lot of energy in the upper ocean.  However, an upper level trough extends from the western Gulf of Mexico across northern Mexico.  The upper level trough is causing westerly winds, which could already be producing vertical wind shear over the northern half of the circulation of Tropical Storm Marty.  Very warm SSTs mean that the potential for intensification exists, but the vertical wind shear will limit how much intensification actually occurs.  If the upper level winds get stronger, they could shear the top half of the circulation away from the bottom half and cause Marty to dissipate.

The upper level trough is beginning to steer Marty toward the north-northeast and the tropical storm is likely to move in that direction over the short term.  The ultimate track of Marty will be determined by the vertical integrity of the circulation and the strength of the vertical wind shear.  If the wind shear is not too strong and the upper and lower portions of the circulation remain together, then the trough will steer all of Marty toward the northeast.  In that case it could make landfall on the Mexican coast in several days.  However, if the vertical wind shear blows then top off of the circulation, then the upper level portion will move northeast toward Mexico, while the lower part of the tropical storm is left behind.  The upper half of the circulation could still bring heavy rain and the potential for floods to parts of Mexico, even if the surface circulation does not make landfall.

Shear Hits Tropical Storm Niala and It Turns West

After intensifying earlier on Saturday, vertical wind shear began to affect Tropical Storm Niala and it turned westward.  At 11:00 p.m. EDT on Saturday the center of Tropical Storm Niala was located near latitude 16.9°N and longitude 152.8°W which put it about 245 miles (395 km) southeast of Hilo, Hawaii.  Niala was moving toward the west at 8 m.p.h. (13 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 992 mb.  A Tropical Storm Watch remains in effect for Hawaii County.

A large upper level trough centered northeast of Hawaii is causing southwesterly winds that are blowing over Tropical Storm Niala.  The wind shear is blowing the tops off the thunderstorms that try to form near the center of circulation.  As a result the low level circulation is exposed on satellite imagery.  The effect of the wind shear will be to weaken Niala even though it is over warm Sea Surface Temperatures.

Since there are not tall thunderstorms near the center of circulation, it is being steered toward the west by winds lower in the atmosphere.  A general westerly motion is expected for the next several days and Tropical Storm Niala is likely to pass south of Hawaii.

Niala Prompts Tropical Storm Watch for Hawaii

Tropical Storm Niala organized quickly southeast of Hawaii on Friday and the Central Pacific Hurricane Center issued a Tropical Storm Watch for Hawaii County.  At 5:00 p.m. EDT on Friday the center of Tropical Storm Niala was located at latitude 15.7°N and longitude 150.4°W which put it about 415 miles (665 km) southeast of Hilo, Hawaii.  Niala was moving toward the northwest at 7 m.p.h. (11km/h).   The maximum sustained wind speed was 45 m.p.h. (70 km/h) and there were wind gusts to 60 m.p.h. (95 km/h).  The minimum surface pressure was 1001 mb.

The circulation inside Niala consolidated quickly around the core of the tropical storm on Friday.  A primary rainband wrapped around the eastern and northern side of the circulation creating a small eyelike feature at the center of circulation.  At least three additional rainbands formed in the eastern half of the tropical storm.  There are fewer thunderstorms in the western half of the circulation which could indicated the presence of drier, more stable air in that part of Niala.

Niala is over water where the Sea Surface Temperatures are nearly 29°C.  The upper level winds are not too strong and the thunderstorms around the core of the circulation are generating upper level divergence,  Niala could strenthen during the next day or so.  A large upper level trough extends from northeast of Hawaii to the islands.  As Niala moves toward the northwest, it will start to move under strong southwesterly winds on the eastern side of the trough.  Those winds will create strong vertical wind shear and Niala will weaken as it approaches Hawaii.

A subtropical ridge is steering Niala toward the northwest and that general motion is expected to continue for another 24 hours.  When the wind shear weakens Niala, the circulation will not extend as high into the atmosphere.  After that time the winds lower in the atmosphere will steer the weakening Niala toward the west.