Typhoon Nolo Passes North of Wake Island

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Typhoon Nolo passed north of Wake Island on Tuesday evening.  At 11:00 p.m. EDT on Tuesday the center of Typhoon Nolo was located at latitude 25.5°N and longitude 162.9°E which put the center about 445 miles (720 km) north of Wake Island.  Nolo was moving toward the west at 25 m.p.h. (40 km/h).  The maximum sustained wind speed was 85 m.p.h. (135 km/h) and there were wind gusts to 105 m.p.h. (165 km/h).  The minimum surface pressure was 977 mb.

Typhoon Nolo weakened on Tuesday.  The eye was no longer visible at the center of Nolo’s circulation.  The distribution of thunderstorms in Typhoon Nolo became more asymmetrical on Tuesday.  Thunderstorms were still occurring in bands in the southern and eastern parts of Nolo’s circulation.  Bands in the northern and western parts of Typhoon Nolo consisted primarily of showers and lower clouds.  Storms near the center of Nolo generated less upper level divergence that pumped less mass away from the typhoon.  The removal of mass in the upper levels was less than the convergence of mass in the lower levels of the atmosphere.  So, the surface pressure increased on Tuesday.

The circulation around Typhoon Nolo was still large.  Winds to typhoon force extended out 75 miles (120 km) from the center of Nolo’s circulation.  Winds to tropical storm force extended out 205 miles (335 km) from the center of Typhoon Nolo.

Typhoon Nolo will move through an environment that will be unfavorable for intensification during the next 24 hours.  Nolo will move over water where the Sea Surface Temperatures are near 28°C.  It will move under the southern part of an upper level ridge that is over the Western North Pacific Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Nolo’s circulation.  Those winds will cause moderate vertical wind shear.  Typhoon Nolo will continue to weaken gradually on Wednesday because of the moderate vertical wind shear.

Typhoon Nolo will move around the southern side of a high pressure system that is over the Western North Pacific Ocean.  The high pressure system will steer Nolo toward the west during the next 24 hours.  On its anticipated track, Typhoon Nolo will move northwest of Wake Island on Wednesday.

Elsewhere over the Western North Pacific Ocean, Typhoon Choi-wan was making a transition to a strong extratropical cyclone east of Japan and Tropical Storm Koguma was gradually intensifying south of Wake Island.

At 5:00 p.m. EDT on Tuesday the center of Typhoon Choi-wan was located at latitude 37.9°N and longitude 151.3°E which put the center about 530 miles (855 km) east-southeast of Misawa, Japan.  Choi-wan was moving toward the northeast at 35 m.p.h. (55 km/h).  The maximum sustained wind speed was 85 m.p.h. (135 km/h) and there were wind gusts to 105 m.p.h. (165 km/h).  The minimum surface pressure was 959 mb.

At 11:00 p.m. EDT on Tuesday the center of Tropical Storm Koguma was located at latitude 15.5°N and longitude 163.6°E which put the center about 325 miles (525 km) south-southwest of Wake Island.  Koguma was moving toward the northwest at 11 m.p.h. (17 km/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 996 mb.

Tropical Depression Forms over Southwest Gulf of Mexico

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Tropical Depression Nine formed over the southwestern Gulf of Mexico on Tuesday afternoon.  At 5:00 p.m. EDT on Tuesday the center of Tropical Depression Nine was located at latitude 22.1°N and longitude 95.6°W which put the center about 380 miles (615 km) west of Progreso, Mexico.  The tropical depression was moving toward the east 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. (75 km/h).  The minimum surface pressure was 1007 mb.

A distinct low level center of circulation formed within a cluster of thunderstorms that was over the southwestern Gulf of Mexico and the U.S. National Hurricane Center designated the system as Tropical Depression Nine.

New thunderstorms were forming near the center of Tropical Depression Nine.  Thunderstorms were also developing in bands that were revolving around the center of the tropical depression.  Storms near the center of the depression started to generate upper level divergence that pumped mass away from the tropical depression.  The removal of mass caused the surface pressure to start to decrease.

Tropical Depression Nine will move through an environment that will be favorable for intensification during the next 24 hours.  The tropical depression will move over water where the Sea Surface Temperatures are near 30°C.  It will move under the western part of an upper level ridge that is over the Gulf of Mexico.  The upper level ridge will produce southerly winds that will blow toward the top of the tropical depression.  Those winds will cause some vertical wind wind shear.  The vertical wind shear will inhibit intensification, but the wind shear will not be enough to prevent that intensification.  Tropical Depression Nine will intensify to a tropical storm during the next 24 hours.  It could strengthen to a hurricane later this week.

An upper level trough over the eastern U.S. and the Gulf of Mexico will steer Tropical Depression Nine toward the east during the next 24 hours.  On its anticipated track, Tropical Depression Nine will move closer to the northwestern part of the Yucatan Peninsula.  A different upper level trough approaching from the west will start to steer the tropical depression toward the north later this week.

Typhoon Nolo Moves Northeast of Wake Island

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Typhoon Nolo moved northeast of Wake Island on Monday evening.  At 11:00 p.m. EDT on Monday the center of Typhoon Nolo was located at latitude 25.7°N and longitude 172.0°E which put the center about 600 miles (970 km) northeast of Wake Island.  Nolo was moving toward the west at 17 m.p.h. (28 km/h).  The maximum sustained wind speed was 120 m.p.h. (195 km/h) and there were wind gusts to 150 m.p.h. (240 km/h).  The minimum surface pressure was 955 mb.

Typhoon Nolo did not change much on Monday.  A circular eye with a diameter of 30 miles (50 km) was at the center of Nolo’s circulation.  The eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the center of Typhoon Nolo.  Storms near the center of Nolo generated upper level divergence that pumped mass away from the typhoon.  The removal of mass in the upper levels was nearly equal to the convergence of mass in the lower levels of the atmosphere.  So, the surface pressure did not change much on Monday.

The distribution of wind speeds around Typhoon Nolo was fairly symmetrical.  Winds to typhoon force extended out 50 miles (80 km) from the center of Nolo’s circulation.  Winds to tropical storm force extended out 155 miles (250 km) from the center of Typhoon Nolo.

The Hurricane Intensity Index (HII) for Typhoon Nolo is 22.1.  The Hurricane Size Index (HSI) is 16.1 and the Hurricane Wind Intensity Size Index (HWISI) is 38.2.  Typhoon Nolo is similar in size and intensity to Hurricane Milton, when Milton hit Florida in 2024.

Typhoon Nolo will move through an environment that will be somewhat unfavorable for intensification during the next 24 hours.  Nolo will move over water where the Sea Surface Temperatures are near 28°C.  It will move under the southern part of an upper level ridge that is over the Western North Pacific Ocean.  The upper level ridge will produce northeasterly winds that will blow toward the top of Nolo’s circulation.  Those winds will cause moderate vertical wind shear.  Typhoon Nolo is likely to weaken gradually on Tuesday because of the moderate vertical wind shear.

Typhoon Nolo will move around the southern side of a high pressure system that is over the Western North Pacific Ocean.  The high pressure system will steer Nolo toward the west during the next 24 hours.  On its anticipated track, Typhoon Nolo will pass north of Wake Island on Tuesday.

Elsewhere over the Western North Pacific Ocean, Typhoon Choi-wan weakened gradually northeast of Iwo To and Tropical Storm Koguma strengthened slowly north of Kwajalein.

At 11:00 p.m. EDT on Monday the center of Typhoon Choi-wan was located at latitude 30.8°N and longitude 146.3°E which put the center about 440 miles (710 km) northeast of Iwo To.  Choi-wan was moving toward the north at 16 m.p.h. (26 km/h).  The maximum sustained wind speed was 110 m.p.h. (175 km/h) and there were wind gusts to 130 m.p.h. (210 km/h).  The minimum surface pressure was 945 mb.

At 11:00 p.m. EDT on Monday the center of Tropical Storm Koguma was located at latitude 13.2°N and longitude 166.7°E which put the center about 295 miles (475 km) north of Kwajalein. Koguma was moving toward the northwest at 11 m.p.h. (17 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 995 mb.

Hurricane Rachel Churns West

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Hurricane Rachel churned westward over the Eastern North Pacific Ocean southwest of Baja California on Monday evening.  At 11:00 p.m. EDT on Monday the center of Hurricane Rachel was located at latitude 20.4°N and longitude 117.9°W which put the center about 540 miles (870 km) west-southwest of the southern tip of Baja California.  Rachel was moving toward the west at 9 m.p.h. (15 km/h).  The maximum sustained wind speed was 90 m.p.h. (145 km/h) and there were wind gusts to 105 m.p.h. (165 km/h).  The minimum surface pressure was 973 mb.

A large circular eye with a diameter of 60 miles (96 km) was at the center of Hurricane Rachel.

The eye was surrounded by a broken ring of thunderstorms and the strongest winds were occurring in that ring of storms.  Thunderstorms were occurring in bands in the eastern and southern part of Rachel’s circulation.  Bands in the western and northern parts of Hurricane Rachel consisted primarily of showers and lower clouds.  Storms near the center of Rachel still generated upper level divergence that pumped mass away from the hurricane.  However, the removal of mass in the upper levels was less than the convergence of mass in the lower levels of the atmosphere.  So, the surface pressure increased slowly on Monday.

The distribution of wind speeds in Hurricane Rachel did not change much on Monday.  Winds to hurricane force extended out 40 miles (65 km) from the center of Rachel’s circulation.  Winds to tropical storm force extended out 140 miles (225 km) from the center of Hurricane Rachel.

Hurricane Rachel will move through an environment that will be unfavorable for intensification during the next 24 hours.  Rachel will move over water where the Sea Surface Temperatures are near 26°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  However, Rachel will continue to move through a mass of drier air that is west of Baja California.  Hurricane Rachel is likely to continue to weaken gradually on Tuesday because of the effects of the drier air.

Hurricane Rachel will move around the southern side of a high pressure system that is over the Eastern North Pacific Ocean.  The high pressure system will steer Rachel toward the west during the next 24 hours. On its anticipated track, Hurricane Rachel will continue to move farther away from Baja California.

Tropical Development Likely over Southwest Gulf of Mexico

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A tropical depression or tropical storm is likely to develop over the southwestern Gulf of Mexico later this week.  The U.S. National Hurricane Center is indicating the probability is 70% that a tropical depression or a tropical storm will form over the southwestern Gulf of Mexico later this week.

A trough of low pressure is currently over the southwestern Gulf of Mexico in the lower levels of the atmosphere.

Scattered showers and thunderstorms are occurring in the trough of low pressure.  However, there is no well defined center of circulation in the trough of low pressure at the current time.

The trough of low pressure will be in an environment that will be favorable for the formation of a tropical depression or a tropical storm during the next few days.  The trough of low pressure will be over water where the Sea Surface Temperatures are near 30°C.  Ir will be under the western part of an upper level ridge that is over the Gulf of Mexico.  The upper level ridge will produce southerly winds that will blow across the top of the surface trough.  Those winds will cause some vertical wind wind shear.  The vertical wind shear will inhibit the formation of a tropical depression or a tropical storm, but the wind shear may not be enough to prevent that formation.

A center of circulation at the surface is likely to organize gradually over the southwestern Gulf of Mexico during the next few days.  The U.S. National Hurricane Center has tentatively tasked a reconnaissance mission to investigate the system on Wednesday afternoon, if necessary.

Hurricane Rachel Still South of Baja California

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Hurricane Rachel was still spinning over the Eastern North Pacific Ocean south of Baja California on Sunday evening.  At 11:00 p.m. EDT on Sunday the center of Hurricane Rachel was located at latitude 20.2°N and longitude 114.8°W which put the center about 365 miles (590 km) west-southwest of the southern tip of Baja California.  Rachel was moving toward the west-northwest at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 100 m.p.h. (160 km/h) and there were wind gusts to 120 m.p.h. (195 km/h).  The minimum surface pressure was 967 mb.

Although Hurricane Rachel strengthened earlier on Sunday, Rachel appeared to be weakening again on Sunday.  Hurricane Rachel was moving into a large mass of drier air.  The drier air caused many of the thunderstorms in the northern side of Rachel’s circulation to dissipate.  Thunderstorms were still occurring in bands in the southern half of Hurricane Rachel.  Storms near the center of Rachel still generated upper level divergence that pumped mass away from the hurricane.  However, the removal of mass in the upper levels was less than the convergence of mass in the lower levels of the atmosphere.  So, the surface pressure started to increase again.

The distribution of wind speeds in Hurricane Rachel was still fairly symmetrical on Sunday evening.  Winds to hurricane force extended out 40 miles (65 km) from the center of Rachel’s circulation.  Winds to tropical storm force extended out 140 miles (225 km) from the center of Hurricane Rachel.

Hurricane Rachel will move through an environment that will be unfavorable for intensification during the next 24 hours.  Rachel will move over water where the Sea Surface Temperatures are near 27°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  However, Rachel will continue to move through the mass of drier air.  Hurricane Rachel is likely to weaken on Monday because of the effects of the drier air.

Hurricane Rachel will move around the southern side of a high pressure system that is over the Eastern North Pacific Ocean.  The high pressure system will steer Rachel toward the west during the next 24 hours.  On its anticipated track, Hurricane Rachel will move farther away from Baja California.

Typhoon Choi-wan Passes East of Iwo To

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Typhoon Choi-wan passed east of Iwo To on Sunday.  At 11:00 p.m. EDT on Sunday the center of Typhoon Choi-wan was located at latitude 25.7°N and longitude 146.4°E which put the center about 325 miles (525 km) east of Iwo To.  Choi-wan was moving toward the northwest at 12 m.p.h. (19 km/h).  The maximum sustained wind speed was 150 m.p.h. (240 km/h) and there were wind gusts to 185 m.p.h. (295 km/h).  The minimum surface pressure was 916 mb.

Typhoon Choi-wan intensified to the equivalent of a Category 4 hurricane on the Saffir-Simpson Scale on Sunday.  An eyewall replacement cycle appeared to be starting in Typhoon Choi-wan.  A circular eye with a diameter of 20 miles (32 km) was at the center of Choi-wan’s circulation.  The eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that ring of storms.  The inner end of a rainband wrapped around the existing eye and eyewall.  A larger outer eyewall appeared to be forming around the existing eye and eyewall.  Bands of showers and thunderstorms were revolving around the core of Typhoon Choi-wan.  Storms near the core of Choi-wan generated upper level divergence that pumped mass away from the typhoon.  The removal of mass caused the surface pressure to decrease.

The circulation around Typhoon Choi-wan was large.  Winds to typhoon force extended out 80 miles (130 km) from the center of Choi-wan’s circulation.  Winds to tropical storm force extended out 355 miles (575 km) from the center of Typhoon Choi-wan.

The Hurricane Intensity Index (HII) for Typhoon Choi-wan is 31.6.  The Hurricane Size Index (HSI) is 27.4 and the Hurricane Wind Intensity Size Index (HWISI) is 59.0.  Typhoon Choi-wan is similar in intensity to Hurricane Laura when Laura hit Southwest Louisiana in 2020.  Typhoon Choi-wan is much larger than Hurricane Laura was.

Typhoon Choi-wan will move through an environment that will be favorable for intensification during the next 24 hours.  Choi-wan will move over water where the Sea Surface Temperatures are near 28°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Even though Typhoon Choi-wan will move through a favorable environment, Choi-wan is likely to weaken during the next 24 hours because of the eyewall replacement cycle.

Typhoon Choi-wan will move around the western end of a high pressure system that is over the Western North Pacific Ocean.  The high pressure system will steer Choi-wan toward the north during the next 24 hours.  On its anticipated track, the center of Typhoon Choi-wan will pass east of Japan during the next few days.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Koguma formed north of Kwajalein and former Hurricane Nolo moved west of the International Date Line.  Nolo is now designated as Typhoon Nolo because it is over the Western North Pacific Ocean.

At 11:00 p.m. EDT on Sunday the center of Tropical Storm Koguma was located at latitude 10.8°N and longitude 168.0°E which put the center about 125 miles (200 km) north of Kwajalein. Koguma was moving toward the northeast at 11 m.p.h. (17 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 1002 mb.

At 11:00 p.m. EDT on Sunday the center of Typhoon Nolo was located at latitude 25.0°N and longitude 178.6°W which put the center about 315 miles (510 km) southwest of Midway Island.  Nolo was moving toward the west-northwest at 18 m.p.h. (30 km/h).  The maximum sustained wind speed was 120 m.p.h. (195 km/h) and there were wind gusts to 150 m.p.h. (240 km/h).  The minimum surface pressure was 955 mb.

Nolo Strengthens Back to a Major Hurricane

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Hurricane Nolo strengthened back to a major hurricane as it moved over the Central North Pacific Ocean far to the west of Hawaii on Saturday.

At 11:00 p.m. EDT on Saturday the center of Hurricane Nolo was located at latitude 23.4°N and longitude 175.1°W which put the center about 200 miles (320 km) south-southwest of Lisianski Island.  Nolo was moving toward the west at 20 m.p.h. (32 km/h).  The maximum sustained wind speed was 115 m.p.h. (185 km/h) and there were wind gusts to 135 m.p.h. (215 km/h).  The minimum surface pressure was 957 mb.

Hurricane Nolo strengthened back to a major hurricane on Saturday.  However, Nolo appeared to be in the middle of an eyewall replacement cycle on Saturday night.  The inner end of a rainband wrapped around the existing eye and eyewall.  The eye was no longer seen on satellite images.  Bands of showers and thunderstorms were revolving around the core of Nolo’s circulation.  Storms near the core of Nolo generated upper level divergence that pumped mass away from the hurricane.  The removal of mass caused the surface pressure to decrease on Saturday.

The distribution of wind speeds in Hurricane Nolo was relatively symmetrical.  Winds to hurricane force extended out 30 miles (50 km) from the center of Nolo’s circulation.  Winds to tropical storm force extended out 150 miles (240 km) from the center of Hurricane Nolo.

The Hurricane Intensity Index (HII) for Hurricane Nolo is 20.6.  The Hurricane Size Index (HSI) is 11.6 and the Hurricane Wind Intensity Size Index (HWISI) is 32.2.  Hurricane Nolo is similar in size and intensity to Hurricane Delta when Delta hit Louisiana in 2020.

Hurricane Nolo will move through an environment favorable for intensification during the next 24 hours.  Nolo will move over water where the Sea Surface Temperatures are near 28°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Hurricane Nolo could weaken during the next few hours until the eyewall replacement cycle is completed.  Nolo is likely to intensify again after the eyewall replacement cycle is completed.

Hurricane Nolo will move around the southern side of a high pressure system that is over the Western North Pacific Ocean.  The high pressure system will steer Nolo toward the west-northwest during the next 24 hours.  On its anticipated track, Hurricane Nolo will move across the International Date Line on Sunday.

Elsewhere, Hurricane Rachel continued to spin south of Baja California.

At 11:00 p.m. EDT on Saturday the center of Hurricane Rachel was located at latitude 20.0°N and longitude 112.8°W which put the center about 275 miles (440 km) southwest of the southern tip of Baja California.  Rachel was moving toward the west-northwest at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 90 m.p.h. (145 km/h) and there were wind gusts to 105 m.p.h. (165 km/h).  The minimum surface pressure was 970 mb.

Typhoon Choi-wan Intensifies to Equivalent of a Major Hurricane

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Typhoon Choi-wan intensified to the equivalent of a major hurricane as it moved east-southeast of Iwo To on Saturday.  At 11:00 p.m. EDT on Saturday the center of Typhoon Choi-wan was located at latitude 22.5°N and longitude 147.1°E which put the center about 410 miles (665 km) east-southeast of Iwo To.  Choi-wan was moving toward the north-northeast at 16 m.p.h. (26 km/h).  The maximum sustained wind speed was 125 m.p.h. (200 km/h) and there were wind gusts to 155 m.p.h. (250 km/h).  The minimum surface pressure was 942 mb.

Typhoon Choi-wan intensified to the equivalent of a major hurricane on Saturday.  A circular eye with a diameter of 20 miles (32 km) was at the center of Choi-wan’s circulation.  The eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Typhoon Choi-wan.  Storms near the core of Choi-wan generated upper level divergence that pumped mass away from the typhoon.  The removal of mass caused the surface pressure to decrease.

The circulation around Typhoon Choi-wan was large.  Winds to typhoon force extended out 90 miles (145 km) from the center of Choi-wan’s circulation.  Winds to tropical storm force extended out 355 miles (575 km) from the center of Typhoon Choi-wan.

The Hurricane Intensity Index (HII) for Typhoon Choi-wan is 23.6.  The Hurricane Size Index (HSI) is 28.8 and the Hurricane Wind Intensity Size Index (HWISI) is 52.4.  Typhoon Choi-wan is similar in size and intensity to Hurricane Wilma when Wilma hit South Florida in 2005.

Typhoon Choi-wan will move through an environment that will be favorable for intensification during the next 24 hours.  Choi-wan Choi-wan will move over water where the Sea Surface Temperatures are near 28°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Typhoon Choi-wan is likely to continue to  intensify during the next 24 hours unless an eyewall replacement cycle occurs.

Typhoon Choi-wan will move around the western end of a high pressure system that is over the Western North Pacific Ocean.  The high pressure system will steer Choi-wan toward the north during the next 24 hours.  On its anticipated track, the center of Typhoon Choi-wan will pass east of Iwo To on Sunday.

Hurricane Rachel Spins South of Baja California

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Hurricane Rachel was spinning over the Eastern North Pacific Ocean south of Baja California on Friday night.

At 11:00 p.m. EDT on Friday the center of Hurricane Rachel was located at latitude 19.4°N and longitude 111.5°W which put the center about 265 miles (425 km) south-southwest of the southern tip of Baja California.  Rachel was moving toward the west at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 100 m.p.h. (160 km/h) and there were wind gusts to 120 m.p.h. (195 km/h).  The minimum surface pressure was 966 mb.

Hurricane Rachel weakened gradually on Friday.  Rachel move over cooler water that was mixed to the surface by the passage of Hurricane Polo last week.  The cooler water caused some of the thunderstorms, especially on the northern side of Rachel’s circulation to weaken.

The circulation around Hurricane Rachel was still well organized even though Rachel was a little weaker than it was yesterday.  A circular eye was still present at the center of Rachel’s circulation.  The eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that ring of storms.  Thunderstorms were also occurring in bands in the southern half of Hurricane Rachel.  Bands in the northern side of Rachel’s circulation consisted primarily of showers and lower clouds.  Storms near the center of Rachel generated less upper level divergence that pumped less mass away from the hurricane.  The removal of mass in he upper levels was less than the convergence of mass in the lower levels of the atmosphere.  So, the surface pressure to increased on Friday.

The distribution of winds speeds in Hurricane Rachel was fairly symmetrical . Winds to hurricane force extended out 45 miles (75 km) from the center of Rachel’s circulation.  Winds to tropical storm force extended out 150 miles (240 km) from the center of Hurricane Rachel.

Hurricane Rachel will move through an environment unfavorable for intensification during the next 24 hours.  Rachel will move over water where the Sea Surface Temperatures are near 27°C. It will move under the southern side of an upper level ridge that is over Baja California.  The upper level ridge will produce northeasterly winds that will blow toward the top of Rachel’s circulation.  Those winds will cause moderate vertical wind shear.  Hurricane Rachel is likely to continue to weaken on Saturday because of the moderate vertical wind shear.

Hurricane Rachel will move around the southern part of a high pressure system that is over the Eastern North Pacific Ocean.  The high pressure system will steer Rachel toward the west during the next 24 hours.  On its anticipated track, Hurricane Rachel will continue to move farther away from Baja California.

Elsewhere, former Tropical Storm Nolo strengthened back to a hurricane far to the west of Hawaii.

At 11:00 p.m. EDT on Friday the center of Hurricane Nolo was located at latitude 23.4°N and longitude 168.5°W which put the center about 145 miles (230 km) west-southwest of French Frigate Shoals.  Nolo was moving toward the west at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 85 m.p.h. (135 km/h) and there were wind gusts to 100 m.p.h. (160 km/h).  The minimum surface pressure was 978 mb.

A Tropical Storm Warning is in effect for the Papahanaumokuakea Marine National Monument from French Frigate Shoals to Lisianaki Island including Maro Reef.