Monthly Archives: August 2016

Hurricane Warning for Hawaii as Madeline Moves Closer

The Central Pacific Hurricane Center issued a Hurricane Warning for Hawaii County (i.e. the Big Island of Hawaii) as Hurricane Madeline moved steadily closer on Tuesday.  A Tropical Storm Watch has been issued for Maui County including Maui, Molokai and Lanai.

At 11:00 p.m. EDT on Tuesday the center of Hurricane Madeline was located at latitude 19.3°N and longitude 150.3°W which put it about 315 miles (505 km) east of Hilo, Hawaii.  Madeline was moving toward the west at 10 m.p.h. (16 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 972 mb.

A subtropical ridge has been steering Hurricane Madeline toward the west.  The ridge is expected to strengthen and steer Madeline more toward the west-southwest for the next day or two.  On its anticipated track Hurricane Madeline could approach the island of Hawaii in about 30 hours.

An upper level trough north of Hawaii has been producing westerly winds which are causing vertical wind shear.  The westerly winds are restricting the upper level divergence to the west of Hurricane Madeline.  However, thunderstorms in the core of the hurricane have strengthened periodically and reduced the impact of the wind shear.  The shear is expected to continue and Hurricane Madeline is forecast to slowly weaken.  However, Madeline is moving over water where the Sea Surface Temperature is near 27°C, and it could move over warmer water if it moves toward the west-southwest.

Madeline is expected to be a hurricane when it moves past the island of Hawaii.  On its anticipated track the greatest threat would be to the southern half of the island.  Madeline is a compact hurricane and winds to hurricane force only extend out about 25 miles (40 km) from the center.  Hurricane Madeline will be capable of causing localized serious wind damage.  It may also produce heavy rain and flash flooding, especially where the wind blows up the slopes.

Tropical Depression Nine Causes Hurricane Watch for Part of Florida

Although Tropical Depression Nine did not strengthen on Tuesday afternoon, guidance from numerical models suggested it could be stronger when it eventually reaches the coast of Florida.  As a result, the National Hurricane Center at 5:00 p.m. EDT issued a Hurricane Watch for the portion of the Florida coast from Anclote River to Indian Pass.  A Tropical Storm Watch was issued for the portion of the coast from Indian Pass to the Walton County/Bay County line.

At 5:00 p.m. EDT on Tuesday the center of Tropical Depression Nine was located at latitude 24.4°N and longitude 87.3°W which put it about 345 miles (555 km) west of Key West, Florida.  It 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 1004 mb.

The circulation of Tropical Depression Nine is not currently well organized.  The surface center is located northwest of an apparent mid-level center.  Upper level divergence is not well developed.  The development of thunderstorms has been cyclical during the past several days.  Clusters of thunderstorms developed south and east of the center and then they weaken.  A few hours later more thunderstorms would develop, persist for a few hours and weaken again.  It appears that new thunderstorms are developing northeast and southwest of the surface center which would be a change from the previous pattern.

The vertical structure of Tropical Depression Nine has been out of sync.  As mentioned above, the surface center was northwest of the mid-level center.  Both the surface and mid-level centers have been located on the western edge of a larger upper level high.  Clockwise flow around the upper high has been creating vertical wind shear, which has prevented the development of a vertically coherent structure in the depression.  Despite the effect of the wind shear and the lack of a coherent vertical structure, the surface center has managed to persist and become a little more organized each day.

Tropical Depression Nine is moving through an environment that is currently marginal for intensification.  It is moving over water where the Sea Surface Temperature is near 31°C.  So, there is plenty of energy in the upper ocean.  The vertical wind shear mentioned previously is the primary factor inhibiting intensification.  However, as Tropical Depression Nine moves north, if is forecast to move into an area where the upper level winds are not as strong.  If that happens, then the depression will strengthen.  As the depression becomes more organized, the rate of intensification could increase and the depression could become a hurricane over the northeastern Gulf of Mexico.

An upper level ridge over the southeastern U.S. has been blocking the northward movement of Tropical Depression Nine.  An upper level trough approaching from the west is expected to weaken the ridge.  As the ridge weakens, The depression will be able to move north.  Eventually in a couple of days, the upper level trough is expected to steer the depression more toward the northeast.  On its anticipated track the depression could be approaching the northeastern Gulf Coast by Thursday afternoon.

The northeastern Gulf Coast is very susceptible to storm surges and a surge is the greatest risk.  Locally heavy rain could cause some flooding, and there could be some minor wind damage.

Typhoon Lionrock Nearing Landfall in Japan

An upper level low is pulling Typhoon Lionrock toward a landfall in northern Japan.  At 8:00 p.m. EDT on Monday the center of Typhoon Lionrock was located at latitude 36.1°N and longitude 142.5°E which put it about 150 miles (240 km) south-southeast of Sendai, Japan.  Lionrock was moving toward the north-northwest at 24 m.p.h. (39 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 965 mb.

An upper level low west of Japan was pulling Typhoon Lionrock back toward the west-northwest.  At its current track and speed Typhoon Lionrock would make landfall on the northeastern coast of Honshu near Sendai in about six hours.

The structure of Typhoon Lionrock is changing as a result of cooler Sea Surface Temperatures and more vertical wind shear.  Lionrock is making a transition of a tropical cyclone to an extratropical cyclone.  The circulation is becoming more elongated and the typhoon is pulling cooler drier air into the western half of the circulation.  The wind field will tend to expand as the typhoon becomes extratropical.

Typhoon Lionrock will be capable of producing minor wind damage along its path.  It could also cause locally heavy rainfall and flash floods over northern Honshu.  It will pass over some of the same areas recently affected by Typhoon Mindulle.

Major Hurricanes Madeline and Lester Moving Toward Hawaii

Hurricanes Madeline and Lester intensified quickly on Monday into Major Hurricanes as they moved toward Hawaii.  The approach of Hurricane Madeline prompted the Central Pacific Hurricane Center to issue a Hurricane Watch for Hawaii County.  Both hurricanes have the potential to affect the weather around Hawaii during the next few days.

At 5:00 p.m. EDT on Monday the center of Hurricane Madeline was located at latitude 18.6°N and longitude 145.5°W which put it about 630 miles (1015 km) east of Hilo, Hawaii.  Madeline was moving toward the west-northwest at 10 m.p.h. (16 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. (220 km/h).  That made Hurricane Madeline the equivalent of a Category 3 hurricane on the Saffir-Simpson Scale.  The minimum surface pressure was 966 mb.

At 5:00 p.m. EDT on Monday the center of Hurricane Lester was located at latitude 18.0°N and longitude 130.5°W which put it about 1375 miles (2210 km) west of the southern tip of Baja California.  Lester was moving toward the west at 14 m.p.h. (22 km/h).  The maximum sustained wind speed was 130 m.p.h. (215 km/h) and there were wind gusts to 150 m.p.h. (240 km/h).  That made Hurricane Lester a Category 4 hurricane on the Saffir-Simpson Scale.  The minimum surface pressure was 951 mb.

Both Hurricanes Madeline and Lester are relatively compact hurricanes and the winds to hurricane force only extend out about 30 miles (50 km) from the center of circulation.  In Hurricane Madeline the Hurricane Intensity Index (HII) is 20.6.  The Hurricane Size Index (HSI) is 11.4 and the Hurricane Wind Intensity Size Index (HWISI) is 32.0.  Hurricane Lester is stronger, but slightly smaller.  The HII for Hurricane Lester is 25.1, while HSI is 10.3 and HWISI is 35.4.

Both hurricanes have well formed symmetrical eyes surrounded by rings of tall thunderstorms.  Each is producing well developed upper level divergence which is pumping out mass in all directions.  Hurricane Madeline has more spiral rainbands, and Hurricane Lester shows some indications that the structure might be assuming more of the shape of an annular hurricane.

Hurricanes Madeline and Lester responded to a favorable environment by intensifying rapidly on Monday.  The maximum sustained wind speed in Hurricane Madeline increased from 65 m.p.h. (105 km/h) to 115 m.p.h. (185 km/h) during the past 24 hours.  The maximum sustained wind speed in Hurricane Lester increased from 85 m.p.h. (140 km/h) to 130 m.p.h. (215 km/h) during the past 24 hours.

Hurricanes Madeline and Lester will remain in a favorable environment during the short term.  They are moving over water where the Sea Surface Temperatures (SSTs) are near 27.5°C.  The upper level winds are light and there is little vertical wind shear.  Thus, both hurricanes could maintain their intensity for another 12 to 24 hours.  When the hurricanes move closer to Hawaii, they will move over slightly cooler SSTs.  In addition, an upper level trough approaching from the northwest could increase the vertical wind shear later this week.  Hurricane Lester may also move over some cooler water mixed to the surface by Hurricane Madeline.

A subtropical ridge is steering Hurricanes Madeline and Lester toward the west and that general motion is expected to continue for the next several days.  On its anticipated track Hurricane Madeline could approach Hawaii in a couple of days.  Hurricane Lester could approach Hawaii in about five days.

 

Tropical Depression Eight Prompts Tropical Storm Warning for North Carolina

The approach of Tropical Depression Eight and the potential for intensification prompted the National Hurricane Center to issue a Tropical Storm Warning for the portion of the coast from Cape Lookout to Oregon Inlet, North Carolina including Pamlico Sound.

At 5:00 p.m. EDT on Monday the center of Tropical Depression Eight was located at latitude 33.6°N and longitude 74.0°W which put it about 140 miles (225 km) southeast of Cape Hatteras, North Carolina.  It was moving toward the northwest at 6 m.p.h. (10 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 1011 mb.

Vertical wind shear disrupted the circulation of Tropical Depression Eight earlier today, but more thunderstorms developed northwest of the center of circulation during the afternoon.  The circulation is still not well organized, but there are indications on radar that it could be developing a tighter center.  An upper level low centered near Savannah, Georgia is producing southerly winds which are causing the moderate vertical wind shear over the depression.  The upper level winds are blocking upper level divergence to the south of Tropical Depression Eight, but there are some sign that upper level divergence could be occurring to the northeast.

Tropical Depression Eight could move into an area marginally more favorable for intensification.  As it gets farther from the upper level low, the winds aloft will decrease.  The depression is moving near the Gulf Stream and the Sea Surface Temperatures are near 29.5°C.  If thunderstorms persist near the center of circulation and a more coherent vertical structure develops, the the depression could strengthen into a tropical storm.

The upper low is steering Tropical Depression toward the northwest and that general motion is expected to continue for another day or so.  When the depression reaches latitude 35°N, westerly winds will begin to steer it off toward the northeast.  On its anticipated track Tropical Depression Eight could be very near Cape Hatteras in 24 to 36 hours.

Although Tropical Depression Eight will bring some stronger winds, locally heavy rain, rip currents, higher waves and beach erosion are greater risks.

Large Typhoon Lionrock Moves Closer to Japan

Large Typhoon Lionrock moved closer to Japan on Sunday.  At 11:00 p.m. EDT on Sunday the center of Typhoon Lionrock was located at latitude 31.1°N and longitude 142.1°W which put it about 385 miles (620 km) south-southeast of Tokyo, Japan.  Lionrock was moving toward the northeast at 19 m.p.h. (31 km/h).  The maximum sustained wind speed was 110 m.p.h. (180 km/h) and there were wind gusts to 130 m.p.h. (210 km/h).  The minimum surface pressure was 952 mb.

Typhoon Lionrock retains a large symmetrical circulation.  Winds to typhoon force extend out about 40 miles (65 km) from the center.  Microwave satellite images suggest that there could be two eyewalls.  The inner eyewall is weaker on the western side and the larger outer eyewall has fewer thunderstorms on the northwestern side.  Other spiral bands are rotating around outside the outer eyewall.  Thunderstorms near the core of the circulation are generating upper level divergence which is pumping out mass primarily to the east of the typhoon.

The environment around Typhoon Lionrock would be marginally favorable for intensification.  Lionrock is moving over water where the Sea Surface Temperature (SSTs) is near 28°C.  An upper level trough west of Lionrock is generating southwesterly winds which are affecting the upper level divergence on the western side of the typhoon.  However, the vertical wind shear is not too significant.  On the other hand, concentric eyewalls often produce weakening as the inner eye wall dissipates and the stronger winds occur in the outer eyewall.  So, Lionrock could maintain a steady intensity or weaken slowly during the next 24 hours.  After that time is will move over cooler SSTs and it could weaken more.

The upper level trough is steering Typhoon Lionrock toward the northeast and that general motion is expect to continue for another 24 hours.  After that time, the upper trough will turn Lionrock back toward the northwest.  On its anticipated track Typhoon Lionrock will make landfall on northeast Honshu north of Tokyo in about 36 hours.  It could cause some wind damage.  Heavy rainfall and flash floods will also pose serious risks since Lionrock will move over some of the same areas affected by Typhoon Mindulle.

Tropical Depressions Form South of Key West & Southeast of Cape Hatteras

Two tropical depressions formed near the U.S. on Sunday.  Tropical Depression Nine formed south of Key West, Florida and Tropical Depression Eight formed southeast of Cape Hatteras, North Carolina.  Both depressions could have an impact on the U.S., but Tropical Depression Nine could pose a greater risk to the southeastern U.S.

At 5:00 p.m. EDT on Sunday the center of Tropical Depression Nine was located at latitude 23.7°N and longitude 81.7°W which put it about 60 miles (95 km) south of Key West, Florida.  It was moving toward the west at 9 m.p.h. (15 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.

At 5:00 p.m. EDT on Sunday the center of Tropical Depression Eight was located at latitude 31.8°N and longitude 70.9°W which put it about 355 miles (570 km) southeast of Cape Hatteras, North Carolina.  It was moving toward the west at 9 m.p.h. (15 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 1010 mb.

The circulation of Tropical Depression Nine is still organizing.  A NOAA plane found a distinct center of circulation, but most of the stronger thunderstorms are south and east of the center.  There is a broader counterclockwise rotation with numerous showers and thunderstorms indicated by the National Weather Service radar in Key West.  An upper level low east of Florida is contributing to easterly winds that are blowing across the northern side of the depression.  The vertical wind shear is inhibiting the development of thunderstorms north and west of the center.

The circulation of Tropical Depression Eight was more well organized earlier today.  Strong easterly winds from the same upper level low that is affecting Tropical Depression Nine are creating significant vertical wind shear.  Those winds and the shear they caused blew the upper portion of the depression’s circulation west of the low level center of circulation.  The low level circulation is presently exposed as seen on visible satellite imagery and by an Air Force Reserve Hurricane Hunter aircraft.

The intensity forecast for Tropical Depression Nine is challenging because it is moving through a complex environment.  The depression is moving over water where the Sea Surface Temperature is near 31°C.  So, there is plenty of energy in the upper ocean.  However, as mentioned above, an upper low is causing vertical wind shear which will inhibit intensification.  Tropical Depression Nine could move into a region where there is less shear when it moves over the Gulf of Mexico.  Tropical Depression Nine has a good chance to intensify into a tropical storm, but it is unclear if it could become a hurricane before it reaches the coast.

There is also significant uncertainty in the track forecast for Tropical Depression Nine.  A ridge over the southeastern U.S. is steering the depression toward the west and that general motion should continue for several more days.  The ridge is forecast to weaken during the middle of the week and that should allow Tropical Depression Nine to turn toward the north.  The timing of that turn and how sharp it will be are still uncertain.

The upper low is expected to continue to generate wind shear over Tropical Depression Eight.  If the upper levels winds remain as strong as they are now, the depression will slowly weaken.  If the upper level winds weaken, then Tropical Depression Eight could strengthen into a minimal tropical storm.  The upper level low is steering the depression west and that general motion is expected to continue in the short term.  The depression could stall just off the coast of North Carolina.

Tropical Depression Nine could intensify and bring wind and rain to the Gulf Coast later this week.  The Gulf Coast is also vulnerable to storm surges.  Given the uncertainty in both the track and intensity, interests along the coast should monitor official sources of information for updates on Tropical Depression Nine.  The primary effects of Tropical Depression Eight are likely to be higher than normal surf, rip currents and some beach erosion along the North Carolina coast.  People along the Mid-Atlantic coast should pay attention to the depression in case the forecast changes.

Gaston Regains Hurricane Intensity East of Bermuda

Gaston intensified back into a hurricane east if Bermuda on Saturday.  At 11:00 p.m. EDT on Saturday the center of Hurricane Gaston was located at latitude 29.6°N and longitude 54.2°W which put it about 655 miles (1055) km east-southeast of Bermuda.  Gaston was moving toward the northwest at 8 m.p.h. (13 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 980 mb.

The circulation of Hurricane Gaston is as well organized as it has ever been.  Gaston has a well formed circular eye surrounded by a ring of thunderstorms.  Multiple spiral rainbands are rotating around the circulation.  Upper level outflow channels to the southwest and east are enhancing upper level divergence and allowing the surface pressure to decrease.

Hurricane Gaston has moved into an environment that is favorable for further intensification.  If it moving over water where the Sea Surface Temperature is near 29°C.  An upper level low northeast of Puerto Rico and an upper level low southeast of Gaston are partially responsible for the two upper level outflow channels.  The upper level winds are weaker in between the two upper level lows and the vertical shear is less than it has been in recent days.  Gaston is likely to intensify further and it could become the first Major Hurricane of the 2016 Atlantic hurricane season.

The steering currents between the two upper lows are weaker and Hurricane Gaston has been moving more slowly toward the northwest.  Gaston is expected to move slowly northward for another day or two.  An upper level trough is likely to begin to steer the hurricane toward the east in 48 to 72 hours.  On its anticipated track Hurricane Gaston should pass well to the east of Bermuda.

Tropical Storm Madeline Forms East of Hawaii

A cluster of thunderstorms between Hawaii and Mexico developed enough organization on Friday night that the National Hurricane Center designated the system as Tropical Storm Madeline.  At 11:00 p.m. EDT on Friday the center of Tropical Storm Madeline was located at latitude 13.9°N and longitude 137.4°W which put it about 1235 miles (1990 km) east-southeast of Hilo, Hawaii.  Madeline was moving toward the west-northwest at 12 m.p.h. (19 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 of Tropical Storm Madeline is still organizing.  A primary spiral band wraps around the western side of the circulation.  There are additional spiral bands of the thunderstorms in the southern part of the tropical storm.  The thunderstorms in the primary rainband are generating upper level divergence which it pumping mass out primarily to the west of tropical storm Madeline.

Tropical Storm Madeline is moving through an environment that is favorable for intensification.  It is moving over water where the Sea Surface Temperature (SST) is near 29°C.  The upper level winds are light and there is not much vertical wind shear.  Tropical Storm Madeline is expected to intensify steadily and it could become a hurricane by the end of the weekend.  In a few days Madeline will move over cooler SSTs and into an area where the is more vertical wind shear.  When that happens, Madeline will start to weaken.

A subtropical high is steering Tropical Storm Madeline toward the west-northwest and a general west-northwest or westerly motion is expected to continue during the next few days.  On its anticipated track Madeline could approach the Hawaiian Islands in about five days.

Typhoon Lionrock Turns in the Direction of Japan

After meandering southeast of Okinawa for several days Typhoon Lionrock started moving northeast toward Japan on Friday.  At 5:00 p.m. EDT on Friday the center of Typhoon Lionrock was located at latitude 23.7°N and longitude 133.0°E which put it about 920 miles (1485 km) south-southwest of Tokyo, Japan.  Lionrockk was moving toward the northeast at 6 m.p.h. (10 km/h).  The maximum sustained wind speed was 105 m.p.h. (170 km/h) and there were wind gusts to 125 m.p.h. (200 km/h).  The minimum surface pressure was 953 mb.

Typhoon Lionrock is very well organized.  It has a circular eye surrounded by a ring of strong thunderstorms.  Additional well formed spiral bands are rotating around outside the core of Lionrock.  Thunderstorms in the eyewall and spiral bands are generating upper level divergence which are pumping out mass in all directions.  The upper level divergence is inhibited a little on the far northern edge of the circulation by northerly winds impinging on Typhoon Lionrock.  Even so, there is enough upper level divergence to compensate for the strong inflow of mass near the surface and Typhoon Lionrock has been in a nearly steady state during recent hours.

Typhoon Lionrock is moving through an environment that should allow for it to maintain its intensity during the next severall days.  It is moving over water where the Sea Surface Temperature (SST) is near 30°C.  An upper level high over China is generating northerly winds which are effecting the extreme northern edge of the outflow from Lionrock.  However, the vertical wind shear is not very strong and it should have a minimal effect on the intensity of the typhoon in the short term.  Eventually, Typhoon Lionrock will move over cooler SSTs and into a region where the upper level winds are stronger and it will start to weaken before it reaches Japan.

Typhoon Lionrock is moving around the western end of a subtropical ridge and that ridge is beginning to steer it toward the northeast.  That general motion is expected to continue for the next several days.  Eventually Lionrock is forecast to turn more toward the northwest.  On its anticipated track Typhoon Lionrock could approach the eastern coast of Honshu in three or four days.  Lionrock could still be a typhoon at that time.

If Lionrock makes landfall in Honshu as a typhoon it will be strong enough to cause some wind damage.  In addition, Typhoon Lionrock could move over some of the same areas affected by Typhoon Mindulle.  Heavy rain caused by Lionrock could create the potential for additional flash flooding and mudslides.