Category Archives: Western North Pacific

Western Pacific Typhoons and Tropical Storms

Tropical Storm Nangka Forms East of Kwajalein

Another tropical storm formed over the western North Pacific when a circulation developed west of the International Dateline and was designated as Tropical Storm Nangka (11W).  At 11:00 p.m. EDT on Friday the center of Tropical Storm Nangka was located at latitude 9.9°N and longitude 169.2°E which put it about 150 miles east-northeast of Kwajalein.  Nangka was moving toward the west-northwest at 10 m.p.h. (16 km/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 992 mb.

Tropical Storm Nangka is moving over water where the Sea Surface Temperature is near 30°C.  The upper level winds are light and upper level divergence is increasing.  However, there is sinking drier air north of the tropical storm and the circulation appears to be pulling some of the drier air into it.  As a result many of the stronger thunderstorms are occurring in the western half of the circulation.  The drier air could inhibit intensification in the short term.  The other favorable environmental factors are likely to produce intensification in the longer term once Nangka moves west of the drier air.

A subtropical ridge north of Nangka is expected to steer it in a west-northwesterly direction during the next few days.  On its expected track Nangka will bring wind and rain to a number of atolls in the Marshall Islands.  Nangka could approach the Mariana Islands in a few days.

Wind Shear Affecting Tropical Storm Chan-hom

Although Tropical Storm Chan-hom briefly reached typhoon intensity on Thursday, strong upper vertical wind shear quickly weakened it back to a tropical storm.  At 11:00 p.m. EDT on Thursday the center of Tropical Storm Chan-hom was located at latitude 10.3°N and longitude 148.0°E which put it about 325 miles (525 km) southeast of Guam.  Chan-hom was moving toward the west 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 981 mb.  A Typhoon Watch has been issued for Guam, Rota, Tinian and Saipan.

The combination of a upper level ridge and an upper level low produced strong northeasterly winds that blew the middle and upper portions of the circulation of Chan-hom west of the low level circulation.  The middle and upper parts of the circulation are about 100 miles (160 km) southwest of the surface center.  There are no thunderstorms currently near the surface center.  The upper level winds and the vertical wind shear they are producing are likely to continue to weaken Chan-hom on Friday.  The upper low is expected to move eastward during the next several days, which would result in a decrease in the wind shear.  If the surface circulation is still intact, it will be over warm Sea Surface Temperatures and reintensification would be possible.

Chan-hom is likely to be steered toward the west on Friday by the winds in the lower levels.  If new thunderstorms develop near the center and the height of the circulation increases, then a subtropical ridge in the middle levels could cause the tropical storm to turn toward the northwest.  If that turn occurs on Friday, it could put Chan-hom on a track toward Guam, Saipan or Tiniana.  If the turn occurs later in the weekend, then Chan-hom could pass to the south of those islands before it turns toward the northwest.

Tropical Storm Linfa Forms East of the Philippines

A well defined low level circulation developed in an area of thunderstorms east of the Philippines on Thursday and the system was designated as Tropical Storm Linfa (10W).  At 5:00 p.m. EDT on Thursday the center of Tropical Storm Linfa was located at latitude 16.3°N and longitude 127.6°E which put it about 470 miles (760 km) east-northeast of Manila, Philippines.  Linfa was moving toward the northwest at 7 m.p.h. (11 km/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 993 mb.

Linfa developed over water where the Sea Surface Temperature (SST) is near 30°C,  There is sufficient energy in the upper ocean to support intensification.  An upper level ridge centered northwest of Linfa is producing northeasterly winds over the top of the circulation and most of the thunderstorms are occurring west of the center.  The vertical wind shear is modest and some upper level divergence is present, especially over the western half of the circulation.  The vertical wind shear is expected to remain moderate and Linfa could intensify during the next several days.  If the upper level winds weaken, then a period of more rapid intensification is possible.

Linfa is being steered by a subtropical ridge located to the east of the tropical storm.  The ridge is expected to steer it toward the northwest in the short term.  As Linfa reaches the western end of the ridge it is expected to be steered more toward the north.  The timing of the turn toward the north will be important because it will determine if Linfa moves over the northern Philippines or moves northeast of that area.  The timing on the turn to the north will also determine the potential risk for Taiwan.  Another factor that could complicated the track forecast is a potential interaction with Typhoon Chan-hom which is abut 1500 miles (2400 km) east-southeast of Linfa.

Tropical Storm Chan-hom Forms East of Guam

A center of circulation developed in an area of thunderstorms on the opposite side of the Equator from Tropical Cyclone Raquel and it was designated as Tropical Storm Chan-hom on Tuesday.  At 11:00 p.m. EDT on Tuesday the center of Tropical Storm Chan-hom was located at latitude 11.0°N and longitude 156.5°E which put it about 250 miles (400 km) north-northeast of Oroluk atoll and about 800 miles (1290 km) east of Guam.  Chan-hom was moving toward the west at 22 m.p.h. (35 km/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 993 mb.

Tropical Storm Chan-hom formed over water where the Sea Surface Temperatures (SSTs) are around 29°C to 30°C and there is plenty of energy in the upper ocean to support intensification.  An upper level ridge located north of the tropical storm is generating easterly winds over the top of the circulation.  The easterly winds are generating moderate amounts of vertical wind shear and many of the stronger thunderstorms are occurring in the western half of the circulation.  Those thunderstorms are producing strong rising motion and upper level divergence is well developed on the western side of Chan-hom.  However the upper level easterly winds are interfering with upper level divergence on the eastern side of the tropical storm.  As a result, a modest rate of intensification is expected in the short term.  If the upper level winds were to lessen, then a more rapid rate of intensification would be possible.

The upper level ridge is expected to steer Chan-hom toward the west during the next several days.  On its anticipated track Chan-hom could approach Guam in about three days.  It could be a typhoon by that time.  However, there is some divergence in the track guidance from numerical models at the end of this week and that is producing uncertainty about the future track of Chan during that time period.

Tropical Storm Kujira Makes Landfall on Hainan Island

Tropical Storm Kujira made landfall on the east coast of Hainan Island on Monday.  At 11:00 p.m. EDT on Monday the center of Tropical Storm Kujira was located at latitude 19.9°N and longitude 109.1°E which put it about 100 miles (160 km) south of Beihai, China.  Kujira was moving toward the northwest at 10 m.p.h. (16 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 992 mb.

Passing across Hainan Island weakened Tropical Storm Kujira on Monday.  In addition, an upper level ridge over southern Asia continues to generate vertical wind shear over the tropical storm.  However, it will move over warm water when the center moves northwest of Hainan Island.  So, Kujira could maintain tropical storm intensity until it makes another landfall in China in about 18 to 24 hours.  The primary risk will be locally heavy rainfall.

Tropical Storm Kujira Nearing Hainan Island

Tropical Storm Kujira moved slowly northward on Sunday.  At 11:00 p.m. EDT on Sunday night the center of Tropical Storm Kujira was located at latitude 18.0°N and longitude 111.2°E which put it about 150 miles (240 km) south-southeast of Xuwen, China.  Kujira was moving toward the north-northwest at 7 m.p.h. (11 km/h).  The maximum sustained wind speed was 45 m.p.h. (70 km/h) and there were wind gusts to 65 m.p.h. (105 km/h).  The minimum surface pressure was 994 mb.

Although Kujira is moving over water where the Sea Surface Temperature is near 30°C, vertical wind shear is inhibiting intensification.  An upper level ridge over southern Asia is producing northeasterly winds over the top of Kujira.  As a result of the vertical shear, most of the stronger thunderstorms are occurring southwest of the center of circulation.  As Kujira moves farther north, some of the circulation will move over Hainan Island, which will further limit the potential for intensification.

Kujira is moving around the western end of a subtropical ridge which is steering the tropical storm toward the north.  The steering pattern is expected to remain in place for the early part of the week.  Kujira could be very close to the east coast of Hainan Island in about 12 hours.  It will move near or just east of Hainan and Kujira could make landfall in China in 24 to 36 hours.  Although it will bring some wind, the primary risk will be locally heavy rainfall.

Tropical Storm Kujira Forms South of Hainan Island

A surface circulation organized within a larger area of thunderstorms east of Vietnam on Saturday and the system was designated as Tropical Storm Kujira.  At 11:00 p.m. EDT on Saturday the center of Tropical Storm Kujira was located at latitude 15.7°N and longitude 111.4°E which put it about 210 miles (340 km) east of Da Nang, Vietnam.  Kujira was moving north-northwest at 3 m.p.h. (5 km/h).  The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 60 m.p.h. (95 km/h).  The minimum surface pressure was 998 mb.

Tropical Storm Kujira is moving over water where the Sea Surface Temperature is near 30°C.  However an upper level ridge over southern Asia is generating northeasterly winds over the top of Kujira.  Those northeasterly winds are producing moderate vertical wind shear, which is causing most of the stronger thunderstorms to be located in the western half of the circulation.  Some spiral bands are beginning to form and a band is wrapping around the southern side of the center of circulation.  It appears that Kujira is becoming more well organized and intensification is likely, although the wind shear could slow that process.

Kujira is in an area where the steering currents are weak.  The tropical storm is near the western end of a subtropical ridge and the highest probability is that it will move north toward Hainan Island and southern China.  Some numerical models project a landfall on Hainan Island, but others have Kujira passing east of the island before making landfall on the coast of China.  In either scenario Kujira could approach Hainan Island in 24 to 36 hours.

Typhoon Dolphin Is Bringing Wind and Heavy Rain to Iwo To

Even though the center of Typhoon Dolphin is still over 100 miles from Iwo To, it is bringing wind and heavy rain to that island.  The most recent surface observation reported southeast winds at 43 m.p.h. with gusts to 66 m.p.h.  At 11:00 p.m. EDT on Monday the center of Typhoon Dolphin was located near latitude 24.6° and longitude 139.7°E which put it about 140 miles west-southwest of Iwo To.  Dolphin was moving toward the northeast at 10 m.p.h.  The maximum sustained wind speed was 85 m.p.h. and there were gusts to 105 m.p.h.  The minimum surface pressure was 967 mb.

Dolphin will continue to move over cooler Sea Surface Temperatures as it moves farther north.  It will also encounter strong upper level westerly winds, which will increase vertical wind shear.  So, Typhoon Dolphin will weaken steadily on Tuesday.  It will eventually transition into an extratropical cyclone as it passes southeast of Japan.

Upper level westerly winds are steering Typhoon Dolphin toward the northeast.  It is expected to accelerate toward the northeast on Tuesday.  On its anticipated track the center of Dolphin will pass northwest of Iwo To during the next few hours.  It could pass very near Chichi Jima on Tuesday and bring strong wind and heavy rain.

Typhoon Dolphin Approaching Iwo To

Although Typhoon Dolphin is weakening, it will still be a typhoon when it approaches Iwo To in about 24 hours.  At 11:00 p.m. EDT on Sunday the center of Typhoon Dolphin was located at latitude 21.3°N and longitude 138.7°E which put it about 320 miles south-southwest of Iwo To.  Dolphin was moving toward the north at 10 m.p.h.  The maximum sustained wind speed was 125 m.p.h. and there were gusts to 155 m.p.h.  The minimum surface pressure was 941 mb.

Upper level westerly winds blowing over the top of Dolphin are tilting the circulation to the east and contributing to the weakening of the typhoon.  Dolphin will soon be moving over water where the Sea Surface Temperature (SST) is lower than 26°C and as it moves farther north it will encounter stronger upper level westerly winds.  Cooler SSTs and more vertical wind shear will continue to weaken Dolphin.  As it moves into a cooler environment southeast of Japan in several days, Dolphin will make a transition to an extratropical cyclone.

Dolphin is moving around the the western end of a subtropical ridge.  It will gradually turn more toward the northeast on Monday.  As it encounters stronger westerly winds, Dolphin will start to move more rapidly toward the northeast.  On its anticipated track, Dolphin will near Iwo To in about 24 hours.  Although it will be weaker, it will still be a typhoon at that time.

 

Typhoon Dolphin Becomes Equivalent of Category 5 Hurricane

Typhoon Dolphin intensified rapidly on Saturday and it reached an intensity equivalent to a Category 5 hurricane on the Saffir-Simpson Scale.  At 11:00 p.m. EDT on Saturday the center of Typhoon Dolphin was located at latitude 18.3°N and longitude 139.0E which put it about 470 miles south-southwest of Iwo To.  Dolphin was moving toward the northwest at 12 m.p.h.  The maximum sustained wind speed was 160 m.p.h. and there were gusts to 195 m.p.h.  The minimum surface pressure was 918 mb.

Dolphin is moving over water where the Sea Surface Temperatures (SSTs) are between 26°C and 27°C.  It is in an area where the upper level winds are light and there is not much vertical wind shear.  It has very well developed upper level outflow, especially on the northeast side of the circulation.  Dolphin developed concentric eyewalls earlier on Saturday, but the inner eyewall appears to have dissipated.  The circulation has consolidated around the outer eyewall and it is now the core of the circulation.  Dolphin is probably near its peak intensity.  As it moves farther north, the SSTs will decrease and it will move over water cooler than 26°C.    In addition, upper level westerly winds will increase as the typhoon moves north of 25°N.  Cooler SSTs and more vertical wind shear will produce a steady weakening of Dolphin as it moves north.

Dolphin is moving around the western end of a subtropical ridge.  It is likely to move northward on Sunday and then turn to the northeast on Monday.  As it encounters westerly winds early next week, it is likely to accelerate toward the northeast.  On its anticipated track Dolphin will approach Iwo To in about 48 hours.  It could still be a significant typhoon at that time.