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Typhoon Sarika Near Catanduanes Island, Threatens Luzon

The center of Typhoon Sarika is located near Catanduanes Island and Sarika poses a serious threat to Luzon.  At 5:00 p.m. EDT on Friday the center of Typhoon Sarika was located at latitude 14.4°N and longitude 124.8°E which put it about 280 miles (455 km) east of Manila, Philippines.  Sarika was moving toward the west-northwest at 8 m.p.h. (13 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 981 mb.

The circulation of Typhoon Sarika is well organized.  An eye has appeared at times on conventional and microwave satellite imagery.  A primary rainband wrapped around the eye and strong thunderstorms are occurring in the eyewall.  Additional, well formed rainbands are rotating around the core of the circulation.  The convection around the core is generating well developed upper level divergence which is pumping away mass.

Typhoon Sarika is moving through a very favorable environment.  It is moving over water where the Sea Surface Temperature is near 30°C.  The upper level winds are weak and there is little vertical wind shear.  Typhoon Sarika will continue to intensify as long as the center stays over the water and it could intensify rapidly now that the circulation is well organized.

A subtropical ridge north of Sarika is steering the typhoon toward the west-northwest and that general motion is expected to continue for several more days.  On its anticipated track the center of Typhoon Sarika will remain north of Catanduanes Island.  It will pass just to the north of Daet and Labo on Saturday.  The center of Typhoon Sarika could be near or just to the north of the Polillo Islands in 12-16 hours.  Sarika could make a landfall near Baler on Luzon in 18-24 hours.

Sarika is a well organized intensifying typhoon.  It could bring strong winds to portions of northern Luzon.  Typhoon Sarika will also bring very heavy rain and create the potential for flash floods and mudslides.  Sarika will generate a storm surge in places where the wind blows the water toward the coast.

Tropical Storm Sarika Forms East of the Philippines

Tropical Storm Sarika formed east of the Philippines on Thursday.  At 11:00 p.m. EDT on Thursday the center of Tropical Storm Sarika was located at latitude 13.8°N and longitude 127.0°W which put it about 425 miles (685 km) east of Manila, Philippines.  Sarika was moving toward the west at 11 m.p.h. (18 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 997 mb.

The circulation of Tropical Storm Sarika is still organizing.  Most of the thunderstorms are occurring in a broad rainband that curls around the western and southern sides of the circulation.  There are a few thunderstorms in thinner rainbands in the eastern half of the circulation.  More thunderstorms are developing closer to the center of circulation.  Those thunderstorms are beginning to produce upper level divergence which is pumping out mass.  As the mass is removed, the pressure decreases and the wind speeds increase.

Tropical Storm Sarika is moving through an environment that is generally favorable for intensification.  It is moving over water where the Sea Surface Temperature is near 30°C.  An upper level ridge to the north of Sarika is producing easterly winds which are blowing across the top of the tropical storm.  The vertical wind shear may account for the asymmetrical distribution of thunderstorms, but it is not strong enough to prevent Sarika from intensifying.  The vertical wind shear could slow the rate of intensification while the core of the circulation becomes better organized.  Sarika could strengthen into a typhoon with the next 24 to 36 hours.

A subtropical ridge north of Sarika is steering the tropical storm toward the west and that general motion is expected to continue for another 12 to 24 hours.  In a day or so Tropical Storm Sarika is forecast to turn more toward the west-northwest.  On its anticipated track Tropical Storm Sarika could be near Catanduanes Island in about 24 hours.  Sarika could be near Central Luzon in about 48 hours.

Tropical Storm Sarika is expected to intensify into a typhoon.  It could bring strong winds and very heavy rain to parts of the northern Philippines.  The heavy rain could cause flash floods and mudslides.

Typhoon Koppu Still Affecting Northern Luzon

The center of Typhoon Koppu moved across northern Luzon on Sunday and it is still affecting that region.  At 11:00 p.m. EDT on Sunday the center of Typhoon Koppu was located at latitude 17.5°N and longitude 120.3°E which put it about 200 miles (320 km) north-northwest of Manila, Philippines and just west of the coast of northwestern Luzon.  Koppu was moving toward the north-northeast at 5 m.p.h. (8 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. (170 km/h).  The minimum surface pressure was 968 mb.

Passage over northern Luzon weakened Typhoon Koppu and its structure is asymmetrical.  Most of the stronger thunderstorms are located in the western half of the circulation.  Much of the eastern half of the circulation is still over Luzon and there are few thunderstorms there.  The center of circulation is just west of Luzon.  Since it is back over water, the core of the typhoon could start to reorganize.  Intensification will be limited because of the large proportion of the circulation which is over land.

Koppu is near the western end of a subtropical ridge, which is causing the typhoon to move slowly northward.  That motion could continue for another 24 to 36 hours.  Eventually the ridge is expected to strengthen and push Typhoon Koppu northward at a faster speed.  Typhoon Koppu will continue to bring heavy rain to parts of northern Luzon for another day or two.

Dangerous Typhoon Koppu Making Landfall in Northern Luzon

Typhoon Koppu intensified rapidly during the past 12 hours and it is making landfall near Baler in northern Luzon as the equivalent of a Category 4 hurricane on the Saffir-Simpson Scale.  At 11:00 a.m. EDT on Saturday the center of Typhoon Koppu was located at latitude 16.0°N and longitude 122.9°E which put it about 170 miles (275 km) east-northeast of Manila, Philippines.  Koppu was moving toward the west-northwest at 7 m.p.h. (11 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 918 mb.  Typhoon Koppu has a Hurricane Intensity Index (HII) of 31.6, a Hurricane Size Index (HSI) of 17.5 and a Hurricane Wind Intensity Size Index (HWISI) of 49.1, which means it is capable of producing regional significant wind damage.  In addition the slow movement of Koppu means it will produce very heavy rainfall which will create the potential for serious flooding and landslides.

Koppu will continue to move toward the west-northwest for another 12 to 24 hours.  Then it will reach the western end of the subtropical ridge that has been steering it and start to move toward the north.  Although Typhoon Koppu will weaken as it moves across northern Luzon, it will be over that area for 36 to 48 hours.  Koppu has the potential to cause widespread damage due to winds, floods and landslides.

Typhoon Koppu Continues to Intensify and Threaten Luzon

Typhoon Koppu continued to intensify on Friday and it maintained its steady course toward northern Luzon.  At 5:00 p.m. EDT on Friday the center of Typhoon Koppu was located at latitude 15.8°N and longitude 124.5°E which put it about 270 miles (435 km) east-northeast of Manila, Philippines.  Koppu 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 947 mb.

Typhoon Koppu is evolving into a large well organized typhoon.  An eye has formed at the center of the circulation and multiple rain bands spiral around the core of the typhoon.  Upper level divergence is pumping mass away from the center of circulation.  Koppu is moving over water where the Sea Surface Temperature is near 30°C.  The upper level winds are light and there is not much vertical wind shear.  Koppu is likely to continue to intensify until it begins to interact with northern Luzon.

A subtropical ridge is steering Koppu toward the west and that steering pattern is expected to continue for another 24 to 36 hours.  On its anticipated track the center of Typhoon Koppu will be very near the northeastern coast of Luzon in about 24 hours.  Koppu will bring strong winds, heavy rain and a storm surge to northern Luzon.  The large size of Koppu and its relatively slow movement means that it could produce very heavy rainfall.  Serious flooding and numerous mudslides are possible across northern Luzon.

Intensifying Typhoon Koppu Moving Toward Northern Luzon

Typhoon Koppu intensified on Thursday as it continued to move steadily toward Northern Luzon.  At 11:00 p.m. EDT the center of Typhoon Koppu was located at latitude 15.6°N and longitude 126.9°E which put it about 425 miles (685 km) east of Manila, Philippines.  Koppu was moving toward the west at 8 m.p.h. (13 km/h).  The maximum sustained wind speed was 90 m.p.h. (145 km/h) and there were wind gusts to 115 m.p.h. (185 km/h).  The minimum surface pressure was 969 mb.

Typhoon Koppu is moving over water where the Sea Surface Temperature is near 30°C.  The upper level winds lessened on Thursday which decreased the vertical wind shear and allowed Koppu to intensify more quickly.  The core of the circulation consolidated and there are suggestions that an eyewall may be forming.  Koppu is expected to move through a favorable environment until it reaches northern Luzon and further intensification is very likely.

A subtropical ridge is steering Koppu toward the west and that general steering pattern is expected to continue for another 36 to 48 hours.  On its anticipated track, Typhoon Koppu will approach northern Luzon in 36 to 42 hours.  It could bring strong winds, heavy rain and a storm surge when it reaches that area.  The heavy rain could produce floods and mudslides as Koppu moves over northern Luzon.

Tropical Storm Koppu Forms North of Yap

In spite of significant vertical wind shear a surface circulation has been consolidating inside an area of thunderstorms north of Yap.  The system has been designated Tropical Storm Koppu.  At 5:00 p.m. EDT on Tuesday the center of Tropical Storm Koppu was located at latitude 15.7°N and longitude 137.1°E which put it about 430 miles (690 km) north of Yap.  Koppu was moving toward the west at 14 m.p.h. (23 km/h).  The maximum sustained wind speed was 45 m.p.h. (75 km/h) and there were gusts to 60 m.p.h. (95 km/h).  The minimum surface pressure was 993 mb.

Significant vertical wind shear is inhibiting the organization of Tropical Storm Koppu.  An upper level ridge north of Koppu is generating strong northeasterly winds over the top of the tropical storm.  The vertical wind shear is causing most of the strong thunderstorms to be located southwest of the center of circulation.  The only other deep convection is occurring in a band that is west of the core of the circulation.

Koppu is over water where the Sea Surface Temperature is near 30°C and so there is plenty of energy in the upper ocean.  The wind shear will inhibit intensification for another 24 to 48 hours before it starts to subside.  Koppu could intensify much more quickly later this week when it moves into an area where the upper level winds are lighter.  Koppu could become a typhoon withing 36 to 48 hours and it could be a strong typhoon by the end of the week.

A subtropical ridge is steering Tropical Storm Koppu quickly to the west.  That general motion is expected to continue for the rest of the week.  On its anticipated track Koppu could be approaching northern Luzon in about three or four days.  It could be a significant typhoon by that time.