Category Archives: Tropical Cyclones

Information about tropical cyclones

Tropical Cyclone Organizing Over Southwest Indian Ocean

A tropical cyclone organized north of La Reunion and east of Madagascar over the Southwest Indian Ocean on Friday.  At 1:00 p.m. EST on Friday the center of the tropical cyclone was located at latitude 14.5°N and longitude 56.1°E, which put it about 435 miles (700 km) north of La Reunion.  The tropical cyclone was moving toward the south 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 1002 mb.

An area of showers and thunderstorms persisted north of La Reunion for much of the past week.  Curved bands of showers and thunderstorms began to develop on Friday and the circulation took on more of a circular shape.  Thunderstorms near the center of the circulation began to generate upper level divergence which was pumping out mass and the surface pressure started to decrease.  There is a distinct center in the low level circulation and the tropical cyclone would be the equivalent of a tropical depression if it were over the Atlantic or Pacific Oceans.

The environment surrounding the tropical cyclone is favorable for further intensification.  The tropical cyclone is over water where the Sea Surface temperature is around 28.5°C.  So, there is plenty of energy in the upper ocean.  The upper level winds over the tropical cyclone are light and there is little vertical wind shear.  The absence of vertical wind shear is allowing the upper level divergence to pump out mass in all directions.  The tropical cyclone is expected to strengthen during the next 24 hours and it could intensify quickly if the inner core continues to develop.

The winds at the steering level are weak, which is why the system did not move much during the past few days.  Weak northerly winds could push the tropical cyclone slowly toward the south toward Mauritius and La Reunion.  The tropical cyclone could be near those islands in about three or four days.

Tropical Cyclone 03S Moving West of Australia

A tropical cyclone designated 03S moved farther west of Australia and weakened on Saturday.  Tropical Cyclone 03S moved across northern Australia as a low pressure system last week before move off the coast near Broome.  After the center of the low moved over the South Indian Ocean thunderstorms developed near the core of the system and the Australian Bureau of Meteorology classified it as a tropical low.  The tropical low strengthened into the equivalent of a tropical storm on Friday night, but the Australian Bureau of Meteorology did not give the system a name.

At 7:00 p.m. EST on Saturday the center of Tropical Cyclone 03S was located at latitude 19.5°S and longitude 109.8°E which put it about 335 miles (540 km) northwest of Learmonth, Australia.  Tropical Cyclone 03S was moving toward the west 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 994 mb.

Tropical Cyclone 03S has a well defined low level circulation but the distribution of thunderstorms is asymmetrical.  Most of the stronger thunderstorms are forming in bands west of the center of circulation.  There are also bands in the eastern half of the circulation but they consist primarily of low clouds and rain showers.  Strong easterly winds in the upper levels are shearing the tops off of any thunderstorms that develop in the eastern part of the circulation.  The easterly winds are also inhibiting upper level divergence to the east of the center.

Tropical Cyclone 03S will move into an environment that will be unfavorable for intensification.  Tropical Cyclone 03S is moving over water where the Sea Surface Temperature is near 26°C, but it will move over cooler water during the next several days.  An upper level ridge centered over Australia is generating easterly winds which are blowing across the top of the tropical cyclone.  The easterly winds are causing moderate vertical wind shear and are responsible for the asymmetrical distribution of thunderstorms.  Tropical Cyclone 03S is likely to weaken slowly during the next several days.

A subtropical ridge will continue to steer Tropical Cyclone 03S to the west during the next few days.  On its anticipated track Tropical Cyclone 03S is expected to move farther away from Western Australia as it weakens.

Tropical Low Forms Over Western Australia

An area of low pressure system has been moving across northern Australia during the past few days.  The low remains organized and the Australian Bureau of Meteorology classified the system as a Tropical Low on Wednesday because of the potential for it to develop into a tropical cyclone.  At 10:00 a.m. EST on Wednesday the center of the Tropical Low was located at latitude 15.9°S and longitude 127.0°E which put it about 80 miles (130 km) west-southwest of Wyndham, Australia.  The Tropical Low was moving toward the west at 9 m.p.h. (15 km/h).  The maximum sustained wind speed was 30 m.p.h. (50 km/h) an there were wind gusts to 40 m.p.h. (65 km/h).  The minimum surface pressure was 1002 mb.

There is a well defined cyclonic circulation in the lower levels of the atmosphere, but there are not many thunderstorms in the core of that circulation.  Most of the thunderstorms are developing in bands that are on the periphery of the circulation.  The strongest thunderstorms are forming in bands in the western portion of the circulation as that part of the Tropical Low begins to moves over water.  The strongest winds are also occurring in these thunderstorms that are over water.  The Tropical Low is moving underneath an upper level ridge and the ridge is causing upper level divergence which is pumping out mass.

The core of the Tropical Low is still over Western Australia and moving over land is the primary factor inhibiting intensification of the system.  The atmospheric environment is favorable for intensification.  The upper level ridge is producing light winds over the Tropical Low and there is little vertical wind shear.  The Sea Surface Temperature of the water west of Australia is near 30°C and there will be plenty of energy in the ocean to support strengthening when the core of the circulation moves west of Australia.  Some slow organization of the circulation is possible during the next 12 hours as the core of the Tropical Low moves closer to the coast of Western Australia.  Further intensification is likely during the next several days once the core of the Tropical Low moves over the warm water.  The Tropical Low could strengthen into the first named tropical cyclone of 2017 later this week.

The upper level ridge is producing light easterly winds which are slowly steering the Tropical Low toward the west.  That general motion is expected to continue for another day or so.  Eventually, the Tropical Low is forecast to move on a west-southwesterly track that would paralle, but keep it to the west of the coast of Western Australia during the next several days.

Tropical Depression 01W Redevelops East of Vietnam

More thunderstorms developed on Saturday around the circulation previously designated Tropical Depression 01W earlier this week when it moved through the southern Philippines.  At 10:00 p.m. EST the center of Tropical Depression 01W was located at latitude 9.4°N and longitude 109.1°E which put it about 220 miles (355 km) east-southeast of Ho Chi Minh City, Vietnam.  The depression was moving toward the west 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. (75 km/h).  The minimum surface pressure was 1002 mb.

After persisting mainly as a low level circulation during the past few days as it moved westward across the South China Sea, more thunderstorms developed in the depression on Saturday.  Most of the thunderstorms developed in bands north and west of the center of circulation.  There were bands of low clouds and showers in the southeastern portion of the circulation. The depression has a well defined low level center of circulation.  Thunderstorms were starting to generate some upper level divergence which was pumping mass away to the northwest of the depression.

The depression will be moving through an environment that is marginal for intensification.  It will be moving over water where the Sea Surface Temperature is near 26°C to 27°C.  So, there will be enough energy in the upper ocean to support intensification.  An upper level ridge to the east of the depression is generating southeasterly winds which are blowing across the top of the circulation.  The moderate vertical wind shear will inhibit intensification.  If the shear does not increase, the depression could maintain its intensity or strengthen slightly during the next 24 hours.

A ridge north of the depression is steering it toward the west and that general motion is expected to continue for another day or two.  On its anticipated track the depression will move toward the southernmost part of Vietnam.  The depression could bring locally heavy rain to southern Vietnam.  The rain could be heavy enough to cause flooding in some areas.

Tropical Depression 01W Forms Near Mindanao

A center of circulation formed within a cluster of thunderstorms east of Mindanao on Saturday and the system was designated Tropical Depression 01W.  At 10:00 p.m. EST on Saturday the center of Tropical Depression 01W was located at latitude 9.2°N and longitude 126.5°E which put it about 200 miles (320 km) east-southeast of Cebu, Philippines.  The depression was moving toward the northwest at 10 m.p.h.  The maximum sustained wind speed was 30 m.p.h. (50 km/h) and there were wind gusts to 40 m.p.h. (65 km/h).  The minimum surface pressure was 1000 mb.

Although there is a distinct center of circulation in Tropical Depression 01W, the distribution of thunderstorms is asymmetrical.  Most of the stronger thunderstorms are forming in the northern half of the circulation and there are few thunderstorms in the southern half of the circulation.  The thunderstorms in the northern half of the circulation are generating upper level divergence that is pumping out mass toward the northeast and northwest of the tropical depression.

Tropical Depression 01W will be moving through an oceanic and atmospheric environment that is somewhat favorable for intensification.  It will move over water where the Sea Surface Temperature is near 28°C.  An upper level ridge is generating southeasterly winds which are blowing across the top of the depression, but the vertical wind shear is not too strong.  However, the center of Tropical Depression 01W will move over some of the islands of the southern Philippines.  Increases friction and high topography will disrupt the circulation each time the center moves over land.  The intermittent passages overland will cause weakening and the intensity of Tropical Depression 01W is likely to fluctuate during the next several days.

A subtropical ridge north of the depression is steering it toward the northwest.  The ridge is forecast to strengthen and it is predicted to steer Tropical Depression 01W in a general westerly direction during the next several days.  On its anticipated track the center of Tropical Depression 01W will pass near northern Mindanao, Siargao Island, Dinogat Island, Leyte, Bohol Island, Cebu, Negros, and Panay Island.

Heavy rain associated will be the greatest threat with Tropical Depression 01W.  The heaviest rain will fall north of where the center moves.  The heavy rain could cause flooding and mudslides,

Typhoon Nock-ten Moves South of Manila

Typhoon Nock-ten moved across southern Luzon and weakened on Sunday.  At 10:00 p.m. EST on Sunday the center of Typhoon Nock-ten was located at latitude 13.8°N and longitude 120.9°E which put it near Batangas and about 75 miles (120 km/h) south-southeast of Manila, Philippines.  Nock-ten was moving toward the west at 18 m.p.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 956 mb.

Typhoon Nock-ten weakened when the center moved over parts of southern Luzon.  Increased friction slowed the wind and areas of higher terrain temporarily disrupted the lower level circulation.  In addition easterly winds in the upper levels appeared to increase.  The increased vertical wind shear contributed to making the circulation more asymmetrical.  More of the thunderstorms formed in the western half of the circulation and there were fewer storms east of the center of circulation.

Typhoon Nock-ten will remain in a favorable environment for another day or so.  When Nock-ten moves west of Luzon into the South China Sea, it will move over water where the Sea Surface Temperature is near 29°C.  Typhoon Nock-ten could maintain its intensity or weaken slowly during the next 24 hours.  After that time Typhoon Nock-ten will move into an environment where the upper level winds are stronger.  Increased vertical wind shear will weaken the circulation.

A subtropical ridge to the north of Nock-ten is steering the typhoon toward the west and that general motion is expected to continue for another day or two.  The center of Typhoon Nock-ten passed near Catanduanes Island.  The center then moved near Tabaco, Ligao, Burias Island, San Francisco, and Marinduque Island.  The center is near Batangas.  It will move across Lake Taal and Lubang Island before it passes into the South China Sea.  Typhoon Nock-ten will continue to produce gusty winds and locally heavy rain as the center passes south of Manila.

Strong Typhoon Nock-ten Makes Landfall in Luzon

Strong Typhoon Nock-ten made landfall in Luzon on Sunday after passing very close to Catanduanes Island.  At 10:00 a.m. EST on Sunday the center of Typhoon Nock-ten was located at latitude 13.5°N and longitude 123.5°E which put it near Tabaco and about 215 miles (345 km) east-southeast of Manila, Philippines.  Nock-ten was moving toward the west 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. (290 km/h).  The minimum surface pressure was 924 mb.

The circulation of Typhoon Nock-ten is very well organized.  There is a circular eye with a diameter of 14 miles (23 km) at the center of circulation.  A ring of very strong thunderstorms surrounds the eye and the strongest winds are occurring in those thunderstorms.  A second ring of thunderstorms nearly surrounds the inner eye and eyewall.  Nock-ten may have a double eyewall structure.  Additional bands of thunderstorms are occurring outside the core of the circulation.  Winds to typhoon force extend out about 50 miles (80 km) from the center.  The core of Typhoon Nock-ten is generating strong upper level divergence which is pumping out mass in all directions.

The Hurricane Intensity Index (HII) is 31.6.  The Hurricane Size Index (HSI) is 15.5 and the Hurricane Wind Intensity Size Index (HWISI) is 47.1.  The indices indicate that Typhoon Nock-ten is capable of causing regional significant wind damage.

Typhoon Nock-ten will be moving through an atmospheric and oceanic environment that is supportive of tropical cyclones.  When the center of Typhoon Nock-ten is over water, it will move across areas where the Sea Surface Temperature is near 29°C.  The upper level winds are weak and there is little vertical wind shear.  At times the center of Typhoon Nock-ten will move over portions of southern Luzon.  Nock-ten will weaken each time the center moves over land.  In addition, if an eyewall replacement cycle occurs, the strongest winds will slow as the inner eyewall decays.  However, the broader outer eyewall will cause Nock-ten to retain typhoon intensity for a longer period of time.

A subtropical ridge to the north of Nock-ten is steering the typhoon toward the west and that general motion is expected to continue.  On its anticipated track the center of Typhoon Nock-ten will pass near Naga, Calauag, Lucena, San Pablo,  and Manila in southern Luzon.

Typhoon Nock-ten is capable of doing significant wind damage.  Wind blowing water toward the coast will also create significant storm surges in east facing bays and inlets as the center of Nock-ten approaches.  When the center of circulation moves past parts of southern Luzon, the wind will shift to a southwesterly direction and there will be storms surges in in westerly facing bays and inlets.  Typhoon Nock-ten will produce very heavy rain over parts of southern Luzon.  Serious flooding and mudslides could occur in areas with steeper slopes.

Dangerous Typhoon Nock-ten Threatens the Philippines

Dangerous Typhoon Nock-ten intensified to super typhoon status on Saturday and it posed a significant threat to the northern Philippines.  At 10:00 a.m. EST on Saturday the center of Typhoon Nock-ten was located at latitude 13.5°N and longitude 127.1°E which put it about 440 miles (715 km) east of Manila, Philippines.  Nock-ten was moving toward the west at 8 m.p.h. (13 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. (290 km/h).  The minimum surface pressure was 928 mb.

Typhoon Nock-ten is a very strong, well organized typhoon.  Nock-ten has a small eye surrounded by a ring of strong thunderstorms.  A rainband is wrapping around the eye and concentric eyewalls could be forming.  Additional rainbands are rotating around the core of the circulation.  Winds to typhoon force extend out about 40 miles (65 km) from the center.  Thunderstorms in the core of the typhoon are generating strong upper level divergence which is pumping out mass in all directions.

Typhoon Nock-ten is moving through an environment that is favorable for tropical cyclones.  It is moving over water where the Sea Surface Temperature is near 29°C.  The upper level winds are weak and there is little vertical wind shear.  If concentric eyewalls forms, then there could be a period of weakening as the inner eyewall dissipates and the inflow becomes concentrated in the outer eyewall.  Wind speeds could increase again if the outer eyewall starts to contract.  In either case Typhoon Nock-ten will be a dangerous typhoon when it reaches the Philippines

A subtropical ridge to the north of Nock-ten is steering the typhoon toward the west and that general motion is expected to continue.  On its anticipated track Typhoon Nock-ten will reach Catanduanes Island within 24 hours.  Nock-ten is expected to move across southern Luzon.

The Hurricane Intensity Index (HII) is 31.6 and the Hurricane Size Index (HSI) is 15.5.  The Hurricane Wind Intensity Size Index (HWISI) is 47.1.  Those indices indicate that Nock-ten is capable of producing regional significant wind damage.

Typhoon Nock-ten will cause significant wind damage when it moves across the Philippines.  It will also generate a significant storm surge in portions of the coast near the path of the center.  Nock-ten will cause heavy rain and create the potential for floods and mudslides over parts of Catanduanes Island and southern Luzon.

Typhoon Nock-ten Rapidly Intensifies Into Equivalent of a Major Hurricane

Typhoon Nock-ten intensified rapidly into the equivalent of a major hurricane on Friday.  At 10:00 p.m. EST on Friday the center of Typhoon Nock-ten was located at latitude 13.2°N and longitude 128.6°E which put it about 545 miles (880 km) east of Manila, Philippines.  Nock-ten was moving toward the west at 11 m.p.h. (18 km/h).  The maximum sustained wind speed was 125 m.p.h. (205 km/h) and there were wind gusts to 155 m.p.h. (250 km/h).  The minimum surface pressure was 935 mb.

Nock-ten is a very well organized typhoon.  There is an eye with a diameter of 14 miles (23 km) at the center of Typhoon Nock-ten.  The eye is surrounded by a ring of strong thunderstorms.  Additional bands of thunderstorms surround the core of the circulation.  Winds to typhoon force extend out about 40 miles (65 km) from the center.  Thunderstorms around the center are generating strong upper level divergence in all directions.  The divergence is pumping out large amounts of mass which allowed the surface pressure to decrease rapidly.

The Hurricane Intensity Index (HII) is 23.6 and the Hurricane Size Index (HSI) is 15.5.  The Hurricane Wind Intensity Size Index (HWISI) is 39.1.  Those indices indicate that Typhoon Nock-ten is capable of causing major regional wind damage.

Typhoon Nock-ten will continue to move through an environment that is very favorable for intensification.  It is moving over water where the Sea Surface Temperature is near 29°C.  The upper level winds are weak and there is little vertical wind shear.  Nock-ten could intensify more during the next 24 hours and it could become a super typhoon before it reaches the Philippines.

A subtropical ridge to the north of Nock-ten is steering the typhoon toward the west and that general motion is expected to continue.  On its anticipated track Typhoon Nock-ten could be near Catanduanes Island within 36 hours.  Nock-ten is likely to pass across southern Luzon and the center could move close to Manila.  Typhoon Nock-ten will be capable of causing major wind damage.  It will also bring heavy rain and create the potential for floods and mudslides.

Tropical Cyclone Yvette Turns Toward Western Australia

Tropical Cyclone Yvette turned toward western Australia on Friday.  At 1:00 p.m. EST on Friday the center of Tropical Cyclone Yvette was located near latitude 15.1°S and longitude 117.3°E which put it about 370 miles (600 km) north-northwest of Port Headland, Australia.  Yvette was moving toward the east-southeast at 8 m.p.h. (13 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.

An upper level ridge located to the northeast of Yvette is generating strong northeasterly winds which are blowing across the top of the tropical cyclone.  Those winds are creating strong vertical wind shear and for a time the strong upper levels winds sheared the top off of the circulation.  The upper level winds weakened slightly and new thunderstorms developed near the center of Tropical Cyclone Yvette.  The circulation of Yvette is very asymmetrical.  Most of the new thunderstorms are forming west of the center of circulation, although a few storms recently formed east of the center.  The upper level winds are also preventing upper level divergence to the east of Yvette.

Tropical Cyclone Yvette will be moving through an environment that will be only marginally favorable for intensification.  Yvette will move over water where the Sea Surface Temperature is near 29°C.  So, there is enough energy in the upper ocean to support intensification.  However, the strong upper level winds and vertical wind shear will inhibit intensification.  It is possible that the shear could decrease when Yvette moves east and gets closer to the core of the upper level ridge.  If the shear decreases, then some intensification may occur before Yvette reaches western Australia.

A subtropical ridge is steering Tropical Cyclone Yvette toward the east-southeast and that general motion is expected to continue.  On its anticipated track Tropical Cyclone Yvette will reach the coast of Western Australia in about 36 hours.  Landfall will likely occur between Cape Leveque and De Grey.  The highest probability is for a landfall near Bidyadanga.  Tropical Cyclone Yvette will produce locally heavy rain near where the center makes landfall.  Heavy rain could create the potential for flash floods.