Tag Archives: Solomon Islands

Tropical Cyclone Jasper Intensifies to Equivalent of Hurricane/Typhoon

Tropical Cyclone Jasper intensified to the equivalent of a hurricane/typhoon over the Coral Sea on Tuesday. At 10:00 p.m. EST on Tuesday the center of Tropical Cyclone Jasper was located at latitude 11.0°S and longitude 157.3°E which put it about 205 miles (330 km) west-southwest of Honiara, Guadacanal. Jasper was moving toward the south-southwest at 9 m.p.h. (15 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 982 mb.

Tropical Cyclone Jasper rapidly intensified to the equivalent of a hurricane/typhoon over the Coral Sea on Tuesday. The inner end of a rainband wrapped around the center of Jasper’s circulation. An eye was visible on satellite images at the center of Tropical Cyclone Jasper. A thin ring of thunderstorms surrounded the eye and the strongest winds were occurring in that ring of storms. Bands of showers and thunderstorms were revolving around the center of Jasper’s circulation. Storms near the center generated upper level divergence that pumped mass away from the tropical cyclone. The removal of mass was causing the surface pressure to decrease.

Winds to hurricane/typhoon force extended out 10 miles (15 km) from the center of Tropical Cyclone Jasper. Winds to tropical storm force extended out 115 miles (185 km) from the center of Jasper’s circulation.

Tropical Cyclone Jasper will move through an environment very favorable for intensification during the next 36 hours. Jasper will move over water where the Sea Surface Temperatures are near 29°C. It will move under the western part of the axis of an upper level ridge over the South Pacific Ocean. The upper level winds are ridge weak near the axis of the ridge and there will be little vertical wind shear. Tropical Cyclone Jasper will intensify during the next 36 hours. Jasper could intensify rapidly after the eye and eyewall are fully developed. Tropical Cyclone Jasper will very likely strengthen to the equivalent of a major hurricane.

Tropical Cyclone Jasper will move around the northwestern part of a high pressure system over the South Pacific Ocean. The high pressure system will steer Jasper toward the southwest during the next 36 hours. On its anticipated track, Jasper will move away from the Solomon Islands. Tropical Cyclone Jasper will continue to produce gusty winds and locally heavy rain in the Solomon Islands until it moves away. Heavy rain could cause flash floods in some locations. Tropical Cyclone Jasper could approach the coast of Queensland, Australia in a few days.

Tropical Cyclone Jasper Forms Near the Solomon Islands

Tropical Cyclone Jasper formed over the Coral Sea near the Solomon Islands on Monday night. At 4:00 a.m. EST on Tuesday the center of Tropical Cyclone Jasper was located at latitude 9.6°S and longitude 156.6°E which put it about 230 miles (370 km) west of Honiara, Guadacanal. Jasper was moving toward the west at 7 m.p.h. (11 km/h). The maximum sustained wind speed was 45 m.p.h. (75 km/h) and there were wind gusts to 60 m.p.h. (95 km/h). The minimum surface pressure was 996 mb.

A low pressure system over the Coral Sea near the Solomon Islands strengthened during Monday night and the Australian Bureau of Meteorology designated the system as Tropical Cyclone Jasper. The circulation around Tropical Cyclone Jasper was organizing rapidly. Bands of showers and thunderstorms were revolving around the center of Jasper’s circulation. Storms near the center generated upper level divergence that pumped mass away from the tropical cyclone. The removal of mass was causing the surface pressure to decrease.

Winds to tropical storm force extended out 100 miles (160 km) in the western side of Tropical Cyclone Jasper. Winds to tropical storm force extended out 45 miles (75 km) in the eastern side of Jasper’s circulation.

Tropical Cyclone Jasper will move through an environment favorable for intensification during the next 36 hours. Jasper will move over water where the Sea Surface Temperatures are near 29°C. It will move under the western part of the axis of an upper level ridge over the South Pacific Ocean. The upper level winds are ridge weak near the axis of the ridge and there will be little vertical wind shear. Tropical Cyclone Jasper will intensify during the next 36 hours. Jasper will strengthen to the equivalent of a hurricane/typhoon. Tropical Cyclone Jasper could intensify rapidly once an inner core with an eye and an eyewall develop.

Tropical Cyclone Jasper will move around the northwestern part of a high pressure system over the South Pacific Ocean. The high pressure system will steer Jasper toward the southwest during the next 36 hours. On its anticipated track, Jasper will move away from the Solomon Islands. Tropical Cyclone Jasper will continue to produce gusty winds and locally heavy rain in the Solomon Islands until it moves away. Heavy rain could cause flash floods in some locations. Tropical Cyclone Jasper could approach the coast of Queensland, Australia in a few days.

Tropical Cyclone Forming over Solomon Islands

A tropical cyclone is forming over the Solomon Islands. The system is currently designated as Invest 92P by the U.S. Joint Typhoon Warning Center. At 1:00 a.m. EST on Monday the center of Invest 92P was located at latitude 8.7°S and longitude 158.3°E which put it about 130 miles (210 km) west-northwest of Honiara, Guadacanal. Invest 92P was moving toward the southwest at 8 m.p.h. (13 km/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 1002 mb.

A low pressure system over the Solomon Islands was gradually becoming better organized on Monday morning. The U.S. Joint Typhoon Warning Center was designating the system as Invest 92P. The Australian Bureau of Meteorology classified the system as a tropical low. Bands of showers and thunderstorms were revolving around the center of the low pressure system. Storms near the center generated upper level divergence that pumped mass away from the low pressure system. The removal of mass was causing the surface pressure to decrease.

The low pressure system will move through an environment favorable for the development of a tropical cyclone during the next 36 hours. The low pressure system will move over water where the Sea Surface Temperatures are near 29°C. It will move under the western part of an upper level ridge over the South Pacific Ocean. The upper level ridge will produce northerly winds that will blow toward the top of the low pressure system. Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification. Invest 92P is very likely to develop into a tropical cyclone during the next 36 hours.

The low pressure system will move around the northwestern part of a high pressure system over the South Pacific Ocean. The high pressure system will steer Invest 92P toward the southwest during the next 36 hours. On its anticipated track, the low pressure system will move away from the Solomon Islands and over the Coral Sea. Invest 92P will continue to produce gusty winds and locally heavy rain in the Solomon Islands until it moves away. Heavy rain could cause flash floods in some locations.

Tropical Cyclone Forms over Coral Sea

Tropical Cyclone 03P formed over the Coral Sea southwest of the Solomon Islands on Saturday. At 4:00 p.m. EST on Saturday the center of Tropical Cyclone 03P was located at latitude 13.2°S and longitude 157.1°E which put it about 650 miles (1050 km) northwest of Poum, New Caledonia. Tropical Cyclone 03P was moving toward the south-southeast at 16 m.p.h. (26 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 997 mb.

The circulation around a small low pressure system over the Coral Sea strengthened on Saturday into Tropical Cyclone 03P. More thunderstorms formed near the center of the tropical cyclone. Thunderstorms also became more numerous in bands revolving around the center of circulation. Storms near the center generated upper level divergence that pumped mass away from the tropical cyclone. The circulation around the tropical cyclone was small. Winds to tropical storm force extended out 20 miles (30 km) from the center of circulation.

Tropical Cyclone 03P will move through an environment favorable for intensification during the next 36 hours. The tropical cyclone 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 over the South Pacific Ocean. The ridge will produce northwesterly winds that will blow toward the top of the tropical cyclone’s circulation. Those winds will cause some vertical wind shear, but the wind shear will be too small to prevent intensification. Tropical Cyclone 03P will intensify and it could strengthen to the equivalent of a hurricane/typhoon within 36 hours.

Tropical Cyclone 03P will move around the southwestern part of a high pressure system over the South Pacific Ocean during the next several days. The high pressure system will steer the tropical cyclone toward the southeast during the next 36 hours. On its anticipated track Tropical Cyclone 03P could approach the northwestern part of New Caledonia in 48 hours. The tropical cyclone is likely to be the equivalent of a hurricane/typhoon when it nears New Caledonia.

Tropical Cyclone Harold Drops Heavy Rain on Guadalcanal

Tropical Cyclone Harold dropped heavy rain over Guadalcanal and San Cristobal on Thursday night.  At 11:00 p.m. EDT on Thursday the center of Tropical Cyclone Harold was located at latitude 10.8°S and longitude 162.1°E which put it about 10 miles (15 km) east of Hauraha, Solomon Islands.  Harold was moving toward the east-southeast at 25 m.p.h. (40 km/h).  The maximum sustained wind speed was 45 m.p.h. (75 km/h) and there were wind gusts to 60 m.p.h. (95 km/h).  The minimum surface pressure was 995 mb.

The center of Tropical Cyclone Harold passed near Guadalcanal and San Cristobal on Thursday night.  The circulation around Harold was gradually becoming more organized.  Multiple bands of showers and thunderstorms were revolving around the center of Tropical Cyclone Harold.  Storms near the center of circulation were generating upper level divergence which was pumping mass away from the tropical cyclone.  Winds to tropical storm force extended out 90 miles (150 km) from the center.

Tropical Cyclone Harold will move through an environment favorable for intensification during the next several days.  Harold will move over water where the Sea Surface Temperature is near 30°C.  It will move under the southwestern portion of an upper level ridge over the South Pacific Ocean.  The ridge will produce northwesterly winds which will blow toward the top of Tropical Cyclone Harold.  Those winds will create some vertical wind shear, but the shear will not be strong enough to prevent intensification.  Tropical Storm Harold will continue to intensify and it will strengthen to the equivalent of a hurricane/typhoon.

The upper level ridge will steer Tropical Cyclone Harold toward the southeast.  On its anticipated track Harold will move away from the Solomon Islands on Friday and the weather should improve there.  Tropical Cyclone Harold could approach Vanuatu in 36 hours  and it could be he equivalent of a hurricane/typhoon at that time.

Tropical Cyclone Raquel Reorganizing Near Solomon Islands

Strong upper level winds blew away the upper potion of Tropical Cyclone Raquel on Wednesday.  However, the upper level winds lessened on Thursday and thunderstorms began to reform on the western side of the circulation.  At 5:00 p.m. EDT on Thursday the center of Tropical Cyclone Raquel was located at latitude 6.4°S and longitude 160.5°E which put it about 220 miles (360 km) north of Honiara in the Solomon Islands.  Raquel was moving toward the south-southeast 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 50 m.p.h. (80 km/h).  The minimum surface pressure was 994 mb.

Tropical Cyclone Raquel is over water where the Sea Surface Temperatures are very warm.  However, an upper level ridge east of Raquel generated strong winds over the top of the tropical cyclone on Wednesday and blew away the upper parts of the circulation.  The upper level winds weakened on Thursday and new thunderstorms began to develop west of the center of circulation.  Upper level divergence is also occurring in the western half of the circulation and Raquel looks like a tropical cyclone again.  The upper level winds are still strong enough to inhibit intensification, but Raquel could strengthen further in the short term.

When the top parts of the circulation were blown away on Wednesday, the lower level circulation was steered by winds in the lower troposphere and it moved toward the northeast.  As the thunderstorms redevelop, the height of the circulation is increasing and Raquel is more likely to be steered by winds in the middle troposphere.  Those winds are expected to steer Raquel back toward the southwest.  On its anticipated track Raquel could again approach Santa Isabel Island on Friday.  It could bring winds and locally heavy rain to portions of the Central Solomon Islands.

Tropical Cyclone Raquel Forms Near the Solomon Islands

A distinct low level center of circulation was detected inside a large area of thunderstorms north of the Solomon Islands and the system was designated as Tropical Cyclone Raquel (25P).  At 11:00 p.m. EDT on Tuesday the center of Tropical Cyclone Raquel was located at latitude 6.5°S and longitude 158.9°E which put it about 210 miles (335 km) north of Honiara in the Solomon Islands.  Raquel was moving toward the southwest 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 989 mb.

Raquel is over water where the Sea Surface Temperature is quite warm and there is plenty of energy in the upper ocean to support intensification.  However, and upper level ridge east of Raquel is northeasterly winds over the top of the circulation and it is creating moderate amounts of vertical wind shear.  The wind shear is causing many of the stronger thunderstorms to occur on the western side of the circulation.  The wind shear may be tilting the vertical structure of the circulation toward the southwest and it is limiting the potential for intensification.

As Raquel moves around the western end of the upper level ridge, it is expected to be steered toward the south on Wednesday.  On its anticipated track Raquel is expected to move across Santa Isabel on Wednesday.  It could be near Guadacanal in 36 to 48 hours.  Raquel is likely to bring some wind and locally heavy rain to parts of the central Solomon Islands during the next two days.