Former Tropical Cyclone Mandous Moves over Arabian Sea

The circulation of former Tropical Cyclone Mandous moved over the Arabian Sea on Tuesday. At 1:00 p.m. EST on Tuesday the center of Tropical Cyclone Mandous was located at latitude 12.6°N and longitude 71.8°E which put it about 215 miles (345 km) west of Mangaluru, India. Mandous was moving toward the west at 5 m.p.h. (8 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 1007 mb.

After making landfall on the coast of southeastern India between Puducherry and Chennai on Friday, Tropical Cyclone Mandous moved westward across southern India during the weekend. The circulation of former Tropical Cyclone Mandous emerged over the Arabian Sea west of India on Tuesday. The circulation around Mandous was still well organized. Bands of showers and thunderstorms were revolving around the center of circulation. Storms near the center generated upper level divergence that pumped mass away to the north and west of the former tropical cyclone.

Former Tropical Cyclone Mandous will move through an environment somewhat favorable for intensification during the next 24 hours. Mandous will move over water where the Sea Surface Temperatures are near 28˚C. It will move under the northwestern part of an upper level ridge over southern Asia and the Arabian Sea. The ridge will produce northwesterly winds will blow toward the top of Mandous’ circulation. Those wind will cause some vertical wind shear, but the wind shear will not be strong enough to prevent intensification. Former Tropical Cyclone Mandous could strengthen during the next 24 hours. Northeasterly winds in the lower levels are transporting drier air from Asia over the western Arabian Sea. Mandous is likely to weaken when it reaches the mass of drier air later this week.

Former Tropical Cyclone Mandous will move south of a high pressure system over southern Asia and the northern Arabian Sea. The high pressure system will steer Mandous toward the west during the next several days. On its anticipated track, former Tropical Cyclone Mandous will move farther away from the coast of southwest India.

Pakhar Weakens to a Tropical Depression

Former Tropical Storm Pakhar weakened to a tropical depression over the Western North Pacific Ocean northeast of the Philippines on Monday. At 4:00 p.m. EST on Monday the center of Tropical Depression Pakhar was located at latitude 19.3°N and longitude 131.1°E which put it about 745 miles (1205 km) east-northeast of Manila, Philippines. Pakhar was moving toward the southeast at 7 m.p.h. (21 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 1003 mb.

After strengthening on Sunday, former Tropical Storm Pakhar weakened to a tropical depression on Monday. An upper level trough west of Japan produced strong southwesterly winds that blew across the top of Pakhar’s circulation. Those winds caused strong vertical wind shear and they blew the top of former Tropical Storm Pakhar away to the northeast of the lower level circulation. The circulation around Tropical Depression Pakhar on Monday afternoon consisted of a swirl of showers and lower clouds. Any clouds that grew higher into the atmosphere were quickly sheared apart by the strong upper level winds.

The circulation around Tropical Depression Pakhar will spin down gradually during the next 24 hours. Pakhar will move over water where the Sea Surface Temperatures are near 28˚C. However, the upper level trough west of Japan will continue to cause strong vertical wind shear. The wind shear will prevent the development of new thunderstorms around Tropical Depression Pakhar.

Since the circulation around Tropical Depression Pakhar only exists in the lower levels of the atmosphere, it will be steered by the winds near the surface. Northeasterly winds will push Pakhar back toward the southwest. On its anticipated track, the circulation around Tropical Depression Pakhar should dissipate east of the Philippines during the next 48 hours.

Tropical Storm Pakhar Develops Northeast of the Philippines

Tropical Storm Pakhar developed over the Western North Pacific Ocean northeast of the Philippines on Sunday. At 10:00 a.m. EST on Sunday the center of Tropical Storm Pakhar was located at latitude 18.5°N and longitude 127.5°E which put it about 470 miles (755 km) east-northeast of Manila, Philippines. Pakhar was moving toward the northeast at 13 m.p.h. (20 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 997 mb.

The circulation around a low pressure system northeast of the Philippines strengthened on Sunday and the Japan Meteorological Agency designated the system as Tropical Storm Pakhar. More thunderstorms developed near the center of Pakhar’s circulation. Bands of showers and thunderstorms were revolving around the center of Tropical Storm Pakhar. Storms near the center of Pakhar generated upper level divergence that pumped mass away to the northeast of the tropical storm. Winds to tropical storm force extended out 100 miles (160 km) from the center of circulation.

Tropical Storm Pakhar will move through an environment favorable for intensification during the next 18 hours. Pakhar will move over water where the Sea Surface Temperatures are near 28˚C. An upper level trough east of China will produce southwesterly winds that will blow toward the top of Pakhar’s circulation. Those winds will cause moderate vertical wind shear. The wind shear will inhibit intensification, but Tropical Storm Pakhar could strengthen during the next 18 hours. The upper level trough will move closer to Pakhar on Monday and the upper level winds will get stronger. More vertical wind shear will cause Tropical Storm Pakhar to weaken early next week.

The upper level trough over eastern China will steer Tropical Storm Pakhar toward the northeast during the next 24 hours. On its anticipated track, Pakhar will move farther away from the Philippines. When the vertical wind shear increases on Monday, strong upper level winds could blow the top off of Tropical Storm Pakhar. If that happens, then Pakhar will be steered by winds in the lower levels of the atmosphere. Those winds could steer Pakhar back toward the southwest early next week.

Tropical Cyclone Mandous Makes Landfall in Southern India

Tropical Cyclone Mandous made landfall in southern India on Friday. At 4:00 p.m. EST on Friday the center of Tropical Cyclone Mandous was located at latitude 12.8°N and longitude 80.4°E which put it about 150 miles (240 km) southwest of Chennai, India. Mandous 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 1000 mb.

The center of Tropical Cyclone Mandous made landfall on the coast of southern India between Chennai and Puducherry on Friday. Mandous moved into a mass of drier air and weakened prior to landfall. Tropical Cyclone Mandous was the equivalent of a tropical storm at the time of landfall. Winds to tropical storm force extended out 70 miles (110 km) from the center of Mandous’ circulation. The heaviest rain was falling in bands in the western half of Tropical Cyclone Mandous.

Tropical Cyclone Mandous will move around the southern side of a high pressure system over southern Asia. The high pressure system will steer Mandous toward the west-northwest during the next 24 hours. On its anticipated track, Tropical Cyclone Mandous move farther inland over southern India during the next 24 hours. Mandous will weaken gradually as it moves farther inland. Tropical Cyclone Mandous will bring gusty winds and locally heavy rain to parts of Puducherry, northern Tamil Nadu and southern Andhra Pradesh. Heavy rain could cause flash floods in some locations.

Tropical Cyclone Mandous Strengthens over Southwest Bay of Bengal

Tropical Cyclone Mandous strengthened over the southwestern Bay of Bengal on Thursday. At 4:00 p.m. EST on Thursday the center of Tropical Cyclone Mandous was located at latitude 10.7°N and longitude 81.9°E which put it about 215 miles (345 km) southeast of Chennai, India. Mandous was moving toward the west-northwest at 9 m.p.h. (15 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 988 mb.

The circulation around Tropical Cyclone Mandous strengthened on Thursday. Even though Mandous was stronger, the distribution of thunderstorms continued to be asymmetrical. Many of the thunderstorms were occurring in bands in the western half of Mandous’ circulation. Bands in the eastern half of Mandous consisted primarily of showers and lower clouds. Storms west of the center of Mandous generated upper level divergence that pumped mass away to the west of the tropical cyclone. Winds to tropical storm force extended out 150 miles (240 km) from the center of Tropical Cyclone Mandous.

Tropical Cyclone Mandous will move through an environment that will become unfavorable for intensification during the next 24 hours. Mandous will move over water where the Sea Surface Temperatures are near 28˚C. It will move under the southwestern part of an upper level ridge over Southeast Asia and the Bay of Bengal. The ridge will produce easterly winds that will blow toward the top of Mandous’ circulation. Those winds will cause moderate vertical wind shear. The wind shear is already contributing to the asymmetrical distribution of thunderstorms and the shear will inhibit intensification. The western side Tropical Cyclone Mandous will interact with a mass of drier air over India, when Mandous gets closer to the coast of India. A combination of moderate vertical wind shear and drier air is likely to cause Mandous to begin to weaken during the next 24 hours.

Tropical Cyclone Mandous will move around the southern side of a high pressure system over southern Asia. The high pressure system will steer Mandous toward the northwest during the next 24 hours. On its anticipated track, Tropical Cyclone Mandous will be near the coast of southern India near Chennai in 24 hours. Mandous will bring gusty winds and locally heavy rain to Puducherry, northern Tamil Nadu and southern Andhra Pradesh. Tropical Cyclone Mandous will also drop heavy rain over northern Sri Lanka. Heavy rain could cause flash floods in some locations.

Tropical Cyclone Mandous Forms over Southwest Bay of Bengal

Tropical Cyclone Mandous formed over the southwestern Bay of Bengal east of Sri Lanka on Wednesday afternoon. At 10:00 p.m. EST on Wednesday the center of Tropical Cyclone Mandous was located at latitude 9.6°N and longitude 83.8°E which put it about 360 miles (580 km) southeast of Chennai, India. Mandous was moving toward the west-northwest at 6 m.p.h. (10 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 997 mb.

The circulation around a low pressure system over the southwestern Bay of Bengal strengthened on Wednesday afternoon and the India Meteorological Department designated the system as Tropical Cyclone Mandous. The distribution of thunderstorms around Tropical Cyclone Mandous was asymmetrical. Many of the thunderstorms were occurring in bands in the western half of Mandous’ circulation. Bands in the eastern half of Mandous consisted primarily of showers and lower clouds. Storms west of the center of Mandous generated upper level divergence that pumped mass away to the west of the tropical cyclone. Winds to tropical storm force extended out 85 miles (135 km) from the center of Tropical Cyclone Mandous.

Tropical Cyclone Mandous will move through an environment somewhat favorable for intensification during the next 24 hours. Mandous will move over water where the Sea Surface Temperatures are near 28˚C. It will move under the southwestern part of an upper level ridge over Southeast Asia and the Bay of Bengal. The ridge will produce easterly winds that will blow toward the top of Mandous’ circulation. Those winds will cause moderate vertical wind shear. The wind shear is contributing to the asymmetrical distribution of thunderstorms and the shear will inhibit intensification. The vertical wind shear may not be strong enough to prevent intensification during the next 24 hours and Tropical Cyclone Mandous could strengthen during that time period.

Tropical Cyclone Mandous will move around the southern side of a high pressure system over southern Asia. The high pressure system will steer Mandous toward the northwest during the next 48 hours. On its anticipated track, Tropical Cyclone Mandous could be near the coast of southern India near Chennai in 48 hours. Mandous could bring gusty winds and locally heavy rain to Puducherry, northern Tamil Nadu and southern Andhra Pradesh. Heavy rain could cause flash floods in some locations.

Possible Subtropical Development Southeast of Bermuda

A low pressure system southeast of Bermuda could develop into a subtropical storm during the next few days. At 9:00 a.m. EST on Monday the center of the low pressure system was located at latitude 24.0°N and longitude 55.0°W which put it about 855 miles (1380 km) southeast of Bermuda. The low pressure system was moving toward the north at 5 m.p.h. (8 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 1005 mb.

A low pressure system southeast of Bermuda has the potential to develop into a subtropical storm this week. There is already a strong surface circulation around the low pressure system. The surface low pressure system is located northeast of an upper level low. Bands of showers and thunderstorms were occurring in the northern and eastern parts of the surface low pressure system. Bands in the southern and western parts of the surface low consisted primarily of showers and lower clouds.

The low pressure system southeast of Bermuda will move through an environment somewhat favorable for the development of a subtropical storm during the next 48 hours. The low pressure system will move over water where the Sea Surface Temperatures are near 26˚C. It will move under the northeastern part of an upper level low. The upper level low will produce southeasterly winds that will blow across the top of the surface low. Those winds will cause some vertical wind shear. The vertical wind shear will likely make the environment unfavorable for the development of a tropical storm. However, the wind shear may be weak enough to allow for the surface low to make a transition to a subtropical storm. The National Hurricane Center is indicating there is a probability of 40% that the surface low pressure system develops into a subtropical storm during the next five days.

The upper low will steer the surface low pressure system slowly toward the northwest during the next 48 hours. On its anticipated track the surface low pressure system will remain far to the southeast of Bermuda.

Tropical Storm Yamaneko Moves North of Wake Island

Tropical Storm Yamaneko moved north of Wake Island on Sunday. At 4:00 p.m. EST on Sunday the center of Tropical Storm Yamaneko was located at latitude 23.4°N and longitude 166.0°E which put it about 245 miles (395 km) north of Wake Island. Yamaneko was moving toward the north at 7 m.p.h. (11 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 1000 mb.

Tropical Storm Yamaneko moved farther north of Wake Island on Sunday. The distribution of thunderstorms in Yamaneko was asymmetrical. Thunderstorms were occurring in bands in the far eastern part of Tropical Storm Yamaneko. Bands in the rest of Yamaneko’s circulation consisted primarily of showers and lower clouds. An upper level trough southeast of Japan was producing strong southwesterly winds that were blowing across the top of Tropical Storm Yamaneko. Those winds were causing strong vertical wind shear. The strong vertical wind shear was causing the upper part of Yamaneko’s circulation to tilt toward the northeast. The strong upper level winds were also blowing off the tops of thunderstorms that started to form near the center of Yamaneko and in the western part of the circulation.

Tropical Storm Yamaneko will move through an environment that will cause it to make a transition to an extratropical cyclone during the next 36 hours. Yamaneko will move over water where the Sea Surface Temperatures are colder than 26˚C. The upper level trough southeast of Japan will continue to cause strong vertical wind shear. A combination of cooler water and strong vertical wind shear will cause Tropical Storm Yamaneko to make a transition to an extratropical cyclone.

The upper level trough will steer Tropical Storm Yamaneko toward the north-northeast during the next 36 hours. On its anticipated track, Tropical Storm Yamaneko will pass far to the west of Midway Island in 24 hours.

Tropical Storm Yamaneko Forms Northwest of Wake Island

Tropical Storm Yamaneko formed over the Western North Pacific Ocean northwest of Wake Island on Saturday afternoon. At 4:00 p.m. EST on Saturday the center of Tropical Storm Yamaneko was located at latitude 22.0°N and longitude 165.7°E which put it about 180 miles (295 km) north-northwest of Wake Island. Yamaneko was moving toward the north-northeast at 7 m.p.h. (11 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 1000 mb.

An area of low pressure over the Western North Pacific Ocean northwest of Wake Island strengthened on Saturday afternoon and the Japan Meteorological Agency designated the system as Tropical Storm Yamaneko. Thunderstorms near the center of circulation generated upper level divergence that pumped mass away to the east of the tropical storm. The inner end of a rainband wrapped around the northern and western side of the center of Yamaneko’s circulation. Other bands of thunderstorms were in the eastern half of Tropical Storm Yamaneko. Many of the bands in the western side of Yamaneko consisted primarily of showers and lower clouds. Winds to tropical storm force extended out 130 miles (210 km) in the eastern side of Tropical Storm Yamaneko. The winds in the western side of Yamaneko were blowing at less than tropical storm force.

Tropical Storm Yamaneko will move through an environment somewhat favorable for intensification during the next 24 hours. Yamaneko will move over water where the Sea Surface Temperatures are near 27˚C. An upper level trough southeast of Japan will produce southwesterly winds that will blow toward the top of Yamaneko’s circulation. Those winds will cause some vertical wind shear. The wind shear will inhibit intensification, but the shear will not be enough to prevent Yamaneko from getting a little stronger. Tropical Storm Yamaneko is likely to intensify gradually during the next 24 hours.

The upper level trough southeast of Japan will steer Tropical Storm Yamaneko toward the north during the next 24 hours. On its anticipated track, Tropical Storm Yamaneko will move farther away from Wake Island.

Tropical Depression Nicole Drops Heavy Rain over Southeast U.S.

Tropical Depression Nicole dropped heavy rain over parts of the southeastern U.S. on Friday morning. At 10:00 a.m. EST on Friday the center of Tropical Depression Nicole was located at latitude 34.2°N and longitude 84.3°W which put it about 35 miles (55 km) north of Atlanta, Georgia. Nicole was moving toward the north-northeast at 23 m.p.h. (37 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 1001 mb.

Tropical Storm Nicole dropped heavy rain over parts of the southeastern U.S. on Friday morning. Heavy rain was falling over eastern Tennessee and eastern Kentucky. Bands in the far eastern side of Nicole’s circulation contained thunderstorms that were dropping heavy rain over parts of eastern South Carolina, eastern North Carolina and southeastern Virginia. Easterly winds blowing around the northern side of Nicole’s circulation were enhancing convergence and rising motion ahead of a cold front moving toward the eastern U.S. The enhanced convergence and rising motion was contributing to rain that was falling in the region from Delaware to Ohio.

The cold front approaching the eastern U.S. and an upper level trough over the central U.S. will steer Tropical Depression Nicole quickly toward the north-northeast during Friday. On its anticipated track the center of Tropical Depression Nicole will be over West Virginia by Friday evening. Heavy rain falling over parts of the southeastern U.S. and Appalachians could cause flooding. Flood Watches were in effect for parts of northern South Carolina, western North Carolina and southern Virginia. There could be enough low level wind shear for tornadoes to develop in the bands on the far eastern side of the circulation around Tropical Depression Nicole. A Tornado Watch was in effect for eastern South Carolina, eastern North Carolina and southeastern Virginia.