Tag Archives: 15W

Lingling Strengthens to Typhoon South of Ryukyu Islands

Former Tropical Storm Lingling strengthened to a typhoon south of the Ryukyu Islands on Tuesday.  At 11:00 a.m. EDT on Tuesday the center of Typhoon Lingling was located at latitude 21.7°N and longitude 124.3°E which put it about 180 miles (295 km) south of Ishigaki, Japan.  Lingling was moving toward the north 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 979 mb.

Typhoon Lingling exhibited much greater organization on Tuesday.  A circular eye with a diameter of 30 miles (50 km) developed at the center of circulation.  The eye was surrounded by a ring of strong thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Typhoon Lingling.  The strongest rainbands were occurring in the southeastern half of the circulation.  Storms near the core of Lingling were generating upper level divergence which was pumping mass away from the typhoon.  Winds to typhoon force extended out about 30 miles from the center of circulation.  Winds to tropical storm force extended out about 140 miles (220 km) from the center.

Typhoon Lingling will move through an environment favorable for intensification during the next 24 to 48 hours.  Lingling will move over water where the Sea Surface Temperature is near 28°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Typhoon Lingling is likely to continue to intensify and it could strengthen into the equivalent of a major hurricane in a couple of days.

Typhoon Lingling is moving around the western end of a large subtropical ridge over the Western North Pacific Ocean.  The ridge will steer Lingling toward the north during the next several days.  On its anticipated track Typhoon Lingling could reach the southern Ryukyu Islands within 24 hours.  Lingling will bring strong, gusty winds and heavy rain to those islands.  Typhoon Lingling could approach Kyushu and South Korea in about three days.

Elsewhere over the Western North Pacific Ocean, Tropical Depression Kajiki was dropping heavy rain over parts of Vietnam and Laos.  At 11:00 a.m. EDT on Tuesday the center of Tropical Depression Kajiki was located at latitude 16.4°N and longitude 107.3°E which put it about 65 miles (105 km) west-northwest of Da Nang, Vietnam.  Kajiki was moving toward the west at 8 m.p.h. (13 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 998 mb.

Tropical Storm Kajiki Forms Near Vietnam

Tropical Storm Kajiki formed near the coast of Vietnam on Monday.  At 5:00 p.m. EDT on Sunday the center of Tropical Storm Kajiki was located at latitude 16.6°N and longitude 107.6°E which put it about 50 miles (80 km) northeast of Vinh Linh, Vietnam.  Kajiki was moving toward the southwest 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 996 mb.

The wind speed around a low pressure system just east of the coast of Vietnam increased to 40 m.p.h. (65 km/h) on Monday and the Japan Meteorological Agency designated the system as Tropical Storm Kajiki.  The distribution of thunderstorms around Kajiki was asymmetrical.  Many of the stronger thunderstorms were occurring in bands in the western half of the circulation.  Bands in the eastern half of Tropical Storm Kajiki contained fewer thunderstorms.  Kajiki was moving south of an upper level ridge over eastern Asia.  The ridge was producing northeasterly winds which were blowing toward the top of the tropical storm.  Those winds were causing moderate vertical wind shear and they were the reason for the asymmetrical distribution of thunderstorms.

The upper level ridge will steer Tropical Storm Kajiki toward the southwest during the next 12 to 24 hours.  On it anticipated track Kajiki will reach the coast of Vietnam within 12 hours.  Even though Tropical Storm Kajiki will move over water where the Sea Surface Temperature is near 30°C, it will have only a few hours to strengthen before the center reaches the coast.  Kajiki will bring some gusty winds to the coast, but the greater risk is for heavy rain.  Tropical Storm Kajiki will drop locally heavy rain over parts of central Vietnam and northern Laos.  Heavy rain could cause flash floods in some locations.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Lingling was strengthening as it north toward the southern Ryukyu Islands.  At 5:00 p.m. EDT on Sunday the center of Tropical Storm Lingling was located at latitude 19.5°N and longitude 124.1°E which put it about 565 miles (915 km) south-southwest of Okinawa.  Lingling was moving toward the north-northwest at 13 m.p.h. (20 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 994 mb.  Tropical Storm Lingling is forecast to strengthen into a typhoon before it reaches the southern Ryukyu Islands.

Tropical Storm Lingling Forms East of Luzon

Tropical Storm Lingling formed east of Luzon on Sunday night.  At 11:00 p.m. EDT on Sunday the center of Tropical Storm Lingling was located at latitude 15.1°N and longitude 126.1°E which put it about 300 miles (485 km) east of Luzon.  Lingling was moving toward the northwest at 14 m.p.h. (22 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.

A distinct center of circulation developed in an area of thunderstorms east of Luzon on Sunday night and the Japan Meteorological Agency designated the system as Tropical Storm Lingling.  The circulation around Tropical Storm Lingling was still organizing.  Bands of showers and thunderstorms were forming around the center of circulation.  Storms around the center of circulation were starting to generate upper level divergence.

Tropical Storm Lingling will move through an environment favorable for intensification.  Lingling will move over water where the Sea Surface Temperature is near 29°C.  It will move near the western end of an upper level ridge.  The ridge will produce southerly winds which will blow toward the top of the circulation.  Those winds will cause some vertical wind shear, but the shear will not be strong enough to prevent intensification.  Tropical Storm Lingling will intensify and it could strengthen into a typhoon in a few days.

Tropical Storm Lingling will move around the western end of a subtropical ridge over the Western North Pacific Ocean.  The ridge will steer Lingling toward the north-northwest.  On its anticipated track the center of Tropical Storm Lingling will remain east of Luzon.  Lingling will approach Taiwan and the southern Ryukyu Islands in about 36 hours.

Tropical Storm Jongdari Makes Landfall South of Shanghai, Shanshan Forms Northeast of Guam

Tropical Storm Jongdari made landfall south of Shanghai on Thursday, while Tropical Storm Shanshan formed northeast of Guam.  At 11:00 p.m. EDT on Thursday the center of Tropical Storm Jongdari was located at latitude 30.7°N and longitude 121.4°E which put it about 40 miles (65 km) south of Shanghai, China.  Jongdari was moving toward the west at 19 m.p.h. (30 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.

The center of Tropical Storm Jongdari made landfall on the east coast of China near Zhoushan and Ningbo on Thursday.  Jongdari retained a distinct low level center of circulation while it made landfall.  The tropical storm brought gusty winds to the coast of Zhejiang and Shanghai Shi provinces.  Tropical Storm Jongdari dropped locally heavy rain over parts of those provinces and some flooding could occur.  The center of Jongdari will move quickly toward Hangzhou and the risk of flooding will continue as the tropical storm moves inland and weakens.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Shanshan formed northeast of Guam.  At 11:00 p.m. EDT on Thursday the center of Tropical Storm Shanshan was located at latitude 17.9°N and longitude 150.1°E which put it about 460 miles (740 km) northeast of Guam.  Shanshan was moving toward the west-southwest 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. (65 km/h).  The minimum surface pressure was 998 mb.

A distinct low level center of circulation formed in a cluster of thunderstorms east of the Northern Marianas on Thursday and the Japan Meteorological Agency designated the system as Tropical Storm Shanshan.  The circulation of Shanshan was still organizing.  Several bands of showers and thunderstorms developed southwest of the center of circulation.  Bands northeast of the center consisted mostly of showers and lower clouds.  Storms near the center of circulation started to generate upper level divergence.

Tropical Storm Shanshan will move through an environment favorable for intensification.  Shanshan will move over water where the Sea Surface Temperature is near 28°C.  It will move through a region where the upper level winds are weak and there will be little vertical wind shear.  Tropical Storm Shanshan will intensify and it could strengthen into a typhoon during the weekend.

Tropical Storm Shashan will move around the western end of a subtropical high pressure system.  The high will steer Shanshan in a general northwesterly direction during the next 12 to 24 hours.  It will turn more toward the north during the weekend.  On its anticipated track Tropical Storm Shanshan will move near the Northern Marianas during the next 24 to 36 hours.

Tropical Storm Jongdari Heads Toward China

Tropical Storm Jongdari headed toward China late on Tuesday.  After dropping heavy rain on parts of Honshu and Kyushu, former Typhoon Jongdari weakened to a tropical storm.  Jongdari then was caught by the circulation of an upper level low south of Japan and the tropical storm made a slow counterclockwise loop south of Kyushu.  Tropical Storm Jongdari completed the loop and moved west toward China on Tuesday.  At 11:00 p.m. EDT on Tuesday the center of Tropical Storm Jongdari was located at latitude 30.0°N and longitude 126.7°E which put it about 360 miles (575 km) east-southeast of Shanghai, China.  Jongdari was moving toward the west at 11 m.p.h. (17 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 990 mb.

Tropical Storm Jongdari moved around the circulation of an upper level low south of Japan on Sunday and Monday.  Strong upper winds rotating around the upper level low caused vertical wind shear which disrupted the upper part of Jongdari’s circulation.  However, the integrity of the lower level circulation remained intact.  There is a well defined low level circulation with bands of showers and thunderstorms revolving around the center of circulation.  Stronger upper level winds have periodically sheared the tops off of the taller thunderstorms.  New thunderstorms were forming near the center of circulation but it is unclear if those storms will persist.

Tropical Storm Jongdari will move through an environment marginally favorable for intensification on Wednesday.  Jongdari will move over water where the Sea Surface Temperature is near 28°C.  However the upper level low south of Japan and an upper level ridge over East Asia will combine to produce strong easterly winds which will blow across the top of the circulation.  Those winds will cause strong vertical wind shear which will inhibit intensification.  Tropical Storm Jongdari could intensify a little during the next 24 hours.

Tropical Storm Jongdari will move south of a high pressure system near East Asia which will steer Jongdari in a general westerly direction.  On its anticipated track Tropical Storm Jongdari could approach the coast of China southeast of Shanghai in about 24 hours.  The center of Jongdari could be near Shanghai in about 36 hours.  Tropical Storm Jongdari will bring some gusty winds, but the greater risk will be locally heavy rainfall.  Heavy rain falling on very moist ground could cause flash floods over parts of eastern China.

Typhoon Jongdari Makes Landfall on Honshu

Typhoon Jongdari made landfall on Honshu near Ise in the Mie Prefecture on Saturday.  The maximum sustained wind speed was 80 m.p.h. (130 km/h) at the time of landfall.  Jongdari weakened to a tropical storm after the center moved over Honshu.  At 5:00 p.m. EDT on Saturday the center of Tropical Storm Jongdari was located at latitude 34.7°N and longitude 135.0°E which put it about 20 miles (30 km) southwest of Kobe, Japan.  Jongdari was moving toward the west-northwest at 25 m.p.h. (40 km/h).  The maximum sustained wind speed was 70 m.p.h. (110 km/h) and there were wind gusts to 85 m.p.h. (135 km/h).  The minimum surface pressure was 980 mb.

The center of Typhoon Jongdari made landfall in the Mie Prefecture on Honshu near Ise and Toba.  Jongdari then moved west-northwest near Matsusaka and Tsu.  It passed near Nara and Osaka before moving to its current position southwest of Kobe.  Typhoon Jongdari brought gusty winds and it dropped locally heavy rain over parts of the Mie, Nara, Shiga, Kyoto, Osaka and Hyogo Prefectures.  The ground in some of those places is very moist from recent rains and flash flooding could occur if more heavy rain falls.  The relatively rapid movement of Tropical Storm Jongdari will help to reduce the amount of rain that falls over specific locations.

Tropical Storm Jongdari will continue to weaken as it moves over western Honshu and northern Kyushu.  Jongdari is moving around the northern side of an upper level low south of Japan.  The upper level low will steer Tropical Storm Jongdari quickly to the west during the next 12 hours.  Jongdari will move southwest on Sunday when it moves around the northwestern part of the upper low.  On its anticipated track Tropical Storm Jongdari will move near Okayama, Hiroshima, Yamaguchi, Kitakyushu and Fukuoka.  The tropical storm will continue to drop locally heavy rain while it weakens over western Japan.

Typhoon Jongdari Turns Toward Honshu

Typhoon Jongdari turned toward Honshu on Friday.  At 5:00 p.m. EDT on Friday the center of Typhoon Jongdari was located at latitude 31.0°N and longitude 143.7°E which put it about 415 miles (665 km) southeast of Tokyo, Japan.  Jongdari was moving toward the north at 24 m.p.h. (39 km/h).  The maximum sustained wind speed was 105 m.p.h. (170 km/h) and there were wind gusts to 125 m.p.h. (205 km/h).  The minimum surface pressure was 957 mb.

An upper level low west of Typhoon Jongdari was affecting the circulation.  Winds blowing around the eastern side of the upper low were cutting under the upper level divergence at the top of the circulation of Jongdari.  In addition, drier flowing around the southern half of the upper low was being pulled into the western side of the circulation of Typhoon Jongdari.  The effects of the upper low were causing the circulation of Typhoon Jongdari to become asymmetrical.  Many of the stronger thunderstorms and stronger winds were occurring in bands in the eastern half of the circulation.  Bands in the western half of the circulation consisted primarily of showers and lower clouds.  With fewer strong thunderstorms in the western part of the typhoon with downdrafts to bring stronger winds to the surface the wind field was also becoming asymmetrical.  Winds to typhoon force extended out about 100 miles (160 km) from the center of circulation on the eastern side of Jongdari, but they only extended out about 50 miles (80 km) on the western side.  Winds to tropical storm force extended out about 230 miles (370 km) to the east of the center, but only extended out about 170 miles (280 km) to the west of the center of circulation.

The upper level low will continue to affect Typhoon Jongdari.  Jongdari will move over water where the Sea Surface Temperature is near 28°C.  So, there will be sufficient energy in the upper ocean to support a strong typhoon.  However, the upper low will inhibit upper level divergence to the west of the circulation.  Upper level divergence will be strong to the southeast of Typhoon Jongdari.  Drier air flowing around the upper low will inhibit the formation of thunderstorms in bands in the southwestern part of the circulation.  Typhoon Jongdari is likely to weaken slowly, although it could maintain its intensity at times as it moves around the northern side of the upper low.

The upper low will also steer Typhoon Jongdari during the weekend.  Jongdari will turn more toward the west-northwest when it moves around the northern part of the upper low.  On its anticipated track Typhoon Jongdari could pass south of Tokyo in about 18 hours.  The center of Jongdari could be very close to Hamamatsu in about 24 hours.  It could make landfall near Matsuzaka in a little over a day.  Typhoon Jongdari could pass very close to Osaka and Kobe and it could pass just south of Kyoto.  Heavy rain fell on parts of Japan earlier this month and Typhoon Jongdari could cause serious flooding in some locations.

Typhoon Jongdari Nears Iwo To

Typhoon Jongdari neared Iwo To on Thursday.  At 11:00 a.m. EDT on Thursday the center of Typhoon Jongdari was located at latitude 24.2°N and longitude 140.5°E which put it about 105 miles (170 km) southwest of Iwo To.  Jongdari was moving toward the northeast at 13 m.p.h. (21 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 975 mb.

Former Tropical Storm Jongdari strengthened as it neared Iwo To on Thursday.  An eye developed at the center of circulation and the Japan Meteorological Agency classified Jongdari as a typhoon.  The eye was surrounded by a ring of strong thunderstorms and the strongest winds were occurring in that ring of storms.  Several bands of showers and thunderstorms were revolving around the core of Jongdari.  Thunderstorms in the core of Jongdari were generating strong upper level divergence which was pumping mass away from the typhoon.  Winds to typhoon force extended out about 20 miles (30 km) from the center of circulation.  Winds to tropical storm force extended out about 130 miles (210 km) from the center.

Typhoon Jongdari will move through an environment favorable for intensification during the next day or two.  Jongdari will move over water where the Sea Surface Temperature is near 28°C.  An upper level low southeast of Honshu will cause easterly winds which will blow over the northern part of the circulation.  Those winds will cause some vertical wind shear, but the shear will be less over the core of the typhoon.  Typhoon Jongdari will strengthen during the next 24 to 48 hours and it could become the equivalent of a major hurricane.

Typhoon Jongdari is moving around the western end of a subtropical ridge over the Western North Pacific and the ridge is steering Jongdari toward the northeast.  A general motion toward the northeast is forecast for the next 12 to 24 hours.  The upper low southeast of Honshu will move slowly toward the west.  When Jongdari moves farther north, it will begin to be steered more by the upper level low.  Typhoon Jongdari is forecast to turn more toward the north on Friday.  Jongdari will start to move toward the northwest in about 36 hours, when it moves northeast of the upper level low.

On its anticipated track Typhoon Jongdari will move over Iwo To in a few hours.  It will bring gusty winds and heavy rain.  Typhoon Jongdari could approach Honshu in about 48 hours and it could cause flooding in addition to strong winds and heavy rain.

Elsewhere over the Western North Pacific, Tropical Storm Wokung was weakening east of northern Japan.  At 11:00 a.m. EDT on Thursday the center of Tropical Storm Wokung was located at latitude 42.2°N and longitude 152.5°E which put it about 600 miles (960 km) east of Misawa, Japan.  Wokung was moving toward the north-northwest at 19 m.p.h. (31 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 995 mb.

Tropical Storm Jongdari Forms Southwest of Iwo To

Tropical Storm Jongdari formed southwest of Iwo To on Tuesday.  At 5:00 p.m. EDT on Tuesday the center of Tropical Storm Jongdari was located at latitude 20.9°N and longitude 136.9°E which put it about 410 miles (665 km) southwest of Iwo To.  Jongdari was moving toward the north 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 996 mb.

A distinct low level center of circulation developed within former Tropical Depression 15W on Tuesday afternoon and the Japan Meteorological Agency designated the system as Tropical Storm Jongdari.  The circulation of Jongdari was asymmetrical.  Most of the stronger thunderstorms were forming in bands north of the center.  Bands south of the center consisted primarily of showers and lower clouds.  Stronger storms near the center were beginning to generate upper level divergence which was pumping mass away from the core of the circulation.

Tropical Storm Jongdari will move through an environment favorable for intensification during the next several days.  Jongdari will move over water where the Sea Surface Temperature is near 28°C.  So, there will be sufficient energy in the upper ocean to support intensification.  It will move under the middle of an upper level ridge where the winds are weaker and there will be little vertical wind shear.  Intensification could be slow at first while the circulation becomes more organized, but Jongdari could strengthen more quickly when the inner core becomes more well developed.  Tropical Storm Jongari could strengthen to a typhoon with 48 hours.  It could eventually intensify into the equivalent of a major hurricane.

Tropical Storm Jongari will move around the western end of a subtropical ridge which will steer Jongari toward the northeast during the next two or three days.  When Jongari moves farther north, it will be affected by a second ridge located farther to the north.  The second ridge is forecast to strengthen and push Jongari more toward the northwest.  On its anticipated track Jongari could reach Iwo To in about 48 hours.  It could be a typhoon at that time.  Jongari could approach Tokyo in about four days and it is likely to be a typhoon when it reaches Honshu.

Elsewhere over the Western North Pacific Ocean, Tropical Storm Wokung was churning well southeast of Japan.  At 5:00 p.m. EDT on Tuesday the center of Tropical Storm Wokung was located at latitude 32.3°N and longitude 158.0°E which put it about 1250 miles (2015 km) east-southeast of Tokyo, Japan.  Wokung was moving toward the north-northwest at 11 m.p.h. (17 km/h).  The maximum sustained wind speed was 60 m.p.h. (95 km/h) and there were wind gusts to 75 m.p.h. (120 km/h).  The minimum surface pressure was 984 mb.

Tropical Storm Wukong Forms Southeast of Japan

Tropical Storm Wukong formed southeast of Japan on Monday.  At 5:00 p.m. EDT on Monday the center of Tropical Storm Wukong was located at latitude 29.0°N and longitude 159.0°E which put it about 1370 miles (2210 km) east-southeast of Tokyo, Japan.  Wukong was moving toward the north at 24 m.p.h. (39 km/h).  The maximum sustained wind speed was 60 m.p.h. (95 km/h) and the were wind gusts to 75 m.p.h. (120 km/h).  The minimum surface pressure was 984 mb.

A cluster of thunderstorms developed southeast of Japan during the weekend and a low level center of circulation formed near the southwestern edge of the cluster of storms.  However, strong upper level winds blowing from the southwest kept blowing the top of the circulation northeast of the low level center and the system was unable to develop.  The upper level winds slowed on Monday and a band of showers and thunderstorms wrapped around the northern and western sides of the center of circulation.  The Japan Meteorological Agency designated the system as Tropical Storm Wukong.

The circulation of Tropical Storm Wukong organized quickly after the upper level winds weakened.   As mentioned above, a primary rainband wrapped around the northern and western sides of the center of circulation.  Storms in the primary rainband generated upper level divergence which was pumping mass away to the north of the tropical storm.  Several other bands of showers and thunderstorms developed in the eastern half of the circulation.  Bands south and west of the center consisted primarily of showers and lower clouds.

Tropical Storm Wukong will move through an environment favorable for intensification during the next day or so.  Wukong will move over water where the Sea Surface Temperature is near 27°C.  Wukong is moving along the eastern portion of an upper level trough.  The trough is producing southwesterly winds which are blowing toward the top of the circulation.  However, those winds weakened on Monday and they will not cause enough vertical wind shear to prevent further intensification.  Tropical Storm Wukong could strengthen into a typhoon during the next 24 to 36 hours.  Eventually, Wukong will move over cooler water and it will begin to weaken.

Tropical Storm Wukong is moving between an upper level trough to the west and an upper level ridge to the east.  The trough and ridge were combining to steer Wukong toward the north and a general northerly motion is expected to continue.  On its anticipated track Tropical Storm Wukong will stay west of the larger islands of Japan.  Wukong could approach the Kuril Islands in about three days.

Elsewhere over the Western North Pacific former Tropical Storm Ampil weakened to a tropical depression over land southeast of Beijing, China, Tropical Storm Son-tinh meandered near the coast of southeastern China and Tropical Depression 15W organized southwest of Iwo To, Japan.  At 5:00 p.m. EDT on Monday the center of Tropical Depression Ampil was located at latitude 38.8°N and longitude 117.6°E which put it about 110 miles (175 km) southeast of Beijing, China.  Ampil was moving toward the north-northwest at 18 m.p.h. (29 km/h).  The maximum sustained wind speed was 35 m.p.h. (55k km/h) and there were wind gusts to 45 m.p.h. (75 km/h).  The minimum surface pressure was 998 mb.  Tropical Depression Ampil was still dropping locally heavy rain over parts of eastern China.

At 5:00 p.m. EDT on Monday the center of Tropical Storm Son-tinh was located at latitude 21.2°N and longitude 109.0°E which put it about 40 miles (65 km) southeast of Beihai, China.  Son-tinh was moving toward the west-northwest at 6 m.p.h. (10 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 996 mb.  Tropical Storm Son-tinh was dropping locally heavy rain over parts of southeastern China and Hainan Island.

At 5:00 p.m. EDT on Monday the center of Tropical Depression 15W was located at latitude 17.6°N and longitude 136.3°E which put it about 585 miles (945 km) southwest of Iwo To, Japan.  It was moving toward the north-northwest at 10 m.p.h. (16 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 998 mb.  The circulation of Tropical Depression 15W became more organized on Monday and it could eventually strengthen into a typhoon when it moves toward Iwo To later this week.