Tag Archives: Nagoya

Tropical Storm Nari Drops Heavy Rain on Honshu

Tropical Storm Nari dropped locally heavy rain and producing gusty winds on Honshu on Friday night.  At 11:00 p.m. EDT on Friday the center of Tropical Storm Nari was located at latitude 35.2°N and longitude 137.0°E which put it about 10 miles (15 km) east of Nagoya, Japan.  Nari was moving toward the north-northeast at 15 m.p.h. (24 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 Nari was dropping locally heavy rain over parts of central Honshu.  The heaviest rain was falling in bands located in the western half of the circulation.  Heavier rain was falling in the area between Nagoya, Osaka and Kyoto.  Bands of heavier rain were also falling north of Nagoya.  Most of the bands in the eastern half of Tropical Storm Nari consisted primarily lighter showers and lower clouds.  The heavier rain could produce flash flooding in some locations.

Tropical Storm Nari will move more toward the east-northeast on Saturday.  The center of Nari is forecast to pass north of Tokyo.  Tropical Storm Nari will continue to drop locally heavy rain over central and eastern Honshu when it moves over those locations.

Tropical Storm Nari Develops South of Japan

Tropical Storm Nari developed south of Japan on Thursday night.  The Japan Meteorological Agency designated a low pressure system south of Honshu as Tropical Storm Nari when the maximum sustained wind speed reached 40 m.p.h. (65 km/h).  At 11:00 p.m. EDT on Thursday the center of Tropical Storm Nari was located at latitude 30.2°N and longitude 136.9°E which put it about 350 miles (565 km) south of Nagoya, Japan.  Nari was moving toward the north 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.

The circulation around Tropical Storm Nari exhibited more of a hybrid structure than the structure of a pure tropical cyclone.  Tropical Storm Nari developed when an upper level low pressure system stalled south of the Japan.  A surface circulation formed beneath the upper low and then more thunderstorms formed closer to the center of circulation.  The original upper level low was located southwest of the surface low on Thursday night.  The upper level low was producing southwesterly winds which were blowing across the surface low.  Those winds were creating vertical wind shear.  The circulation around Tropical Storm Nari showed evidence of the effect of that wind shear.  The stronger thunderstorms were in a band that curved around north and west of the center of circulation.  Bands south and east of the center consisted primarily of showers and lower clouds.  The wind field around Tropical Storm Nari was also asymmetric.  Winds to tropical storm force extended out about 115 miles (185 km) to the east of the center of circulation, but only extended out about 60 miles (95 km) to the west of the center.

Tropical Storm Nari will move through an environment only marginally favorable for intensification.  Nari will move over water where the Sea Surface Temperature is near 28°C.  The upper low will continue to cause vertical wind shear, which will inhibit intensification.  The upper low will also pull some drier air around the southern side of the circulation.  Nari could strengthen a little during the next 24 hours if more thunderstorms develop closer to the center of circulation.  Tropical Storm Nari will move under stronger westerly winds in about a day or so.  Those winds will cause more vertical wind shear and they should prevent further intensification.

Tropical Storm Nari will be steered by the interaction of the upper low and a subtropical ridge over the western North Pacific Ocean.  Those two features are likely to steer Nari toward the north during the next 24 hours.  On its anticipated track Tropical Storm Nari could approach the coast of Honshu near Nagoya in about 24 hours.  Nari will move more toward the east when it reaches the stronger westerly winds in a day or so.  Tropical Storm Nari could bring gusty winds and locally heavy rain to central Honshu on Saturday.

Typhoon Noru Skirts Coast of Shikoku on Way to Honshu

The eye of Typhoon Noru skirted the coast of Shikoku on Sunday as it moved closer to a landfall on Honshu.  At 11:00 p.m. EDT on Sunday the center of Typhoon Noru was located at latitude 33.6°N and longitude 134.5°W which put it about 85 miles (135 km) southwest of Osaka, Japan.  Noru was moving toward the northeast at 14 m.p.h. (22 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 970 mb.

The structure of Typhoon Noru improved on Sunday.  The circulation contracted around an eye with a diameter of approximately 20 miles (32 km).  They eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in the ring of storms.  Additional spiral bands were revolving around the core of Typhoon Noru.

An upper level trough northwest of Japan steered Typhoon Noru toward the northeast on Sunday.  The eye of Noru moved near the south coast of Shikoku.  The eye passed south of Kochi and very near Muroto, Toyo and Kainan.  Typhoon Noru brought gusty winds and heavy rain to the southern parts of Shikoku.

Typhoon Noru is expected to continue to move toward the northeast on Monday.  On its anticipated track the center of Typhoon Noru is expected to skirt the east coast of Shikoku and make landfall on Honshu near Wakayama.   After it makes landfall, Typhoon Noru is forecast to pass near Osaka and Kyoto.  Typhoon Noru will weaken as it moves across Honshu, but it will produce gusty winds and locally heavy rain.  The rain could cause floods in some locations.