Typhoon Kirogi (2000)

Meteorological history

Typhoon Kirogi originated out of a disorganized area of showers and thunderstorms on June 30, 2000, associated with a weak area of low pressure, situated roughly 650 km (405 mi) east of the Philippine island of Mindanao. The system remained nearly stationary for two days as it became increasingly organized. On July 1, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert as they anticipated the low to develop into a significant tropical cyclone within 24 hours. Around 0600 UTC the following day, the Japan Meteorological Agency (JMA) began monitoring the system as a tropical depression. At the same time, the JTWC also classified the system as Tropical Depression 05W and six hours later, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) began issuing advisories on the same system, classifying it as Tropical Depression Ditang.

Throughout the day on July 2, the depression began to take a slow northward track in response to a mid-level subtropical ridge to the east and later that day, the JTWC upgraded it to a tropical storm. Early the next day, the JMA also upgraded the system to a tropical storm, at which time it received the name Kirogi. Although a broad cyclone, convection was gradually wrapping around the southern periphery of the circulation. Several hours after being named, the JMA upgraded Kirogi to a severe tropical storm and later a typhoon. At the same time, the JTWC classified the storm as a typhoon. Upon being upgraded the typhoon featured a well-developed outflow and prominent banding features consolidating around the system.

Not long after attaining typhoon intensity, Kirogi began to undergo rapid intensification. Roughly 18 hours later, the JTWC reported that the storm had attained its peak intensity with winds of 215 km/h (135 mph 1-minute sustained), equivalent to a Category 4 hurricane on the Saffir–Simpson Hurricane Scale. By this time, the typhoon was situated roughly 870 km (540 mi) southeast of Okinawa. The storm featured a 59 km (37 mi) wide symmetrical eye. Early on July 5, the JMA reported that Kirogi attained its peak intensity with winds of 155 km/h (100 mph 10-minute sustained) and a barometric pressure of 940 mbar (hPa; 27.76 inHg). The storm was a relatively large typhoon, with a gale diameter of 520 km (325 mi).

Several hours after attaining peak intensity on July 5, a mid-level trough caused convection around the center of Kirogi to weaken and the eye became cloud-filled. Later in the day, most of the convective bands were confined to the eastern periphery of the system. Around this time, the storm took a northeasterly track, which it maintained for several days. Increasing in forward motion, the storm began to weaken; however, it also grew in size. By July 6, the storm had a gale-diameter of 925 km (575 mi). Gradual weakening took place as Kirogi tracked towards Japan, with both the JTWC and JMA reporting sustained winds at 140 km/h (85 mph) by July 7. Early on July 8, the storm brushed the eastern coast of Japan near Chōshi, Chiba with winds of 130 km/h (80 mph 10-minute sustained). Several hours later, the typhoon weakened to a severe tropical storm before transitioning into an extratropical cyclone near the southeast coast of Hokkaido. By this time, the storm took a sharp eastward turn and briefly slowed before re-accelerating. The remnants of the storm persisted until July 10, at which time it dissipated to the southwest of the Aleutian Islands.

To measure wind speeds at the storm's center, the Japan Meteorological Agency and Joint Typhoon Warning Center use 10-minute sustained winds and one-minute sustained winds respectively. The conversion factor between 10-minute and one-minute winds is 1.14x. The JMA's peak intensity for Kirogi was 155 km/h (100 mph) 10-minute sustained, or 185 km/h (115 mph) one-minute sustained. The JTWC's peak intensity for Kirogi was 215 km/h (135 mph) one-minute sustained, or 185 km/h (115 mph) 10-minute sustained.

Philippines

In the typhoon's early stages, news reports stated that the outer bands of the storm produced heavy rainfall in the Philippines, resulting in 16 fatalities. However, a meteorological analysis of the storm showed that Kirogi was not responsible for the rain; instead, a monsoon depression that later became Typhoon Kai-tak caused the flooding rains. Typhoon Kirogi was never closer than 835 km (520 mi) from the Philippines. However, large swells produced by the storm caused moderate damage along coastal areas of the Philippines, forcing workers in Manila to clear debris left by the damaging waves.

Japan

In Japan, Kirogi became the first typhoon to threaten the city of Tokyo since a storm in the 1989 Pacific typhoon season, prompting hundreds of residents to evacuate. A total of 120 flights were canceled ahead of the storm and 30 ferry services were halted due to rough seas up to 9 m (30 ft). On Kozushima, 788 residents were evacuated as heavy rain from the typhoon produced landslides. Forecasters warned that upwards of 250 mm (9.8 in) of rain could fall in the Tokyo region. In the city of Tokyo, Japanese officials ordered 800 residents to evacuate to shelters due to the threat of Typhoon Kirogi.

Since the storm weakened considerably from its peak intensity, damage was much less than initially anticipated. In all, damages from the storm amounted to 15 billion (2001 JPY, $140 million USD). Three people were killed by the storm, all of whom were found in irrigation ditches. The first fatality was an 81-year-old man, the second was a 30-year-old man who lost control of his car and crashed into a ditch, and the last fatality was a 3-year-old boy who fell in a ditch near his home. Two 11-year-old boys, initially reported as missing, were later found in a ditch after being swept away by flood waters.

About 1,300 homes were inundated by flood waters around Tokyo and three were destroyed on Kōzushima by a landslide. Widespread power outages took place, leaving an estimated 20,000 people without power in Kanagawa and Shizuoka prefectures as winds up to 177 km/h (110 mph) knocked down trees and power lines. Rainfall from the storm fell at rates of 55 mm/h (2.2 in/h). Total amounts reached 416 mm (16.4 in) in Tokyo, 400 mm (16 in) on Izu Ōshima and 357 mm (14.1 in) in Ogatsu, Miyagi Prefecture. These rains were more than double the monthly average for July in eastern Japan.

Rainfall up to 182 mm (7.2 in) caused flooding throughout eastern Hokkaidō, resulting in widespread agricultural losses. Throughout Aomori Prefecture, large stretches of roads were washed out by flood waters and several thousand homes were inundated. Damage from the storm in Aomori was estimated at 600 million (2001 JPY, $6.6 million USD). In Obihiro, Hokkaidō, a total of 2,957 ha (7,310 acres) of agricultural land was inundated by flood waters. The fishing industry in Urakawa District, Hokkaidō sustained severe losses, amounting to 889 million (2001 JPY, $10 million USD). High winds in the district resulted in moderate roof damage to several homes, some of which lost their roofs.