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Typhoon Ma-on (2004)
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Typhoon Ma-on (2004)
Typhoon Ma-on, known in the Philippines as Typhoon Rolly, was a powerful typhoon that produced record breaking wind gusts across the Tokyo Metropolitan Area during early October 2004. It was the strongest typhoon to hit the region since Typhoon Higos in 2002. The twenty-second named storm of the 2004 Pacific typhoon season, Ma-on was the second of three consecutive storms to hit Japan during the period between late-September to mid-October 2004.
Typhoon Ma-on originated from a weak low-pressure area accompanied by persistent convection, or thunderstorms, north-northwest of Guam on September 29, 2004. Though environmental conditions featured weak wind shear and modest diffluence, favoring tropical cyclogenesis, the convection was cyclical and the system did not develop much over the following two days. Over the first three days of October, organization fluctuated as semi-persistent convection appeared over the circulation center. On October 3, a QuikScat satellite pass revealed a well-developed circulation while a ship 555 km (345 mi) south of the low reported 45 km/h (28 mph) winds. The Japan Meteorological Agency (JMA) began monitoring the low as a tropical depression at 06:00 UTC. Twelve hours later, the depression crossed 135°E and entered the Philippine Atmospheric, Geophysical and Astronomical Services Administration's (PAGASA) area of responsibility, receiving the local name Rolly from the agency. Becoming nearly stationary, the system turned due north late on October 3. At 00:00 UTC on October 4, the Joint Typhoon Warning Center (JTWC) classified the system as Tropical Depression 26W; the newly designated cyclone was situated over the Philippine Sea roughly 1,145 km (711 mi) west-northwest of Guam at this time. Six hours later, both the JMA and JTWC analyzed the depression and concluded it had become a tropical storm; the JMA assigning it the name Ma-on. Slow organization of Ma-on ensued over the following two days as it moved north and later northwest along the edge of a high-pressure area. The JTWC estimated Ma-on to have reached typhoon status around 06:00 UTC on October 6, with the JMA following suit 12 hours later.
Synoptic patterns changed dramatically on October 7 as a trough emerged off the coast of East China and prompted Ma-on to turn northeast. Simultaneously, it provided a greatly enhanced poleward outflow channel toward Japan. The shift in motion was also accompanied by a period of rapid intensification, with a well-defined eye forming. Over the 24 hour-period from 18:00 to 18:00 UTC October 6–7, Ma-on's barometric pressure dropped from 965 mb (hPa; 28.50 inHg) to 920 mb (hPa; 27.17 inHg). The end of this phase marked the peak intensity of the typhoon, with winds reaching 185 km/h (115 mph). The JTWC estimated Ma-on to have been a significantly stronger storm with one-minute sustained winds topping out at 260 km/h (160 mph) at 00:00 UTC on October 8. This ranked it as a Category 5-equivalent typhoon on the Saffir–Simpson hurricane wind scale. They also assessed the pressure to have decreased to 898 mb (hPa; 26.52 inHg). Not long after reaching this intensity, Ma-on's eye began to shrink and become ragged. Acceleration to the northeast, with its forward speed reaching 54 km/h (34 mph), ensued throughout the day and weakening ensued. Convection became increasingly asymmetric with dry air impinging on the southwestern semicircle, indicating the beginning of extratropical transition. The typhoon made landfall along the Izu Peninsula of Japan around 07:00 UTC on October 9, with winds of 150 km/h (93 mph) and a central pressure of 950 mb (hPa; 28.06 inHg). The JTWC estimated Ma-on to have been a Category 3-equivalent with one-minute sustained winds of 195 km/h (121 mph). Roughly six hours after striking Japan, the rapidly weakening typhoon re-emerged over the Pacific Ocean. The system completed its extratropical transition later on October 9 as it weakened below typhoon intensity.
After losing a defined low-level circulation early on October 10, Ma-on's the remnant trough continued eastward across the North Pacific. More than a week later, by October 18, the storm moved over the Bering Sea and began to intensify rapidly as conditions favored bombogenesis of the baroclinic system. It is not certain whether this system was predominantly the remnants of Ma-on or another non-tropical system which had its origins near Norway and traversed Eurasia. Regardless of its dominant origin the storm moved across the central Aleutian Islands with a pressure of 978 mb (hPa; 28.88 inHg) on October 17 and doubled back to the west throughout the next day. As it moved over the Gulf of Anadyr, it quickly deepened to an exceptionally powerful 941 mb (hPa; 27.79 inHg). The intensification resulted from the influx of warm, moist air directly associated with the remnants of Ma-on combining with cold air from an upper-level low over the Russian Far East being entrained into the southeastern portion of the circulation. Winds up to typhoon-force occurred over a large swath of the Bering Sea and portions of western coastal Alaska. Situated 640 km (400 mi) west of Nome, Alaska, the powerful storm subsequently weakened and slowed on October 19. By October 20, the system filled to 980 mb (hPa; 28.95 inHg) low and reached a position 640 km (400 mi) west of Kotzebue, Alaska. Over the subsequent four days, the low meandered in the same general area and was last noted on October 24.
As Typhoon Ma-on began turning to the north on October 8 towards Japan, the JMA warned residents in the Tōkai, Kansai, and Shikoku regions of heavy rain. Meteorologists warned it would likely become the strongest storm to strike the Kantō region in at least a decade. Japan Airlines and All Nippon Airways cancelled 262 flights collectively on October 9, affecting 53,000 passengers. Overall, 380 domestic and 72 international flights were cancelled because of Ma-on. The Central Japan Railway Company temporarily suspended service for the entire Tōkaidō Shinkansen line, which travels from Tokyo to Shin-Ōsaka. Mandatory evacuation orders were issued for 3,528 families across five prefectures, while a further 1,600 families voluntarily evacuated from 13 others. Voluntary evacuations also took place on Minamidaitōjima. Practice and qualifying runs for the 2004 Japanese Grand Prix at the Suzuka Circuit, initially scheduled for October 9, were suspended until the following day. Play at the Japan Open was suspended briefly because of the rain from the storm.
Typhoon Ma-on was the eighth of a record-breaking ten landfalling typhoons in Japan during the 2004 season. Of these storms, Ma-on was the only system to strike eastern areas of the nation directly and the second-strongest, with a landfall pressure of 950 mb (hPa; 28.06 inHg). Collectively, these storms resulted in 214 fatalities and over 2,000 injuries. Widespread and extensive damage to housing and infrastructure occurred with well over 200,000 homes damaged or destroyed and financial losses in excess of ¥564 billion (US$5 billion).
The typhoon produced record-breaking wind across the Izu Peninsula when it made landfall on October 9. The most intense winds of more than 215 km/h (134 mph) were confined to areas along Sagami Bay, about 40 km (25 mi) southeast of Tokyo. Contrary to most tropical cyclones, which see their strongest winds in the right-front quadrant, these winds occurred along the backside of Typhoon Ma-on. As the storm passed through, a low level jet formed along the east edge of the Kanto Mountains and facilitated an extreme gap flow event. A peak gust of 243 km/h (151 mph) was measured in Irōzaki; sustained values reached 142 km/h (88 mph) in Ajiro. Record high gusts were observed in Irōzaki, Ajiro, and Ojima, while record high sustained winds occurred in Ajiro, Haneda, and Ojima. The extreme gap flow event resulted from the warm air associated with Ma-on moving over the relatively cool air over the Kanto Plain. As the backside of the storm moved through, northerly winds pushed the cooler air south and allowed it to extend to higher altitudes as it paralleled the mountains along the west side of the plains. Model simulations of the event indicated that without the mountains, winds would have been no more than 126 km/h (78 mph) in the same areas.
Torrential rains accompanied the storm, with several areas reporting rainfall rates in excess of 60 mm (2.4 in) per hour. A local record of 89 mm (3.5 in) per hour was measured in Omaezaki, Shizuoka, which contributed to a 24-hour record of 360 mm (14 in) at the same station. Storm total values peaked in Omaezaki at 413 mm (16.3 in) over a three-day period; measurements in excess of 300 mm (12 in) were confined to Aichi, Chiba, Kanagawa, Shizuoka, and Yamanashi prefectures. Enhanced precipitation affected areas well to the west of Ma-on, such as in Okinawa Prefecture where up to 190 mm (7.5 in) fell in Motobu.
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Typhoon Ma-on (2004)
Typhoon Ma-on, known in the Philippines as Typhoon Rolly, was a powerful typhoon that produced record breaking wind gusts across the Tokyo Metropolitan Area during early October 2004. It was the strongest typhoon to hit the region since Typhoon Higos in 2002. The twenty-second named storm of the 2004 Pacific typhoon season, Ma-on was the second of three consecutive storms to hit Japan during the period between late-September to mid-October 2004.
Typhoon Ma-on originated from a weak low-pressure area accompanied by persistent convection, or thunderstorms, north-northwest of Guam on September 29, 2004. Though environmental conditions featured weak wind shear and modest diffluence, favoring tropical cyclogenesis, the convection was cyclical and the system did not develop much over the following two days. Over the first three days of October, organization fluctuated as semi-persistent convection appeared over the circulation center. On October 3, a QuikScat satellite pass revealed a well-developed circulation while a ship 555 km (345 mi) south of the low reported 45 km/h (28 mph) winds. The Japan Meteorological Agency (JMA) began monitoring the low as a tropical depression at 06:00 UTC. Twelve hours later, the depression crossed 135°E and entered the Philippine Atmospheric, Geophysical and Astronomical Services Administration's (PAGASA) area of responsibility, receiving the local name Rolly from the agency. Becoming nearly stationary, the system turned due north late on October 3. At 00:00 UTC on October 4, the Joint Typhoon Warning Center (JTWC) classified the system as Tropical Depression 26W; the newly designated cyclone was situated over the Philippine Sea roughly 1,145 km (711 mi) west-northwest of Guam at this time. Six hours later, both the JMA and JTWC analyzed the depression and concluded it had become a tropical storm; the JMA assigning it the name Ma-on. Slow organization of Ma-on ensued over the following two days as it moved north and later northwest along the edge of a high-pressure area. The JTWC estimated Ma-on to have reached typhoon status around 06:00 UTC on October 6, with the JMA following suit 12 hours later.
Synoptic patterns changed dramatically on October 7 as a trough emerged off the coast of East China and prompted Ma-on to turn northeast. Simultaneously, it provided a greatly enhanced poleward outflow channel toward Japan. The shift in motion was also accompanied by a period of rapid intensification, with a well-defined eye forming. Over the 24 hour-period from 18:00 to 18:00 UTC October 6–7, Ma-on's barometric pressure dropped from 965 mb (hPa; 28.50 inHg) to 920 mb (hPa; 27.17 inHg). The end of this phase marked the peak intensity of the typhoon, with winds reaching 185 km/h (115 mph). The JTWC estimated Ma-on to have been a significantly stronger storm with one-minute sustained winds topping out at 260 km/h (160 mph) at 00:00 UTC on October 8. This ranked it as a Category 5-equivalent typhoon on the Saffir–Simpson hurricane wind scale. They also assessed the pressure to have decreased to 898 mb (hPa; 26.52 inHg). Not long after reaching this intensity, Ma-on's eye began to shrink and become ragged. Acceleration to the northeast, with its forward speed reaching 54 km/h (34 mph), ensued throughout the day and weakening ensued. Convection became increasingly asymmetric with dry air impinging on the southwestern semicircle, indicating the beginning of extratropical transition. The typhoon made landfall along the Izu Peninsula of Japan around 07:00 UTC on October 9, with winds of 150 km/h (93 mph) and a central pressure of 950 mb (hPa; 28.06 inHg). The JTWC estimated Ma-on to have been a Category 3-equivalent with one-minute sustained winds of 195 km/h (121 mph). Roughly six hours after striking Japan, the rapidly weakening typhoon re-emerged over the Pacific Ocean. The system completed its extratropical transition later on October 9 as it weakened below typhoon intensity.
After losing a defined low-level circulation early on October 10, Ma-on's the remnant trough continued eastward across the North Pacific. More than a week later, by October 18, the storm moved over the Bering Sea and began to intensify rapidly as conditions favored bombogenesis of the baroclinic system. It is not certain whether this system was predominantly the remnants of Ma-on or another non-tropical system which had its origins near Norway and traversed Eurasia. Regardless of its dominant origin the storm moved across the central Aleutian Islands with a pressure of 978 mb (hPa; 28.88 inHg) on October 17 and doubled back to the west throughout the next day. As it moved over the Gulf of Anadyr, it quickly deepened to an exceptionally powerful 941 mb (hPa; 27.79 inHg). The intensification resulted from the influx of warm, moist air directly associated with the remnants of Ma-on combining with cold air from an upper-level low over the Russian Far East being entrained into the southeastern portion of the circulation. Winds up to typhoon-force occurred over a large swath of the Bering Sea and portions of western coastal Alaska. Situated 640 km (400 mi) west of Nome, Alaska, the powerful storm subsequently weakened and slowed on October 19. By October 20, the system filled to 980 mb (hPa; 28.95 inHg) low and reached a position 640 km (400 mi) west of Kotzebue, Alaska. Over the subsequent four days, the low meandered in the same general area and was last noted on October 24.
As Typhoon Ma-on began turning to the north on October 8 towards Japan, the JMA warned residents in the Tōkai, Kansai, and Shikoku regions of heavy rain. Meteorologists warned it would likely become the strongest storm to strike the Kantō region in at least a decade. Japan Airlines and All Nippon Airways cancelled 262 flights collectively on October 9, affecting 53,000 passengers. Overall, 380 domestic and 72 international flights were cancelled because of Ma-on. The Central Japan Railway Company temporarily suspended service for the entire Tōkaidō Shinkansen line, which travels from Tokyo to Shin-Ōsaka. Mandatory evacuation orders were issued for 3,528 families across five prefectures, while a further 1,600 families voluntarily evacuated from 13 others. Voluntary evacuations also took place on Minamidaitōjima. Practice and qualifying runs for the 2004 Japanese Grand Prix at the Suzuka Circuit, initially scheduled for October 9, were suspended until the following day. Play at the Japan Open was suspended briefly because of the rain from the storm.
Typhoon Ma-on was the eighth of a record-breaking ten landfalling typhoons in Japan during the 2004 season. Of these storms, Ma-on was the only system to strike eastern areas of the nation directly and the second-strongest, with a landfall pressure of 950 mb (hPa; 28.06 inHg). Collectively, these storms resulted in 214 fatalities and over 2,000 injuries. Widespread and extensive damage to housing and infrastructure occurred with well over 200,000 homes damaged or destroyed and financial losses in excess of ¥564 billion (US$5 billion).
The typhoon produced record-breaking wind across the Izu Peninsula when it made landfall on October 9. The most intense winds of more than 215 km/h (134 mph) were confined to areas along Sagami Bay, about 40 km (25 mi) southeast of Tokyo. Contrary to most tropical cyclones, which see their strongest winds in the right-front quadrant, these winds occurred along the backside of Typhoon Ma-on. As the storm passed through, a low level jet formed along the east edge of the Kanto Mountains and facilitated an extreme gap flow event. A peak gust of 243 km/h (151 mph) was measured in Irōzaki; sustained values reached 142 km/h (88 mph) in Ajiro. Record high gusts were observed in Irōzaki, Ajiro, and Ojima, while record high sustained winds occurred in Ajiro, Haneda, and Ojima. The extreme gap flow event resulted from the warm air associated with Ma-on moving over the relatively cool air over the Kanto Plain. As the backside of the storm moved through, northerly winds pushed the cooler air south and allowed it to extend to higher altitudes as it paralleled the mountains along the west side of the plains. Model simulations of the event indicated that without the mountains, winds would have been no more than 126 km/h (78 mph) in the same areas.
Torrential rains accompanied the storm, with several areas reporting rainfall rates in excess of 60 mm (2.4 in) per hour. A local record of 89 mm (3.5 in) per hour was measured in Omaezaki, Shizuoka, which contributed to a 24-hour record of 360 mm (14 in) at the same station. Storm total values peaked in Omaezaki at 413 mm (16.3 in) over a three-day period; measurements in excess of 300 mm (12 in) were confined to Aichi, Chiba, Kanagawa, Shizuoka, and Yamanashi prefectures. Enhanced precipitation affected areas well to the west of Ma-on, such as in Okinawa Prefecture where up to 190 mm (7.5 in) fell in Motobu.
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