Typhoon Etau (2003)

Map plotting the storm's track and intensity, according to the Saffir–Simpson scale

Map key

Saffir–Simpson scale

  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown

Storm type

Tropical cyclone

Subtropical cyclone

Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

The origins of Typhoon Etau were from an area of convection that persisted along the west side of a weak circulation near Chuuk State on July 31. With initially moderate but steadily decreasing wind shear, the system was able to organize as it moved generally westward.[2] On August 2, the Joint Typhoon Warning Center (JTWC)[nb 2] initiated advisories on Tropical Depression 11W.[4] That day, another circulation was developing on the western side of the system, briefly classified by the Taiwan Central Weather Bureau as a tropical depression. The eastern circulation became dominant with pronounced outflow to the south, although it was initially broad and elongated.[2] Later on August 2, the Japan Meteorological Agency (JMA)[nb 3] classified the system as a tropical depression to the northeast of Yap.[5]

With a subtropical ridge in the vicinity of the Marianas Islands, the nascent depression moved to the northwest.[2] On August 3, the JMA upgraded the depression to tropical storm status, naming it Etau.[5] An upper-level low to the northeast improved northerly outflow, allowing the storm to strengthen quickly.[4] On August 4 the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) began issuing advisories as the storm approached the region, naming it Kabayan.[1] Late on August 4, the JMA upgraded Etau to typhoon status,[5] with the storm later developing an eye. An approaching shortwave trough weakened the ridge, causing Etau to turn more to the north.[2] At around 0030 UTC on August 7, the typhoon made its closest approach to Okinawa,[5] passing within 120 km (75 mi), and close enough for the 100 km (62 mi) wide eye to cross over the island.[2][6] Later that day, the JMA estimated peak maximum sustained winds of 155 km/h (96 mph), sustained over a duration of 10 minutes;[5] the JTWC estimated 1 minute winds of 205 km/h (127 mph).[4]

After reaching peak winds, Etau began turning to the north-northeast due to the approaching trough, passing near Amami Ōshima. By that time, the typhoon had become large, with gale-force winds extending 870 km (540 mi) in diameter.[2] Increasing wind shear and cooler air caused Etau to weaken.[4] The typhoon still maintained 10 minute winds of 140 km/h (87 mph) when it made landfall near Muroto on the Japanese island of Shikoku, shortly before 1300 UTC on August 8. Continuing northeastward, the typhoon weakened into a severe tropical storm as it passed near Awaji Island, before making landfall on Honshu near Nishinomiya at 2100 UTC on August 8.[5] While accelerating to the northeast, Etau lost tropical characteristics over land. After briefly reaching open waters to the northeast of Honshu, the storm made its final landfall near Erimo, Hokkaido at 1630 UTC on August 9, shortly before becoming extratropical. This was based on analysis from the JMA,[5] whereas the JTWC assessed the storm remaining offshore Hokkaido.[4] The remnants of Etau entered the Sea of Okhotsk and persisted for several more days, dissipating on August 12 to the west of the Kamchatka Peninsula.[5]

Typhoon Etau approaching Japan on August 8

Rough waves from Typhoon Etau produced rip currents on Saipan that swept up four swimmers, who were later rescued after holding onto a buoy.[7] The outer periphery of the storm caused P36.98 million (PHP, $673,000 USD) in damage,[nb 4] mostly to infrastructure with some minor crop damage.[9] Late in its duration, Etau caused damage in Russia's Kuril Islands.[10]

While Etau was in the vicinity of Okinawa, wind gusts at Kadena Air Base reached 181 km/h (112 mph).[4] Rainfall on Okinawa peaked at 215 mm (8.5 in), while on nearby Yakushima to the north, rainfall reached 57 mm (2.2 in).[11] Throughout Okinawa prefecture, the typhoon left 166,800 buildings without power due to the strong winds. Etau damaged seven buildings, blocked one road, and caused moderate damage to crops and fisheries.[6] In the Amami Islands, about 45,000 houses, lost power due to high winds from the storm, affecting 53% of residents. Etau injured ten people in the island group, including one man who was blown off his roof.[12] Officials closed the Naha Airport due to the typhoon, causing 293 flights in the region to be canceled.[13] Ahead of the storm, ExxonMobil oil refineries in Okinawa were closed, but were reopened after sustaining minimal damage.[14]

On Shikoku, Muroto reported typhoon-force winds for eight hours,[2] and wind gusts peaked at 166 km/h (103 mph).[15] At the time, this was the third strongest gust ever reported there, behind Typhoon Nancy in 1961 and Typhoon Shirley in 1965.[2] Sustained winds there reached 180 km/h (110 mph).[16] In Tokushima Prefecture, Etau dropped heavy rainfall peaking at 683 mm (26.9 in), although similarly heavy totals of 639 and 543 mm (25.2 and 21.4 in) were reported in Kōchi and Miyazaki prefectures, respectively. About 95% of the rainfall total in Kōchi fell in 24 hours. In Miyazaki, a station reported an hourly rainfall total of 79 mm (3.1 in).[15] Rainfall at Biratori, Hokkaido reached 306.2 mm (12.06 in) in a 48‑hour period, the highest at the station since records began in 1962. The heavy rainfall caused landslides across Hokkaido, particularly in areas where rainfall totaled over 330 mm (13 in). In the area around the Saru River, shallow landslides displaced about 13,000,000 m³ (460,000,000 cu ft) of soil, of which about 190,000 m³ (6,700,000 cu ft) entered the river.[17] This caused the highest sediment levels in the river since the 1960s,[18] washing about 50,000 m³ (1,800,000 cu ft) into the Nibutani Dam.[17] Landslides also swept about 65,000 m³ (2,300,000 cu ft) of soil and trees into the Appetsu River, which caused additional damage by washing away adjacent homes and bridges.[17] In addition the rainfall, Etau spawned a weak tornado near Kumagaya on the Honshu mainland, rated around an F1.[19] The typhoon brought a plume of warm air to the country that caused the warmest temperatures of the year at that point.[20]

The heavy rainfall in Tokushima caused landslides and blocked roads, resulting in disruptions to bus and train service. Strong winds overturned a truck, injuring the two occupants.[21] In Muroto, several people were injured by flying glass. Rough waves killed two people in the same city,[16] one in Fukuoka,[22] damaged the seawall in Kyoto,[23] and damaged 25 ships.[15] In Takamatsu, Kagawa, Etau left about ¥1.2 billion (JPY, $10 million USD) in crop damage, mainly due to damaged greenhouses.[24] Two workers were killed in Higashiuwa after being swept away by a river.[25] On Hokkaido, heavy rainfall caused landslides, damaging hundreds of roads and bridges and isolating several villages.[26] River flooding swept away a vehicle in Kamishihoro, killing the five occupants.[27] Along Mount Poroshiri, 29 people were rescued by helicopter from a mountain lodge after Etau blocked off their descending trail.[28]

Throughout Japan, Etau caused over 1,000 flights to be canceled,[29] and for bullet trains to operate at a slower speed, causing delays.[30] About 62,000 people lost power during the storm, and across the country.[31] The typhoon destroyed 708 houses and flooded 2,253 others,[15] causing over 6,000 people to evacuate to storm shelters.[31] About 295 ha (730 acres) of fields were damaged. Throughout Japan, Etau killed 20 people and injured 93 others, 19 of them seriously. Overall damage totaled ¥35.1 billion (JPY, US$294.8 million).[nb 5][15] Largely because Etau remained tropical and weakened over Japan, damage was much less than Typhoon Tokage a year later, which produced comparable rainfall totals at a similar intensity but struck the country while extratropical.[33]

• Other tropical cyclones named Etau
• Other tropical cyclones named Kabayan
• Typhoon Neoguri (2014)
• Typhoon Tokage (2004)

Wikimedia Commons has media related to Typhoon Etau (2003).

• JMA General Information of Typhoon Etau (0310) from Digital Typhoon
• JMA Best Track Data of Typhoon Etau (0310) (in Japanese)
• JMA Best Track Data (Graphics) of Typhoon Etau (0310)
• JMA Best Track Data (Text)
• JTWC Best Track Data of Typhoon 11W (Etau)
• 11W.ETAU from the U.S. Naval Research Laboratory