Typhoon Songda, known in the Philippines as Typhoon Nina, was the third-costliest typhoon on record. The 18th named storm of the 2004 Pacific typhoon season, Songda developed on August 26 near the Marshall Islands. Following a path that Typhoon Chaba took nine days prior, Songda moved west-northwestward and strengthened quickly amid favorable conditions.
|Typhoon Songda (Nina)|
|Typhoon (JMA scale)|
|Category 4 typhoon (SSHWS)|
Typhoon Songda near Northern Mariana Islands on September 1
|Formed||August 26, 2004|
|Dissipated||After September 13, 2004|
|(Extratropical after September 8, 2004)|
|Highest winds||10-minute sustained: 175 km/h (110 mph) |
1-minute sustained: 230 km/h (145 mph)
|Lowest pressure||925 hPa (mbar); 27.32 inHg|
|Damage||$9.3 billion (2004 USD)|
|Areas affected||Mariana Islands, Japan|
|Part of the 2004 Pacific typhoon season|
Forming in a similar region as Typhoon Chaba did nine days earlier, Typhoon Songda originated on August 26 from an area of convection, or thunderstorms, east-northeast of Kwajalein in the Marshall Islands. At 06:00 UTC that day, the Japan Meteorological Agency (JMA) assessed that a tropical depression developed. The convection steadily organized and consolidated into rainbands around a well-developed circulation, aided by low wind shear. At 11:30 UTC on August 28, the Joint Typhoon Warning Center issued a tropical cyclone formation alert, and just 30 minutes later upgraded the system to Tropical Depression 22W.
Favorable conditions allowed the nascent system to quickly intensify. At 00:00 UTC on August 28, the JMA upgraded the depression to a tropical storm, naming it Songda. Moving west-northwestward around the subtropical ridge to the north, the storm passed north of the Marshall Islands. An eye began becoming visible on satellite imagery on August 29, prompting the JTWC to upgrade Songda to typhoon status at 12:00 UTC that day. A day later, the JMA also upgraded the storm to typhoon status, and the agency estimated an initial peak intensity on August 31 of 165 km/h (105 mph). That day, the JTWC also estimated peak 1 minute winds of 230 km/h (145 mph), equivalent to a Category 4 on the Saffir-Simpson scale. Operationally, the JTWC estimated slightly higher winds and assessed Songda as a "super typhoon", but it was revised downward.
The typhoon increased in size as it approached the Northern Marianas Islands (CNMI), which was struck by Typhoon Chaba a week prior. On August 31, Songda turned more to the northwest, which spared the more populated islands of Saipan and Tinian. On September 1, the storm passed about 32 km (20 mi) northeast of Agrihan with 1 minute winds estimated at 233 km/h (145 mph). Subsequently, the typhoon turned more to the west-northwest and weakened slightly. However, an increase in northward outflow caused the convection to deepen, resulting in Songda re-intensifying. On September 4, the JTWC again estimated peak 1 minute winds of 230 km/h (145 mph), and the JMA assessed a peak 10 minute wind peak of 175 km/h (110 mph). Around that time, Songda had turned to the northwest and had developed a symmetric eyewall. At 08:00 UTC on September 5, the typhoon made landfall on the Japanese island of Okinawa while at peak intensity.
A break in the ridge steered Songda northward after the storm struck Okinawa. The storm gradually weakened, partly due to drier air, and accelerated northeastward on September 6 toward western Japan. At 00:00 UTC on September 7, Songda made landfall on Nagasaki in western Kyushu with 10 minute winds of 140 km/h (85 mph). Influenced by an approaching shortwave trough, the storm raced into the Sea of Japan and weakened to tropical storm status. Late on September 7, the JTWC issued their last advisory on Songda, noting that the storm was becoming extratropical. The JMA declared Songda as fully extratropical at 00:00 UTC the next day while the storm was just west of Hokkaido; at that time, the storm merged with a nearby non-tropical low and a cold front. After a brief turn to the north, the storm moved northeastward over northern Hokkaido and southern Sakhalin and entered the Sea of Okhotsk. On September 9, the remnants of Songda moved across the southern Kamchatka Peninsula before moving into the Bering Sea. Late on September 10, the JMA stopped tracking the storm after Songda crossed the 180th meridian. The storm continued eastward, entering the Gulf of Alaska on September 11. Two days later, the system moved inland after weakening further.
Ahead of the storm's passage, a typhoon watch was issued for Agrihan. Moving through the CNMI as a powerful typhoon, Songda largely spared the more populated islands in the south. The center passed about 310 km (190 mi) of Saipan – the commonwealth's center of population. On the island, wind gusts peaked at 61 km/h (38 mph), and rainfall reached 64 mm (2.5 in). Similar conditions occurred on Rota and Tinian to the south, with a peak gust of 79 km/h (49 mph) on Rota. On Pagan Island, Songda produced wind gusts of 174 km/h (108 mph) as well as 98 mm (3.84 in) of rainfall. Typhoon-force winds also affected Agrihan and Alamagan. In the northern islands of the CNMI, Songda destroyed all of the homes while defoliating the coconut and breadfruit trees. Damage was estimated at $500,000 (USD).
On September 3, the storm came close enough to the Philippines to warrant monitoring from PAGASA,[nb 1] which named the storm Nina. Monsoon-induced rainfall from Songda, in conjunction with Typhoon Aere in the South China Sea, caused flooding in portions of the Philippines. This led to landslides and traffic accidents, as well as eight deaths.
The outskirts of the typhoon dropped heavy rainfall in South Korea, with a peak 24‑hour total of 112 mm (4.4 in) on the offshore island of Ulleungdo. On the mainland, Pohang recorded 110.5 mm (4.35 in) of rainfall over 24 hours. Damage in the country was estimated at $250 million (USD).
Typhoon Songda was the seventh of ten typhoons to strike the Japanese mainland during 2004, the most typhoon landfalls since the JMA began keeping records in 1951. Its track across Kyushu into the Sea of Japan brought the strongest winds to most of Japan, peaking at 144 km/h (89 mph) in Seto, Ehime on western Shikoku. While the storm was near Okinawa, it produced a 1200 km (745 mi) plume of moisture that spread northward across Japan. In some places, the rains were enhanced by mountains, a process known as orographic lift. The heaviest rainfall from Songda was 905 mm (35.6 in) in Morotsuka, Miyazaki on Kyushu, of which 513 mm (20.2 in) was reported in 24 hours. Significant rainfall totals occurred in short periods of time, including 78 mm (3.1 in) in Soeda, Fukuoka. The heaviest damage was on Kyushu and western Honshu. The high winds damaged many roofs, including that of newer public buildings, which accounted for a large portion of the damage. Flooding affected 8,360 houses, and 42,183 homes sustained damage during the storm, of which 109 were completely destroyed. In addition to housing damage, Songda wrecked 104 ha (260 acres) of crop fields and damaged 1,592 ships. Overall, the typhoon killed 47 people in Japan and injured another 1,364, 205 of them severely. Damage nationwide were about JP¥126.2 billion (US$1.15 billion) .
The typhoon first passed near Okinawa Prefecture. Nago recorded a minimum pressure of 924.4 mbar (27.30 inHg), which was the lowest recorded during the storm's duration. Minamidaitōjima to the east of Okinawa registered a peak wind gust of 190 km/h (118 mph). Songda also dropped heavy rainfall on the island, peaking at 351 mm (13.8 in) on Mount Yonaha. High waves flooded six houses and inundated several roads, and one roof was damaged. Across the prefecture, 152 people evacuated, while air and sea travel was halted. The storm injured 16 people, one seriously, and left JP¥880 million (US$8 million) in damage, mostly sugar cane losses.
Along western Honshu, Songda damaged the Yamaguchi Center for Arts and Media and the Kirara Genki Dome in Yamaguchi Prefecture. Winds and strong waves heavily damaged the Itsukushima Shrine, a structure over water in Hiroshima that dates back to the 14th century.
The storm restrengthened while over the Sea of Japan, causing additional heavy damage by the time it reached Hokkaido. High wind gusts knocked down trees and sign posts. There, about 0.1% of the houses were damaged. High winds damaged the roof of a high school in Ebetsu.
The high damage across Japan caused insurance companies to pay $4 billion (USD) to policy holders.
The name Nina has been used for thirteen typhoons in the northwest Pacific Ocean, one tropical cyclone in the northeast Pacific Ocean, and one tropical cyclone in the southwest Pacific.
Twelve typhoons have been named Nina. In addition, one hurricane in the Central Pacific was given this name because the policy at the time was to use typhoon names in the Central Pacific.
Typhoon Nina (1953) (T5307) made landfall in China
Hurricane Nina (1957) Category 1 hurricane.
Typhoon Nina (1960) (T6025, 51W) never made landfall.
Tropical Storm Nina (1963) – minor storm.
Typhoon Nina (1966) (T6607, 07W) was a Category 1 tropical cyclone
Typhoon Nina (1968) (T6826, 31W, Seniang) crossed the Philippines.
Tropical Storm Nina (1972) (T7204, 05W) minor storm.
Typhoon Nina (1975) (T7503, 04W, Bebeng) struck Taiwan. Contributed to the collapse of the Banqiao Dam in central China, killing around 200,000.
Tropical Storm Nina (1978) (T7823, 24W) minor storm.
Tropical Storm Nina (1981) (T8109, 09W, Ibiang) minor storm.
Tropical Storm Nina (1984) (T8415, 18W) minor storm.
Typhoon Nina (1987) (T8722, 22W, Sisang) crossed the Philippines as a major typhoon.
Tropical Storm Nina (1992) (T9213, 14W) minor storm.
Tropical Storm Nina (1995) (T9511, 15W, Helming) minor storm.PAGASA Naming The following typhoons were named Nina by PAGASA. After 2016, the PAGASA retired the name Nina in their naming lists and was replaced with Nika.
Typhoon Songda (2004) (T0418, 22W, Nina)
Typhoon Hagupit (2008) (T0814, 18W, Nina) – struck China, killing 67 and causing 1 billion in damage.
Typhoon Prapiroon (2012) (T1221, 22W, Nina)
Typhoon Nock-ten (2016) (T1626, 30W, Nina) – a late-season powerful storm that affected the Philippines.Southwest Pacific:
Cyclone Nina (1992–93), category 3 storm, crossed Oceania.Typhoon Nabi
Typhoon Nabi (pronounced [na.bi]), known in the Philippines as Typhoon Jolina, was a powerful typhoon that struck southwestern Japan in September 2005. The 14th named storm of the 2005 Pacific typhoon season, Nabi formed on August 29 to the east of the Northern Mariana Islands. It moved westward and passed about 55 km (35 mi) north of Saipan on August 31 as an intensifying typhoon. On the next day, the Joint Typhoon Warning Center upgraded the storm to super typhoon status, with winds equivalent to that of a Category 5 hurricane on the Saffir–Simpson Hurricane Scale. The Japan Meteorological Agency estimated peak ten-minute winds of 175 km/h (110 mph) on September 2. Nabi weakened while curving to the north, striking the Japanese island of Kyushu on September 6. After brushing South Korea, the storm turned to the northeast, passing over Hokkaido before becoming extratropical on September 8, before dissipating on September 12.
The typhoon first affected the Northern Mariana Islands, where it left US$2.5 million in damage, while damaging or destroying 114 homes. The damage was enough to warrant a disaster declaration from the United States government. While passing near Okinawa, Nabi produced gusty winds and caused minor damage. Later, the western fringe of the storm caused several traffic accidents in Busan, South Korea, and throughout the country Nabi killed six people and caused US$115.4 million in damage. About 250,000 people evacuated along the Japanese island of Kyushu ahead of the storm, and there were disruptions to train, ferry, and airline services. In Kyushu, the storm left ¥4.08 billion (US$36.9 million) in crop damage after dropping 1,322 mm (52.0 in) of rain over three days. During the storm's passage, there were 61 daily rainfall records broken by Nabi's precipitation. The rains caused flooding and landslides, forcing people to evacuate their homes and for businesses to close. Across Japan, Nabi killed 29 people and caused ¥94.9 billion (US$854 million) in damage. Soldiers, local governments, and insurance companies helped residents recover from the storm damage. After affecting Japan, the typhoon affected the Kuril Islands of Russia, where it dropped the equivalent of the monthly precipitation, while also causing road damage due to high waves. Overall, Nabi killed 35 people.Typhoon Songda
The name Songda has been used to name three tropical cyclones in the northwestern Pacific Ocean. The name was contributed by Vietnam, and is a river in northwestern Vietnam.
Typhoon Songda (2004) (T0418, 22W, Nina) – struck Japan.
Typhoon Songda (2011) (T1102, 04W, Chedeng) – approached Japan.
Typhoon Songda (2016) (T1620, 23W)- approached Canada as a post tropical storm.
Tropical cyclones of the 2004 Pacific typhoon season