Meteorological history | |
---|---|
Formed | July 30,2020 |
Extratropical | August 5 |
Dissipated | August 14,2020 [1] |
Typhoon | |
10-minute sustained (JMA) | |
Highest winds | 130 km/h (80 mph) |
Lowest pressure | 975 hPa (mbar);28.79 inHg |
Category 1-equivalent typhoon | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 140 km/h (85 mph) |
Lowest pressure | 971 hPa (mbar);28.67 inHg |
Overall effects | |
Fatalities | 17 total |
Missing | 11 |
Damage | $1.5 billion (2020 USD) |
Areas affected | Ryukyu Islands,Taiwan,East China,Korean Peninsula,Kamchatka Peninsula,Alaska |
IBTrACS | |
Part of the 2020 Pacific typhoon season |
Typhoon Hagupit,known in the Philippines as Severe Tropical Storm Dindo,was a Category 1 typhoon that heavily impacted Eastern China and South Korea in August 2020. It was the fourth named storm and the second typhoon of the annual typhoon season. The JMA began monitoring a tropical depression that developed in the Philippine Sea on July 30,with PAGASA assigning the name “Dindo”to the storm,later that day it strengthened into a tropical storm,according to the JMA. PAGASA issued its final advisory on Dindo early on August 3,as it moved out of their area of responsibility. Hagupit intensified into a typhoon on August 3,before making landfall in Wenzhou,China at 19:30 UTC that day at peak intensity. Hagupit subsequently weakened over China,before degenerating into an extratropical low on August 5. Hagupit's remnants persisted for another several days,as the storm moved eastward,before dissipating south of Alaska on August 14.
Hagupit caused over a foot of rainfall in portions of Eastern China and South Korea. Hagupit caused 17 fatalities due to bringing heavy rains in the Korean Peninsula,and triggered a landslide which killed 6 people. Damage totals was reported to be at US$1.5 billion.
In late July 2020, the JMA designated a weak tropical depression that developed approximately 991 km (616 mi) east-northeast of Manila, Philippines. [2] [3] Later on the same day, the Philippine Atmospheric, Geophysical and Astronomical Services Administration named the depression as Dindo. [4] In the following hours, the Joint Typhoon Warning Center gave a Tropical Cyclone Formation Alert on the system. [5] The next day, the JTWC designated Dindo as 03W. [6]
Within an overall favorable environment of low vertical wind shear, strong equatorial outflow and 31 °C sea surface temperatures, [6] Dindo further organized in the Philippine Sea, and around midday of the same day, the JMA upgraded the depression to a tropical storm, naming it as Hagupit. [7] Hagupit then began gradually intensifying, and by 09:00 UTC on August 2, the JTWC upgraded the storm to a category 1 typhoon. [8] Late on the same day, JMA upgraded Hagupit to a severe tropical storm. [9] As Hagupit moved generally northwestward, it exited the Philippine Area of Responsibility (PAR), prompting PAGASA to issue its final advisory on the system. [10]
Now northeast of Taiwan, Hagupit was upgraded into a typhoon by the JMA. [11] The storm will later peak in intensity when the JMA reported a pressure drop into 975 hPa (28.28 inHg). [12] At around 19:30 UTC, Hagupit made landfall in Zhejiang, China, with winds of 85 mph and pressure of 975 mbar (hPa). [13] After its landfall, Hagupit began gradually weakening, and on early August 3, Hagupit was downgraded into a tropical storm by the JTWC. [14] At the same time, the JMA downgraded Hagupit into a severe tropical storm. [15] Around midday of the same day, the JTWC downgraded Hagupit into a tropical depression, and later issued their final advisory on the weakening storm, [16] but the JMA still monitored Hagupit as a tropical storm, although the said storm was undergoing an extratropical transition. [17]
The transition completed on August 6, and the JMA issued their final advisory on Hagupit. [18] Over the next several days, Hagupit's remnants moved northeastward, and then eastward, before dissipating just south of Alaska on August 14. [1]
In advance of Hagupit, Chinese officials ordered the evacuation of areas vulnerable to flooding. [19] At least 200,000 people evacuated to shelters in Wenzhou. [20] Ferry services were shut down and trains ran shortened routines in the cities of Taizhou and Wenzhou. Fishing boats in the provinces of Fujian and Zhejiang were advised to return to shore. [21]
Hagupit caused torrential rainfall over portions of China peaking at 13.11 inches (333 mm) in the Jingshan district of Wenzhou. [22] Waves up to 14 ft. (4.2 m) were reported, in association with Hagupit. [23] Over 830,000 customers lost power in China. A 62-year-old woman was killed when she fell 11 stories out of a broken window in Yuhuan, where a panel truck was toppled by high winds. [24] [25] Direct economic losses reached ¥10.46 billion (US$1.5 billion). [26]
The Central Weather Bureau posted a heavy rain warning for portions of Taiwan. Hagupit dropped heavy precipitation up to 3.15 inches (80 mm) in parts of the country. [27] A government employee drowned due to heavy rains caused by Hagupit and a motorcyclist was injured when they collided with a fallen tree. [28] Hagupit brought tropical storm-force winds to the southern portion of the Ryukyu Islands of Japan. Fortunately, no injuries or damage were reported. [29] In the Korean Peninsula, another round of torrential rainfall caused by Hagupit worsened already severe flooding in the area. Up to 5.7 inches (145 mm) of rain was reported in the South Korean city of Suwon. [30] 15 people were reported dead across South Korea, 6 of them following a landslide in South Chungcheong Province, 11 people were reported missing, and 9 people were injured. [31] [32]
The 2008 Pacific typhoon season was a below average season which featured 22 named storms, eleven typhoons, and two super typhoons. The season had no official bounds; it ran year-round in 2008, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
This timeline documents all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation during the 2008 Pacific typhoon season. The 2008 Pacific typhoon season officially started on January 1, 2008 and ended on January 1, 2009.
Typhoon Rammasun, known in the Philippines as Super Typhoon Butchoy, was recognized as the second typhoon of the 2008 Pacific typhoon season by the Japan Meteorological Agency (JMA) and the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA). Rammasun was also recognised as the third tropical storm, the second typhoon and the first super typhoon of the 2008 Pacific typhoon season by the Joint Typhoon Warning Center (JTWC).
Typhoon Hagupit, known in the Philippines as Typhoon Nina, was a powerful cyclone that caused widespread destruction along its path in September 2008. The 21st depression, 14 tropical storm and 10th typhoon of the 2008 Pacific typhoon season, Hagupit developed from a tropical wave located a couple hundred miles east of the Marshall Islands on September 14. Moving generally north-west westwards towards the Philippines, the depression gradually intensified into a tropical storm the following day, and then into became a typhoon on September 22 off the northern coast of Luzon. Located within an environment conducive for strengthening, Hagupit rapidly strengthened to attain 10-min sustained winds of 165 kilometres per hour and 1-min sustained winds of 230 kilometres per hour. After making landfall in Guangdong province in China at peak intensity on September 23, Hagupit rapidly weakened over rugged terrain and dissipated on the 25th.
The 2012 Pacific typhoon season was a slightly above average season that produced 25 named storms, fourteen typhoons, and four intense typhoons. It was a destructive and the second consecutive year to be the deadliest season, primarily due to Typhoon Bopha which killed 1,901 people in the Philippines. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2012, though most tropical cyclones typically develop between May and October. The season's first named storm, Pakhar, developed on March 28, while the season's last named storm, Wukong, dissipated on December 29. The season's first typhoon, Guchol, reached typhoon status on June 15, and became the first super typhoon of the year on June 17.
This timeline documents all of the events of the 2009 Pacific typhoon season which was the period that tropical cyclones formed in the Western Pacific Ocean during 2009, with most of the tropical cyclones forming between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency. Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center. In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.
The 2011 Pacific typhoon season was a below average season that produced a total of 21 named storms, 8 typhoons, and four super typhoons. This season was much more active than the previous season, although both seasons were below the Pacific typhoon average of 26. The season ran throughout 2011, though most tropical cyclone tend to develop between May and October. The season's first named storm, Aere, developed on May 7 while the season's last named storm, Washi dissipated on December 19.
The 2013 Pacific typhoon season was the most active Pacific typhoon season since 2004, and the deadliest since 1975. It featured Typhoon Haiyan, one of the most powerful storms and one of the strongest landfalling tropical cyclones in history. It was an above-average season with 31 named storms, 13 typhoons, and five super typhoons. The season's first named storm, Sonamu, developed on January 4 while the season's last named storm, Podul, dissipated on November 15. Despite the activity, most of the first seventeen named storms before mid-September were relatively weak, as only two of them reached typhoon intensity. Total damage amounted to at least $26.41 billion (USD), making it at the time the costliest Pacific typhoon season on record; it is currently the fourth costliest, behind the 2018, 2019 and 2023 seasons.
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The 2016 Pacific typhoon season is considered to have been the fourth-latest start for a Pacific typhoon season since reliable records began. It was an average season, with a total of 26 named storms, 13 typhoons, and six super typhoons. The season ran throughout 2016, though typically most tropical cyclones develop between May and October. The season's first named storm, Nepartak, developed on July 3, while the season's last named storm, Nock-ten, dissipated on December 28.
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Most of the tropical cyclones of the 2013 Pacific typhoon season formed between May and November of that year. The scope of this article is the Pacific Ocean north of the equator, between 100°E and the International Date Line. Tropical storms which form in the Western Pacific basin are assigned a name by the Japan Meteorological Agency (JMA). Tropical depressions forming in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center (JTWC). The Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility, but these names are not in common use outside the Philippines.
This timeline documents all of the events of the 2014 Pacific typhoon season. Most of the tropical cyclones forming between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency. Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center. In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.
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