Traditional Culture Encyclopedia - Weather forecast - What is the biggest and strongest typhoon in the history of the world?
What is the biggest and strongest typhoon in the history of the world?
The biggest and strongest typhoon in the history of the world: Taipei
Typhoon Taibei (English: Typhoon Tip, translated by Taiwan Province Province: Dipu) is a tropical cyclone with the largest influence range, the second strongest intensity and the lowest sea surface pressure in the west of the North Pacific. The joint typhoon warning center called it the super typhoon tip. This typhoon caused massive floods in Japan from 65438 to 0979. The typhoon at that time was never named in Japan, so the Japanese Meteorological Observatory called it Typhoon No.20 at that time, and it was recorded as Typhoon No.20 in Showa in 54 years.
The Development Process of Typhoon Taipei
Typhoon tip is a tropical cyclone with the largest influence range (the second largest is Typhoon Ute) and the strongest intensity. It is called super typhoon tip because it is located in the western Pacific Ocean. This typhoon caused massive floods in Japan from 65438 to 0979. The typhoon at that time was never named in Japan, so the Japanese Meteorological Observatory called it Typhoon No.20 at that time, and it was recorded as Typhoon No.20 in Showa in 54 years. At the beginning of 1979 10, the monsoon trough in the northwest Pacific Ocean and the South China Sea was quite wide and active, and there were three disturbances in the trough, namely Typhoon Sarah, Tropical Storm Roger and Typhoon Tip. Typhoon Sada affected the South China Sea and moved generally westward. The highest wind force in its center reaches 205 kilometers per hour, which has no influence on Taipei. However, tropical storm Roger interacted with Taipei more, affecting the northwest Pacific ocean east of east longitude 135 degrees, and the highest wind force at its center reached 85 kilometers per hour.
In the early days of typhoon Taipei's formation
Roger was first formed in the morning of 65438+1October 2, about 300 kilometers southwest of Guam, and intensified into a tropical depression in the afternoon about 420 kilometers west of Guam. Roger then intensified into a tropical storm on 10/0/October 4, and reached its peak in the afternoon of the same day, with the highest wind force in the center reaching 85 kilometers per hour. On the same day, Taipei was formed about 300 kilometers southeast of Zhuoke Island (6.3 degrees north latitude and 154. 1 degree east longitude). Joint typhoon warning center issued a tropical cyclone warning (TCFA) to it, and then it intensified into a tropical depression about190km southeast of Zhuoke Island. At that time, influenced by Roger, who was quite mature, he slowly moved to the southeast.
Influenced by Roger, the monsoon trough extends to east longitude 160 degrees. At that time, there was a broad and powerful air flow across the southwest of the equator, indicating that the monsoon trough was extremely active at that time. However, Roger was stronger and took away most of the water vapor and radiation confluence brought by the southwest monsoon, so the initial development of Taipei was suppressed.
Start strengthening and go straight to Guam.
Tropical storm Roger moved to the mid-latitude area on June 6 10, and its impact on Taipei was relatively reduced, so Taipei gradually strengthened and intensified into a tropical storm on June 6 10. Roger moved near Japan on1October 7 10, weakened obviously, entered the westerly belt and turned into an extratropical cyclone.
With the weakening of Roger, the east longitude 135 degrees to 140 degrees, from the equator to Roger center, became a wide trough of low pressure and a large saddle-shaped field. There is a strong subtropical ridge in the east of the ground trough and a continental anticyclone in the west, so the southwest monsoon will concentrate and converge strongly between the troughs. When Taipei moves into the trough, it can get strong large-scale convergence and high temperature and high humidity water vapor support. Affected by the strong subtropical ridge east of the ground trough, Taipei moved roughly to the west-northwest and moved to Guam. It strengthened slowly and intensified into a severe tropical storm on the afternoon of June 54381October 8. Later, I went straight to Guam, posing a serious threat to Guam (Guam is the headquarters of the Joint Typhoon Warning Center), so the Joint Typhoon Warning Center made 60 aircraft observations. 654381on the afternoon of October 9 10, Taipei passed about 46 kilometers south of Guam, and it was stormy, with an average wind speed of 90 kilometers per hour and gusts of 1 18 kilometers per hour.
Outbreak enhancement
After passing through the waters south of Guam, Taipei further strengthened into a typhoon on the afternoon of June 5438+1October 9. Later, Taipei moved to the strong convergence and high-altitude divergence area composed of the southwest monsoon and high-level anticyclone, which strengthened rapidly. At that time, its enhancement speed was faster than expected. During the period from June 9 10 to June 9 1 1, the air pressure in Taipei center dropped by 98 hectopascals. 65438+1October 1 1 day, Taipei was further strengthened and was assessed as a super typhoon by the Joint Typhoon Warning Center, with a central wind force of 240 kilometers per hour. On June 65438+1October 1 1, Taipei turned to the northwest and moved.
The Disaster Impact of Typhoon Taipei
Influence on Japan
? 1 10 people died, 5 people were missing and 543 people were injured.
? 65,438+039 houses collapsed and another 65,438+0,287 houses were damaged.
? There are 8 157 buildings under the bed and 47943 buildings under the bed.
? Cultivated land was affected by 2545 1 hectare.
? 19 Ship injured.
After reaching the top speed, Taipei gradually weakened and approached the coast of Japan. A large amount of uninterrupted precipitation has caused many landslides and mudslides in Honshu Island. Taipei weakened into a tropical storm and landed in Japan on June 10. Taipeiyi * * * caused 1 10 deaths and caused millions of dollars in heavy losses to Japanese agriculture and fisheries.
Influence on Fujian Province of China
Wind and rain and disaster in Quanzhou: generally speaking, wind disaster is the main disaster.
No.79 19 "Typhoon Taipei" was a turning typhoon, and typhoon Taipei occurred at 08: 00 on 10/9.
When Japan landed, the wind force exceeded 12. During the influence period, the coastal winds in Fujian Province reached 6~7, and the gusts were 8~9. Affected by cold air and typhoon * * *, northerly winds blow almost every day along the northern coast of Pingtan from 1 1 to 18, and the duration is unprecedented since liberation.
Disaster situation in the whole province: strong winds are very destructive to fisheries and cause heavy losses. According to Pingtan County's report, the gale broke sailboats 1 boat, damaged 123 boats, broke 42 wooden boats, damaged 55 boats, broke or lost 4 18 fishing nets, and the artificially cultured laver was rejected by 2.526 mu, affecting about 25,000 people.
Disaster of Typhoon Taipei
1 10 people died, 5 people were missing and 543 people were injured.
65,438+039 houses collapsed and another 65,438+0,287 houses were damaged.
There are 8 157 buildings under the bed and 47943 buildings under the bed.
Cultivated land was affected by 2545 1 hectare.
19 Ship injured.
After reaching the top speed, Taipei gradually weakened and approached the coast of Japan. A large amount of uninterrupted precipitation has caused many landslides and mudslides in Honshu Island. In the end, Taipei weakened into a weak storm and landed in Japan on 10/9, but the loss was not small. Taipeiyi * * * caused 1 10 deaths and caused millions of dollars in heavy losses to Japanese agriculture and fisheries.
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