Traditional Culture Encyclopedia - Weather inquiry - Which typhoons have landed in Northeast China in history?
Which typhoons have landed in Northeast China in history?
The center of "Blavin" was located at 05: 00 on August 23rd, 2065438 +05: 00 on August 28th, 2065438 on the northwest Pacific Ocean, about 1800 km southeast of Xiangshan County, Zhejiang Province, and landed on the southwest coast of Korea (South Yellow Sea Road) at 20 15: 08. 20 12 landed again at about 22: 50 on August 28th in the south coast of North Pyongan Province in the northwest of Korea.
20 12 weakened into a tropical depression in Tonghe county, Heilongjiang province on August 29th, and the Central Meteorological Observatory stopped numbering it as 17. This typhoon and tembin formed a double typhoon, which led to large-scale heavy rainfall and windy weather in northeast China, North Korea and South Korea.
2. Typhoon Meihua (No.9 super typhoon in 20 1 1 year)
20 1 1 weakened into a tropical depression in Tieling city, Liaoning province at 2 o'clock on August 9. At 2 o'clock, its center is located in Tieling City, Liaoning Province, which is 42.4 degrees north latitude and 124.7 degrees east longitude. The maximum wind force near the center is level 7 (15m/s), and the lowest pressure in the center is 995 hectopascals. It is estimated that "Meihua" will move to the northeast at a speed of about 30 kilometers per hour, and its intensity will continue to weaken.
At 7 o'clock on August 9, 201/kloc-0, its center is located in Changchun City, Jilin Province, that is, 43.8 degrees north latitude and 0/25.6 degrees east longitude. The maximum wind force near the center is 6 (13m/s), and the lowest pressure in the center is 995 hectopascals. After that, the strength continued to weaken, and the impact on China gradually decreased. Central Meteorological Observatory (in China)
3. Typhoon Oulu (No.5 super typhoon on 20 17)
On July 20 17 18, a low pressure area was generated in the northwest waters of wake island. At 08: 00, the U.S. Naval Research Laboratory gave a disturbance number of 95 W.
At 07: 45 on July 17, the Joint Typhoon Warning Center rated its probability of becoming a tropical cyclone in the next 24 hours as "low". 12: 30, Japan Meteorological Agency upgraded it to tropical depression. At 2 1, according to the tropical nature of the system, convection also broke out near the center, and the Japan Meteorological Agency issued a gale warning to it.
At 04: 00 on July 20, 20 17, the joint typhoon warning center raised the probability of becoming a tropical cyclone in the next 24 hours to "medium", and then raised it to "high" at 13, and simultaneously issued an alarm for tropical cyclone generation.
At 05: 00 on July 2 17, joint typhoon warning center upgraded it to a tropical depression with the number of 07W. At 09: 00, Japan Meteorological Agency upgraded it to a tropical storm with the international number 1705, and named it Oulu. At 20: 30, the joint typhoon warning center upgraded it to a tropical storm.
Around July 25th, 20 17, typhoon Rosa in Oulu and its north side produced Fujiwara effect. Because its intensity is much stronger than that of rose, the convective cloud system of rose is absorbed by Oulu circulation, which could have supplemented a lot of energy, but at the same time it also inhaled a lot of dry air and entered the sea area with a sea temperature of about 27℃. These factors further slow down the enhancement speed of Oulu.
At 08: 00 on July 23, 20 17, the Central Meteorological Observatory upgraded it to a severe tropical storm. After 1 hour, Japan Meteorological Agency upgraded it to a severe tropical storm. 17, which was upgraded to a typhoon by the Central Meteorological Observatory. 2 1, the Japan Meteorological Agency upgraded to a typhoon, and at the same time, it was upgraded to a first-class typhoon in conjunction with the Typhoon Warning Center.
4. typhoon goni (No.7 Severe Tropical Storm in 2009)
Swan developed into a tropical depression about 630 kilometers east-northeast of Manila on August 1 2009. It moves westward along the northward ridge of high pressure. Under the influence of strong vertical wind shear, most of the convection of swan is cut off to the South China Sea in the west. As a result, the center of the swan became unstable, and the next day it formed a new center in the northern part of the South China Sea.
Swan intensified into a tropical storm on the night of August 2, 2009, and turned to the northwest. Because the turning flow is weak, the swan path is unstable Swan began to move to the north on August 3, 2009, but it accelerated slightly to the west-northwest direction in the early morning of the next day, but resumed its movement to the north-northwest path in the morning.
Because swan is a large system, it takes time to integrate the circulation, so swan only intensified into a strong tropical storm on the afternoon of August 4, 2009, and reached its peak in the evening, with the highest sustained wind speed of 95 kilometers per hour.
Swan suddenly turned to the west in the early morning of August 5, 2009, crossing the western coastal area of Guangdong. Swan landed in Haiyan Town, Taishan City, Jiangmen City, Guangdong Province on 1 1. Then the swan weakened into a tropical storm at noon, slowly moved to the west-southwest direction and passed Yangjiang. Swan weakened into a tropical depression in the early morning of August 6, 2009.
Swan entered Beibu Gulf on August 7th, 2009. In the environment with sufficient water vapor, Swan re-intensified into a tropical storm on August 8, 2009, and turned southeast to bypass Hainan counterclockwise. Typhoon Morakot swept the southeast coast of China and brought a strong southwest airflow to the South China Sea, which greatly increased the vertical wind shear in this area and inhibited the development of convection.
Swan weakened into a tropical depression again that night, and was influenced by southwest airflow. On August 9, 2009, its low-level circulation center turned to the east-northeast direction, away from its main convection, and circled in the sea off Hainan Island. Finally, Swan weakened into a low pressure area in the northern South China Sea that night.
5. Typhoon Bus No.3 (No.2012 16 Super Typhoon)
201September 1 1 was generated at 08: 00 in the east of the Philippines. At September/6, 2065438 14, the center of Typhoon Sanba was located in the East China Sea about 600 kilometers south of Zhoushan East, Zhejiang Province, that is, 28.8 degrees north latitude, 28.0 degrees east longitude1degree east longitude, with a central pressure of 930 hectopascals and the maximum wind force near the center.
201September 17 weakened into a typhoon around 10 in the south coast of Korea, landed around 1 1 in the southwest of gyeongsangnam-do, South Korea, and landed around 5 o'clock in the south coast of Fujino, Primorsky Krai, Russia.
20 12 and 18 weakened into tropical depression in the east of Heilongjiang in the afternoon, and the central meteorological observatory stopped numbering them 17 on 2012,65438.
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