首页|1979-2015年西北太平洋热带气旋的强度与移动速度关系分析

1979-2015年西北太平洋热带气旋的强度与移动速度关系分析

Analysis of the Relationship Between the Intensity and the Velocity of Tropical Cyclones in the Northwest Pacific from 1979 to 2015

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基于6 h西北太平洋热带气旋的强度变化,根据美国联合台风预警中心(joint typhoon warning center,JTWC)1979-2015年西北太平洋热带气旋的最佳路径数据集,研究西北太平洋热带气旋的强度与移动速度关系.结果表明,受地形阻挡,热带气旋登陆后强度减弱,移动速度变小;暖海温有利于热带气旋的发生发展、维持中层水汽充足、维持热带气旋的内部结构.热带气旋的强度与移动速度具有强相关关系,即热带气旋的强度变化越大,其移动速度越慢;快速移动的热带气旋易引起海表温度的负反馈作用,使海面温度降低至热带气旋强度减弱的效果.
Based on the intensity change of tropical cyclones in the Northwest Pacific for 6 hours and the best path data set of tropical cyclones in the Northwest Pacific from 1979 to 2015 from the Joint Typhoon Warning Center(JTWC)of the United States,the relationship between the intensity of tropical cyclones in the Northwest Pacific and the moving speed was studied.The results show that due to the blocking effect of terrain,the tropical cyclones will weaken after landing and the moving speed will slow down.Warm sea temperature is conducive to the occurrence and development of tropical cyclones,maintaining sufficient water vapor in the middle layer and maintaining the internal structure of tropical cyclones.There is a strong correlation between the intensity of tropical cyclone and its moving speed,that is,the greater the intensity of tropical cyclone changes,the slower its moving speed.Rapidly moving tropical cyclones tend to cause negative feedback of sea surface temperature,for the cooling of the sea surface can reduce the intensity of tropical cyclones.

tropical cycloneintensityvelocity

喇楠、谢智沛、武莹、牛宏宇、殷子月

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中国气象局旱区特色农业气象灾害监测预警与风险管理重点实验室,宁夏银川 750002

宁夏气象防灾减灾重点实验室,宁夏银川 750002

吴忠红寺堡区气象站,宁夏吴忠 751999

惠水县气象局,贵州 惠水 550600

石嘴山市气象局,宁夏 石嘴山 753000

乌鲁木齐市气象局,新疆 乌鲁木齐 830001

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热带气旋 强度 移动速度

中国气象局旱区特色农业气象灾害监测与风险管理重点实验室青年培养基金

CAMT-202108

2023

宁夏大学学报(自然科学版)
宁夏大学

宁夏大学学报(自然科学版)

CSTPCD
影响因子:0.377
ISSN:0253-2328
年,卷(期):2023.44(4)
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