| 注册
首页|期刊导航|海洋气象学报|2022年春季浙江一次持续性海雾过程的特征及成因

2022年春季浙江一次持续性海雾过程的特征及成因

傅方奇 杜雪婷 王健捷 钱艳珍 俞燎霓

海洋气象学报2024,Vol.44Issue(3):78-86,9.
海洋气象学报2024,Vol.44Issue(3):78-86,9.DOI:10.19513/j.cnki.hyqxxb.20230131001

2022年春季浙江一次持续性海雾过程的特征及成因

Characteristics and causes of a persistent sea fog process over Zhejiang in spring 2022

傅方奇 1杜雪婷 1王健捷 2钱艳珍 3俞燎霓1

作者信息

  • 1. 浙江省气象台,浙江杭州 310017
  • 2. 宁波市鄞州区气象局,浙江宁波 315194
  • 3. 宁波市气象台,浙江宁波 315012
  • 折叠

摘要

Abstract

From 10 to 14 April 2022,a long-duration,wide-range and high-concentration sea fog event occurred in the coastal waters of Zhejiang.The characteristics and causes are analyzed by using satellite data,ECMWF(European Centre for Medium-Range Weather Forecasts)Reanalysis-Interim(ERA-Interim)data and data of coastal automatic meteorological observing stations in Zhejiang.The results show that the inversion layer makes it difficult for the low-level water vapor to spread to the upper air,which is conducive to the generation and maintenance of fog.In the fog formation stage,there is obvious water vapor convergence,and at the same time,the air temperature is higher than SST(sea surface temperature)and the difference is between 0 and 2.0 ℃.When the sea fog maintains and the concentration is high,the water vapor convergence gradually weakens,and the air-sea temperature difference(Δt=ta-ts)is around 0℃.In the dissipation stage,there is obvious water vapor divergence;the air-sea temperature difference is greater than 2.0 ℃ or less than 0 ℃.

关键词

海雾/逆温层/水汽输送/气海温差

Key words

sea fog/inversion layer/transfer of water vapor/air-sea temperature difference

分类

天文与地球科学

引用本文复制引用

傅方奇,杜雪婷,王健捷,钱艳珍,俞燎霓..2022年春季浙江一次持续性海雾过程的特征及成因[J].海洋气象学报,2024,44(3):78-86,9.

基金项目

浙江省气象局科研项目(2023ZD02,2021YBY01) (2023ZD02,2021YBY01)

国家自然科学基金项目(42105135) (42105135)

宁波市公益性科技计划重点项目(2022S181) (2022S181)

海洋气象学报

2096-3599

访问量0
|
下载量0
段落导航相关论文