首页|Evolution Mechanism of a Severe Squall Line Triggered by the Coupling of a Sea Breeze Front and a Gust Front

Evolution Mechanism of a Severe Squall Line Triggered by the Coupling of a Sea Breeze Front and a Gust Front

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In the present study,a severe squall line(SL)was analyzed by using intensive observational surface data and radar monitoring products.In this process,mesoscale convergence lines,such as the sea breeze front(SBF),gust front and dry line,served as the main triggering and strengthening factors.The transition from convection triggering to the formation of the initial shape was mainly affected by the convergence line of the SBF,which combined with thermal convection to form the main parts of the SL.In the later stage,the convergence line of the gust front merged with other convergence lines to form a series of strong convective cells.The SBF had good indicative significance in terms of severe convective weather warnings.The suitable conditions of heat,water vapor and vertical wind shear on the Shandong Peninsula were beneficial to the maintenance of the SL.Before SL occurrence,tropopause folding strengthened,which consequently enhanced the baroclinic property in the middle and upper troposphere.The high sensible heat flux at the surface easily produced a positive potential vorticity anomaly in the low layer,resulting in convective instability,which was conducive to the maintenance of these processes.In the system,when precipitation particles passed through the unsaturated air layer,they underwent strong evaporation,melting or sublimation,and the cooling effect formed negative buoyancy,which accelerated the sinking of the air and promoted the sustained development of the surface gale.Together with the development of low-level mesocyclones,the air pressure decreased rapidly,which was conducive to gale initiation.

squall linesea breeze frontgust frontcold poolthunderstorm gale

万夫敬、孙敏、庞华基、赵海军、赵传湖

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Qingdao Meteorological Bureau,Qingdao,Shandong 266003 China

Shanghai Central Meteorological Observatory,Shanghai 200030 China

Linyi Meteorological Bureau,Linyi,Shandong 276037 China

Frontier Science Center for Deep Ocean Multispheres and Earth System(FDOMES)and Physical Oceanography Laboratory,Ocean University of China,Qingdao,Shandong 266101 China

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Natural Science Foundation of Shandong ProvinceNatural Science Foundation of Shandong ProvinceNatural Science Foundation of Shandong ProvinceNational Natural Science Foundation of ChinaShandong Meteorological Bureau Innovation Team ProjectHuaihe River Meteorology Open Research FundKey Special Project of Qingdao Meteorological Bureau

ZR2021MD062ZR2021MD010ZR2023MD11842275001SDCXTD2023-1HRM2018072023qdqxz02

2024

10.3724/j.1006-8775.2024.018

热带气象学报(英文版)
中国气象局广州热带海洋气象研究所

热带气象学报(英文版)

影响因子：0.169
ISSN：1006-8775
年,卷(期)：2024.30(2)