首页|期刊导航|中国海洋大学学报(自然科学版)|利用毫米波和激光雷达资料对2024年4月黄海西部一次海雾过程的结构特征分析

利用毫米波和激光雷达资料对2024年4月黄海西部一次海雾过程的结构特征分析OA

Analyses of Structural Characteristics of a Sea Fog Event over the Western Yellow Sea in April,2024 by Using the Millimeter-Wave Radar and Lidar Data

中文摘要英文摘要

本文利用毫米波雷达数据、激光雷达数据、常规气象观测数据和ERA5客观再分析数据,对2024年4月发生在黄海西部的一次海雾过程进行观测分析,结果表明:受海上高压后部暖湿气流影响,2024年4月12日至15日青岛及近海海域出现长达4天的海雾过程,海雾发展期间气海温差适宜,海气界面稳定,适宜的逆温条件、大气边界层内弱风切变和高静力稳定度,有利于海雾的发展和维持.安置于黄岛国家基本气象站的激光雷达较好地监测到了海雾生成阶段向岸发展的过程和生消阶段的大气能见度变化趋势,但在海雾发展旺盛阶段探测衰减严重.毫米波雷达捕捉到了不同发展阶段的海雾垂直结构特征,生成阶段雾体回波在0.5 km以下,雾顶的长波辐射冷却导致雾顶边缘的反射率因子明显低于中下层,抑制着雾顶的向上发展.发展旺盛阶段,在雾层内部非雾顶和雾底区出现细碎的、不规则的亮暗波动,推测可能与雾中的小湍流运动有关.发展后期,雾滴的碰并增长与下沉使得回波出现类似弱降水对流性特征的丝缕状结构,回波高度升至1.2 km以上,不再有利于海雾的维持和发展.利用常规气象观测设备与新型观测设备相互补充进行观测,有利于加深黄海海雾结构特征的认识.

Using the millimeter-wave radar and lidar data,conventional meteorological observation da-ta,and ERA5 reanalysis data,the authers conducted observational analyses of a sea fog event that oc-curred over the western Yellow Sea in April,2024.A prolonged sea fog event lasting four days on April 12-15,2024 occurred in Qingdao and its adjacent coastal waters.It influenced by warm and moist air-flows behind the maritime high-pressure system.During the fog development stage,favorable air-sea temperature difference,stable air-sea interface,suitable conditions of inversion layer,weak wind shear within the atmospheric boundary layer,and high static stability collectively facilitated the development and maintenance of the sea fog.The lidar deployed at Huangdao National Basic Meteorological Station successfully captured the variation trend of atmospheric visibility throughout the fog's formation and dissipation processes.It also captured the onshore propagation of sea fog during its formation stage.However,significant detection attenuation was observed during the mature stage of sea fog event.The millimeter-wave radar revealed the vertical structural characteristics of this sea fog event at different de-velopmental stages.During the formation stage,see fog echo signals were detected below 0.5 km.Longwave radiative cooling at the fog top resulted in a significantly lower reflectivity factor at the fog top edge compared to the middle and lower layers,inhibiting the upward expansion of the fog top.Dur-ing the mature stage,fine and irregular bright-dark fluctuations emerged within the non-top and non-bottom regions of the fog layer.This phenomenon might have been closely associated with small-scale turbulent motions inside the fog.In the late stage,the coalescence and growth of fog droplets followed by sinking led to echo signals exhibiting a filamentous structure similar to the convective features of weak precipitation,with the echo height rising above 1.2 km.At this time,the conditions were no lon-ger conducive to the maintenance and development of the sea fog.The combined application of conven-tional and new observational equipment,leveraging their complementary advantages,may contribute to an in-depth understanding of the structural characteristics of sea fog over the Yellow Sea.

鄢珅;时晓曚;吴凤远;雷勇;王倩;高荣珍

青岛市气象局,山东 青岛 266003青岛市气象局,山东 青岛 266003成都信息工程大学,四川 成都 610225中国气象局气象探测中心,北京 100081青岛市气象局,山东 青岛 266003青岛市气象局,山东 青岛 266003

海洋科学

毫米波雷达资料激光雷达资料黄海海雾大气能见度

millimeter-wave radar datalidar datasea fog over the Yellow Seaatmospheric visibility

《中国海洋大学学报(自然科学版)》 2026 (7)

23-34,12

山东省自然科学基金项目(ZR2024LQX004)中国气象局创新发展专项项目(CXFZ2025Q001)环渤海区域海洋气象科技协同创新项目(QYXM202412)项目青岛市气象局科研项目(2025qdqxq04,2026qdqxzl-04)资助 Supported by Shandong Provincial Natural Science Foundation(ZR2024LQX004)China Meteorological Administration Innovation and Development Special Project(CXFZ2025Q001)Bohai Sea Rim Collaborative Innovation Project of Marine Meteorological Tech-nology(QYXM202412)Qingdao Meteorological Bureau Research Project(2025qdqxq04,2026qdqxzl-04)

10.16441/j.cnki.hdxb.20250217

评论