###
DOI:
本文二维码信息
一次1月山东半岛东部极端海效应暴雪的机制分析
李刚1, 刘畅2, 曹玥瑶2, 孟宪贵2
(1.山东省气象局;2.山东省气象台)
Case Study on Generation Mechanism of Extreme Ocean-effect Snowstorm in the East of Shandong Peninsula in January
LI Gang1, LIU Chang2, CAO Yueyao2, Meng Xiangui2
(1.Shandong Meteorological Bureau,Ji’nan;2.Shandong Meteorological Observatory,Ji’nan)
摘要
相似文献
本文已被:浏览 495次   下载 125
投稿时间:2019-05-17    修订日期:2020-03-03
中文摘要: 利用海上浮标站、自动站、多普勒天气雷达、L波段雷达探空、NCEP/NCAR再分析逐6h和降水等观测资料,结合EVAP雷达风场反演获得的水平风场资料,对2018年1月9—11日一次渤海海效应暴雪过程的产生机制进行了分析。结果表明:(1)此次海效应暴雪过程是一次极端降雪事件,具有强降雪持续时间长、降雪量大、暴雪分布近中-γ尺度等特征。(2)暴雪发生前后有两次强冷空气影响,造成渤海和山东半岛地区持续降温,850hPa温度降至-16~-18℃,是产生强海效应降雪的有利条件;此次冷空气强度明显低于12月份渤海海效应暴雪,1月份产生海效应暴雪的冷空气强度中位数较12月份低约5℃。(3)强冷空气影响时,海气温差明显增大,海洋向低层大气输送的最大感热通量可达226.8 W×m-2,低层大气高湿饱和,导致大气层结不稳定,不稳定局限于850hPa以下,为浅层对流。(4)雷达反射率因子图上具有明显的“列车效应”。造成窄带回波的原因在于出现了低层切变线,即在山东半岛北部沿海的小范围区域内出现了东北风及西西南风,形成了西北风与东北风、西西南风与东北风的切变线,触发暴雪产生。而东北风达到的高度不超过1.2km,多在0.6km以下。通过此次极端暴雪过程的综合观测资料分析,揭示了较少出现的1月份海效应暴雪的特征,其形成的环流形势、热力不稳定、动力条件等与常见的12月份海效应暴雪基本类似,主要差异在于冷空气强度较12月份偏强,这可成为1月份海效应暴雪的首要预报着眼点;海上浮标站、雷达风场反演技术是定量揭示海效应暴雪中尺度特征的良好资料和方法。
Abstract:Analysis is conducted on the generation mechanism of ocean-effect snowstorm in Bohai which occurred from 9 to 11 January 2018,using multiple observation data of buoy station, automatic weather station, Doppler weather radar L-band radar, NCEP/NCAR 6h reanalysis and precipitation, combined with horizontal wind data retrieved from EVAP technology. The results are as follows: Firstly, this ocean-effect snowstorm process is an extreme snowfall event,characterized by long duration of heavy snowfall, large snowfall and near mid-γ scale distribution of heavy snowfall. Secondly, temperature of Bohai and Shandong Peninsula decreased continuously caused by two strong cold air effect before and after snowstorm, the 850hPa temperature dropped to -16~-18℃ which is helpful to the strong ocean-effect snowstorm generation; the cold air intensity of this process is obviously weaker than December ocean-effect snowstorm. It is said that the median cold air intensity of January ocean-effect snowstorm is about 5℃ lower than December. Thirdly, obvious difference of air and sst leads to prominent sense heat flux with maximum 226.8 W×m-2 when strong cold air flows, convective instability occurs over Bohai and the coastal areas of Northern Shandong Peninsula. It’s a thin convective limited below 850hPa. There is an obvious thermal ridge of pseudo-equivalent potential temperature during the snowstorm. Lastly, the radar reflectivity factor graphs shows obvious “Train Effect”. NE and WSW wind appear over a small coastal area of Northern Shandong Peninsula causing wind direction shear of NW and NE, WSW and NE. The lower shear line leads to the narrow-band echo which triggered the snowstorm. And the NE wind reaches the height of less than 1.2km, usually under 0.6km. Characteristics of January ocean-effect snowstorm that less appeared is revealed though the study of this extreme snowstorm process, its characteristics such as the circulation pattern, thermal instability and dynamical condition are similar to the December ocean-effect snowstorm’s, the major difference is that the cold air intensity is stronger than the December’s which should be the primary forecasting focus of January ocean-effect snowstorm. Bouy data and EVAP radar retrieved wind can reveal quantitatively meso-scale character of ocean-effect snowstorm.
文章编号:201905170212     中图分类号:P426    文献标志码:
基金项目:国家自然科学基金项目(面上项目,重点项目,重大项目)
引用文本:
李刚,刘畅,曹玥瑶,孟宪贵,0.[en_title][J].Meteor Mon,():-.
LI Gang,LIU Chang,CAO Yueyao,Meng Xiangui,0.Case Study on Generation Mechanism of Extreme Ocean-effect Snowstorm in the East of Shandong Peninsula in January[J].Meteor Mon,():-.