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INLAND PENETRATION OF SEA BREEZE IN THE COASTAL ZONE OF THE NORTHWESTERN BLACK SEA

机译:西北黑海沿岸海域海风的内陆渗透

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摘要

Radar and synoptic data from the Anti-Hail Service, Republic of Moldova, for 1987-2000 were used to study the depth of inland penetration of a sea breeze and related convection intensity in the coastal zone of the northwestern Black Sea (southwest of Odessa region of Ukraine and southern Moldova). Inland penetration of a sea breeze was classified into five types. The most intense convection is connected with the second type of penetration. The maximum frequency of hail clouds is also observed there (44.1%). The integral picture of the radar echo from cumulonimbus clouds (RECC) is compared with different types of inland penetration of a sea breeze. It is shown that the RECC structures developing in the coastal zone are independent of the type of inland penetration of a sea breeze.
机译:使用来自摩尔多瓦共和国防雹服务的1987-2000年雷达和天气数据,研究了黑海西北部沿海地区(敖德萨地区西南部)海风向内陆渗透的深度和相关的对流强度乌克兰和摩尔多瓦南部)。海风向内陆的渗透分为五种类型。最强烈的对流与第二种类型的穿透有关。那里也观察到冰雹云的最大频率(44.1%)。将积雨云(RECC)产生的雷达回波的完整图片与海风向内陆的不同类型进行了比较。结果表明,沿海岸带发展的RECC结构与海风向内陆渗透的类型无关。

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