从2007年到2015年,波兰出现了非常大的冰雹

Wojciech Pilorz
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引用次数: 5

摘要

超大冰雹是指存在直径大于或等于5厘米的冰雹。这种现象很少见,但它的严重后果,不仅对农业,而且对汽车,家庭和户外的人,使它成为必须研究的问题。冰雹的出现与风暴的频率和种类密切相关。最危险的风暴是超级单体风暴。将冰雹的地理分布与波兰风暴的地理分布进行了比较。发现了相似之处。风暴数量最多的地区是波兰东南部。分析欧洲恶劣天气数据库(ESWD)的数据显示,大部分特大冰雹报告发生在波兰的这一地区。造成这种情况的可能原因是波兰东南部热带气团持续时间最长。空间分布分析还显示,上西里西亚、小波兰、下喀尔巴阡和Świętokrzyskie地区的冰雹事件较多。冰雹发生的信息来源是ESWD -开放数据库,每个人都可以添加报告并查找符合给定搜索条件的报告。对2007 - 2015年期间的69次冰雹进行了分析。它们造成了121次特大冰雹报告。研究发现,冰雹和冰雹报告的数量在个别年份之间存在较大的不均衡。波兰的大冰雹季节从5月开始,9月结束,7月积累。大部分冰雹发生在世界标准时间12:00至17:00之间,但也有一些非常大(一个特大)的冰雹发生在夜间和清晨。然而,特大冰雹是一种非常壮观的现象,其局部性决定了其潜在的高信息损失率,是冰雹研究中最重要的问题。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Very large hail occurrence in Poland from 2007 to 2015
Abstract Very large hail is known as a presence of a hailstone greater or equal to 5 cm in diameter. This phenomenon is rare but its significant consequences, not only to agriculture but also to automobiles, households and people outdoor makes it essential thing to examine. Hail appearance is strictly connected with storms frequency and its kind. The most hail-endangered kind of storm is supercell storm. Geographical distribution of hailstorms was compared with geographical distribution of storms in Poland. Similarities were found. The area of the largest number of storms is southeastern Poland. Analyzed European Severe Weather Database (ESWD) data showed that most of very large hail reports occurred in this part of Poland. The probable reason for this situation is the longest period of lasting tropical airmasses in southeastern Poland. Spatial distribution analysis shows also more hail incidents over Upper Silesia, Lesser Poland, Subcarpathia and Świętokrzyskie regions. The information source about hail occurrence was ESWD - open database, where everyone can add report and find reports which meet given search criteria. 69 hailstorms in the period of 2007 - 2015 were examined. They caused 121 very large hail reports. It was found that there is large disproportion in number of hailstorms and hail reports between individual years. Very large hail season in Poland begins in May and ends in September with cumulation in July. Most of hail occurs between 12:00 and 17:00 UTC, but there were some cases of very large (one extremely large) hail at night and early morning hours. However very large hail is a spectacular phenomenon, its local character determines potentially high information loss rate and it is the most significant problem in hail research.
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