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2
Content available remote Pokrycie dachu z folii PVC zniszczone przez grad
PL
W wyniku opadu gradu w trakcie majowej burzy w 2014 r. nastąpiła perforacja pokrycia z membrany PVC na dachu sześcioletniej hali przemysłowej oraz budynku socjalno-technicznego i administracyjnego. Zalanie hali po uszkodzeniu pokrycia było wynikiem błędnego zaprojektowania połączenia blach T55 z obudową ścian zewnętrznych i z płatwiami. Małe pochylenie połaci dachowej uniemożliwiło zmianę pokrycia z membrany PVC na blaszane.
EN
PVC roof membrane covering the six-year old industrial building, social and technical building as well as office building as a result of heavy spring hailstorm in May 2014 was perforated. Flooding industrial hall after damage of roofing resulted from incorrect design of connection between steel sheet T55 and purlin as well as external fittings. Small slope of roofing disabled change the PVC membrane on the new cover steel sheet.
3
EN
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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