FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1983716808> ?p ?o ?g. }

• W1983716808 endingPage "606" @default.
• W1983716808 startingPage "587" @default.
• W1983716808 abstract "Abstract In 1986, the Tornado and Storm Research Organisation (TORRO) developed and published an eleven point Hailstorm Intensity Scale and this has been used to characterise more than 2500 hailstorms known to have occurred in Britain and Ireland since the first documented hailstorm event of 1141 AD; this scale has recently (2005) been revised with additional parameters. Most analyses relate to Great Britain, but reference is made to the more extreme recorded events in Ireland. The most intense hailstorm in these Islands reached intensity H8 on the TORRO international scale which extends from intensities H0 to H10. For the 75 years 1930 to 2004 this paper examines significant, damaging (H2 or more intensity) storms in respect of seasonal frequency and geographical distribution. This paper also discusses the climatology (including diurnal incidence) of the less common, but potentially devastating storms of H5 intensity or more, using the much longer period 1800 to 2004 and with particular attention to hail swath lengths and widths. The synoptic origins for these major events, where known, are discussed, with particular reference to Lamb's classification of weather types across the British Isles from 1861 onwards. More than 2500 British and Irish hailstorms are recorded in TORRO's database of which over 1300 are of hailstorm intensity H2 or more, including 156 British storms since 1800 that reached intensity H4–5 or more on the TORRO H scale. The geographical distribution of hailstorms in the British Isles shows that the highest frequency of significant, damaging storms (H2 or more intensity with hailstones usually over 15 mm diameter) is in central and eastern England, with the East Midlands, East Anglia and the lower Thames Valley most conspicuous when the incidences are mapped. Since 1870 the severest (H5 intensity or greater) events have been predominantly associated with cyclonic, southerly or south-easterly weather types; however a significant minority (19%) occurred with an anticyclonic element in the classification. For storms of this severity (e.g. with potential for severe structural damage, pitting of aircraft bodywork and even the risk of serious injuries), reporting will have been more consistent over a longer period. These destructive storms, (the most recent “cluster” of which was between 1992 and 1997) have typically followed a track from the S, SSW or SW to the N, NNE or NE with a swath length often 25 km or more (reaching 335 km in one case) and a swath width sometimes in excess of 10 km. Analysis of the database since 1800 indicates a very conspicuous July maximum for these more extreme (H5 intensity plus) events." @default.
• W1983716808 created "2016-06-24" @default.
• W1983716808 creator A5016465419 @default.
• W1983716808 creator A5065639876 @default.
• W1983716808 creator A5081145081 @default.
• W1983716808 date "2009-07-01" @default.
• W1983716808 modified "2023-09-23" @default.
• W1983716808 title "Severe hailstorms in Britain and Ireland, a climatological survey and hazard assessment" @default.
• W1983716808 cites W1965727834 @default.
• W1983716808 cites W1972886953 @default.
• W1983716808 cites W1973921715 @default.
• W1983716808 cites W1984368005 @default.
• W1983716808 cites W1997145405 @default.
• W1983716808 cites W1999032407 @default.
• W1983716808 cites W2005692691 @default.
• W1983716808 cites W2006709305 @default.
• W1983716808 cites W2010454144 @default.
• W1983716808 cites W2019861107 @default.
• W1983716808 cites W2021363173 @default.
• W1983716808 cites W2022182528 @default.
• W1983716808 cites W2027792511 @default.
• W1983716808 cites W2038522157 @default.
• W1983716808 cites W2045641929 @default.
• W1983716808 cites W2049364730 @default.
• W1983716808 cites W2050297422 @default.
• W1983716808 cites W2052669383 @default.
• W1983716808 cites W2059848819 @default.
• W1983716808 cites W2064974328 @default.
• W1983716808 cites W2066560538 @default.
• W1983716808 cites W2088512525 @default.
• W1983716808 cites W2095304683 @default.
• W1983716808 cites W2120794252 @default.
• W1983716808 cites W2122565126 @default.
• W1983716808 cites W2122696448 @default.
• W1983716808 cites W2126006486 @default.
• W1983716808 cites W2169157318 @default.
• W1983716808 cites W2173079983 @default.
• W1983716808 cites W2175462665 @default.
• W1983716808 cites W2176574844 @default.
• W1983716808 cites W4237129636 @default.
• W1983716808 doi "https://doi.org/10.1016/j.atmosres.2008.10.034" @default.
• W1983716808 hasPublicationYear "2009" @default.
• W1983716808 type Work @default.
• W1983716808 sameAs 1983716808 @default.
• W1983716808 citedByCount "45" @default.
• W1983716808 countsByYear W19837168082013 @default.
• W1983716808 countsByYear W19837168082014 @default.
• W1983716808 countsByYear W19837168082015 @default.
• W1983716808 countsByYear W19837168082016 @default.
• W1983716808 countsByYear W19837168082017 @default.
• W1983716808 countsByYear W19837168082018 @default.
• W1983716808 countsByYear W19837168082020 @default.
• W1983716808 countsByYear W19837168082021 @default.
• W1983716808 countsByYear W19837168082022 @default.
• W1983716808 countsByYear W19837168082023 @default.
• W1983716808 crossrefType "journal-article" @default.
• W1983716808 hasAuthorship W1983716808A5016465419 @default.
• W1983716808 hasAuthorship W1983716808A5065639876 @default.
• W1983716808 hasAuthorship W1983716808A5081145081 @default.
• W1983716808 hasConcept C127313418 @default.
• W1983716808 hasConcept C153294291 @default.
• W1983716808 hasConcept C178790620 @default.
• W1983716808 hasConcept C185592680 @default.
• W1983716808 hasConcept C205649164 @default.
• W1983716808 hasConcept C39432304 @default.
• W1983716808 hasConcept C49204034 @default.
• W1983716808 hasConcept C49261128 @default.
• W1983716808 hasConceptScore W1983716808C127313418 @default.
• W1983716808 hasConceptScore W1983716808C153294291 @default.
• W1983716808 hasConceptScore W1983716808C178790620 @default.
• W1983716808 hasConceptScore W1983716808C185592680 @default.
• W1983716808 hasConceptScore W1983716808C205649164 @default.
• W1983716808 hasConceptScore W1983716808C39432304 @default.
• W1983716808 hasConceptScore W1983716808C49204034 @default.
• W1983716808 hasConceptScore W1983716808C49261128 @default.
• W1983716808 hasIssue "1-3" @default.
• W1983716808 hasLocation W19837168081 @default.
• W1983716808 hasOpenAccess W1983716808 @default.
• W1983716808 hasPrimaryLocation W19837168081 @default.
• W1983716808 hasRelatedWork W1564116264 @default.
• W1983716808 hasRelatedWork W1965953496 @default.
• W1983716808 hasRelatedWork W1967150532 @default.
• W1983716808 hasRelatedWork W2003357297 @default.
• W1983716808 hasRelatedWork W2109926766 @default.
• W1983716808 hasRelatedWork W2145070017 @default.
• W1983716808 hasRelatedWork W2161549781 @default.
• W1983716808 hasRelatedWork W2243996446 @default.
• W1983716808 hasRelatedWork W2748952813 @default.
• W1983716808 hasRelatedWork W2899084033 @default.
• W1983716808 hasVolume "93" @default.
• W1983716808 isParatext "false" @default.
• W1983716808 isRetracted "false" @default.
• W1983716808 magId "1983716808" @default.
• W1983716808 workType "article" @default.