Matches in SemOpenAlex for { <https://semopenalex.org/work/W3050350634> ?p ?o ?g. }
- W3050350634 endingPage "3771" @default.
- W3050350634 startingPage "3747" @default.
- W3050350634 abstract "Abstract This paper investigates the transient characteristics in 41 velocity records of 19 thunderstorm events from around the world—9 from Europe, 9 from the United States, and 1 from Australia. The transient features of thunderstorm winds were examined by introducing an objective method for the detection of changepoints in the time series. The methodology divides velocity records into segments characterized by different statistical properties. The segmentation is based on the following properties of the isolated segments: mean (M) and the standard deviation (SD). This study demonstrated that the maximum velocity during the thunderstorm peak in the events from Europe is typically 2–4 times larger than the mean wind speed before the thunderstorm. The duration of the thunderstorm velocity peak was 2–5 min in approximately 60% of the analyzed records using the M statistic and 5–10 min when analyzed using the SD statistic. Therefore, the velocity fluctuations caused by thunderstorm winds last longer than the abrupt changes in the mean wind field. Similarly, the ramp-up time was longer when the records were analyzed using the SD statistic. The segmentation methodology was tested for different duration of velocity records and using data with different sampling frequencies. The performances of the introduced method were compared against the results of two other segmentation procedures proposed in the literature. One of the practical applications of this method is the physical separation between the thunderstorm and nonthunderstorm components of a wind event. Significance Statement Thunderstorm outflow winds are short-lived phenomena produced by cold downdrafts that originate in thunderstorm clouds. This study analyzes the transient nature of thunderstorm winds from Europe, the United States, and Australia using a segmentation method applied to anemometer velocity records. This segmentation method identifies abrupt changes of mean wind speed and wind fluctuations in the velocity data. This research provides the means of isolating different segments within the thunderstorm wind records in an objective way that is based on rigorous mathematical principles. The proposed method can automatically distinguish thunderstorm from nonthunderstorm winds. The peak velocities in thunderstorm outflows are 2–4 times the mean wind speed before the thunderstorm. The most intense episodes of thunderstorm winds usually last 2–5 min." @default.
- W3050350634 created "2020-08-24" @default.
- W3050350634 creator A5011380729 @default.
- W3050350634 creator A5014066848 @default.
- W3050350634 creator A5065445166 @default.
- W3050350634 creator A5078391287 @default.
- W3050350634 date "2020-08-26" @default.
- W3050350634 modified "2023-09-28" @default.
- W3050350634 title "Investigation of the Transient Nature of Thunderstorm Winds from Europe, the United States, and Australia Using a New Method for Detection of Changepoints in Wind Speed Records" @default.
- W3050350634 cites W1608031639 @default.
- W3050350634 cites W1975684011 @default.
- W3050350634 cites W1982445297 @default.
- W3050350634 cites W1985277880 @default.
- W3050350634 cites W1990470333 @default.
- W3050350634 cites W2001641529 @default.
- W3050350634 cites W2003743091 @default.
- W3050350634 cites W2013389119 @default.
- W3050350634 cites W2019586532 @default.
- W3050350634 cites W2022827183 @default.
- W3050350634 cites W2027748823 @default.
- W3050350634 cites W2028285658 @default.
- W3050350634 cites W2043768836 @default.
- W3050350634 cites W2048665316 @default.
- W3050350634 cites W2053890797 @default.
- W3050350634 cites W2061532673 @default.
- W3050350634 cites W2062296968 @default.
- W3050350634 cites W2086182614 @default.
- W3050350634 cites W2087794968 @default.
- W3050350634 cites W2088590021 @default.
- W3050350634 cites W2089135536 @default.
- W3050350634 cites W2092159048 @default.
- W3050350634 cites W2106822551 @default.
- W3050350634 cites W2117227640 @default.
- W3050350634 cites W2172163876 @default.
- W3050350634 cites W2172176129 @default.
- W3050350634 cites W2173682680 @default.
- W3050350634 cites W2177751923 @default.
- W3050350634 cites W2177824836 @default.
- W3050350634 cites W2251053774 @default.
- W3050350634 cites W2303319653 @default.
- W3050350634 cites W2598203838 @default.
- W3050350634 cites W2610284820 @default.
- W3050350634 cites W2612130841 @default.
- W3050350634 cites W2621237610 @default.
- W3050350634 cites W2734569259 @default.
- W3050350634 cites W2747221121 @default.
- W3050350634 cites W2781716665 @default.
- W3050350634 cites W2793048823 @default.
- W3050350634 cites W2799481890 @default.
- W3050350634 cites W2902005811 @default.
- W3050350634 cites W2919599859 @default.
- W3050350634 cites W2967050714 @default.
- W3050350634 cites W3098618426 @default.
- W3050350634 cites W4213338549 @default.
- W3050350634 cites W4251807571 @default.
- W3050350634 cites W625327783 @default.
- W3050350634 cites W639907764 @default.
- W3050350634 doi "https://doi.org/10.1175/mwr-d-19-0312.1" @default.
- W3050350634 hasPublicationYear "2020" @default.
- W3050350634 type Work @default.
- W3050350634 sameAs 3050350634 @default.
- W3050350634 citedByCount "8" @default.
- W3050350634 countsByYear W30503506342020 @default.
- W3050350634 countsByYear W30503506342021 @default.
- W3050350634 countsByYear W30503506342022 @default.
- W3050350634 countsByYear W30503506342023 @default.
- W3050350634 crossrefType "journal-article" @default.
- W3050350634 hasAuthorship W3050350634A5011380729 @default.
- W3050350634 hasAuthorship W3050350634A5014066848 @default.
- W3050350634 hasAuthorship W3050350634A5065445166 @default.
- W3050350634 hasAuthorship W3050350634A5078391287 @default.
- W3050350634 hasBestOaLocation W30503506341 @default.
- W3050350634 hasConcept C105795698 @default.
- W3050350634 hasConcept C111919701 @default.
- W3050350634 hasConcept C127313418 @default.
- W3050350634 hasConcept C153294291 @default.
- W3050350634 hasConcept C161067210 @default.
- W3050350634 hasConcept C205649164 @default.
- W3050350634 hasConcept C2780799671 @default.
- W3050350634 hasConcept C33923547 @default.
- W3050350634 hasConcept C39432304 @default.
- W3050350634 hasConcept C41008148 @default.
- W3050350634 hasConcept C49204034 @default.
- W3050350634 hasConcept C80316258 @default.
- W3050350634 hasConcept C89128539 @default.
- W3050350634 hasConceptScore W3050350634C105795698 @default.
- W3050350634 hasConceptScore W3050350634C111919701 @default.
- W3050350634 hasConceptScore W3050350634C127313418 @default.
- W3050350634 hasConceptScore W3050350634C153294291 @default.
- W3050350634 hasConceptScore W3050350634C161067210 @default.
- W3050350634 hasConceptScore W3050350634C205649164 @default.
- W3050350634 hasConceptScore W3050350634C2780799671 @default.
- W3050350634 hasConceptScore W3050350634C33923547 @default.
- W3050350634 hasConceptScore W3050350634C39432304 @default.
- W3050350634 hasConceptScore W3050350634C41008148 @default.
- W3050350634 hasConceptScore W3050350634C49204034 @default.
- W3050350634 hasConceptScore W3050350634C80316258 @default.
- W3050350634 hasConceptScore W3050350634C89128539 @default.