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1000 Titel
  • Convection-permitting climate model representation of severe convective wind gusts and future changes in southeastern Australia
1000 Autor/in
  1. Brown, Andrew |
  2. Dowdy, Andrew |
  3. Lane, Todd P. |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-09-24
1000 Erschienen in
1000 Quellenangabe
  • 24(9):3225-3243
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/nhess-24-3225-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. Previous research has suggested that the frequency and intensity of surface hazards associated with thunderstorms and convection, such as severe convective winds (SCWs), could potentially change in a future climate due to global warming. However, because of the small spatial scales associated with SCWs, they are unresolved in global climate models, and future climate projections are uncertain. Here, we evaluate the representation of SCW events in a convection-permitting climate model (Bureau of Meteorology Atmospheric Regional Projections for Australia, BARPAC-M) run over southeastern Australia for the months of December–February. We also assess changes in SCW event frequency in a projected future climate for the year 2050 and compare this with an approach based on identifying large-scale environments favourable for SCWs from a regional parent model (BARPA-R). This is done for three different types of SCW events that have been identified in this region, based on clustering of the large-scale environment. Results show that BARPAC-M representation of the extreme daily maximum wind gust distribution is improved relative to the gust distribution simulated by the regional parent model. This is due to the high spatial resolution of BARPAC-M output, as well as partly resolving strong and short-lived gusts associated with convection. However, BARPAC-M significantly overestimates the frequency of simulated SCW events, particularly in environments having steep low-level temperature lapse rates. A future decrease in SCW frequency under conditions with steep lapse rates is projected by BARPAC-M, along with less frequent favourable large-scale environments. In contrast, an increase in SCW frequency is projected under conditions of high surface moisture, with more frequent favourable large-scale environments. Therefore, overall changes in SCWs for this region remain uncertain, due to different responses between event types, combined with historical model biases. </jats:p>
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/QnJvd24sIEFuZHJldw==|https://frl.publisso.de/adhoc/uri/RG93ZHksIEFuZHJldw==|https://frl.publisso.de/adhoc/uri/TGFuZSwgVG9kZCBQLg==
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1000 Erstellt am 2024-10-03T02:43:23.854+0200
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1000 Zuletzt bearbeitet 2024-10-04T11:47:19.533+0200
1000 Objekt bearb. Fri Oct 04 11:47:19 CEST 2024
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1000 Oai Id
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