Wind and Structures

  • 제24권6호
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  • Pages.529-564
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  • 2017
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  • 1226-6116(pISSN)
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  • 1598-6225(eISSN)
테크노프레스 (Techno-Press)
권호 표지
DOI QR코드

DOI QR Code

The Santa Ana winds of Southern California: Winds, gusts, and the 2007 Witch fire

  • Fovell, Robert G. (Department of Atmospheric and Environmental Sciences, University at Albany, State University of New York) ;
  • Cao, Yang (Department of Hydrology and Atmospheric Sciences, The University of Arizona)
  • 투고 : 2016.01.08
  • 심사 : 2016.03.10
  • 발행 : 2017.06.25
⟨ 이전 논문 다음 논문 ⟩

초록

The Santa Ana winds occur in Southern California during the September-May time frame, bringing low humidities across the area and strong winds at favored locations, which include some mountain gaps and on particular slopes. The exceptionally strong event of late October 2007, which sparked and/or spread numerous fires across the region, is compared to more recent events using a numerical model verified against a very dense, limited-area network (mesonet) that has been recently deployed in San Diego County. The focus is placed on the spatial and temporal structure of the winds within the lowest two kilometers above the ground within the mesonet, along with an attempt to gauge winds and gusts occurring during and after the onset of October 2007's Witch fire, which became one of the largest wildfires in California history.

키워드

과제정보

연구 과제 주관 기관 : San Diego Gas and Electric Company

참고문헌

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피인용 문헌

  1. Winds and Gusts during the Thomas Fire vol.1, pp.3, 2018, https://doi.org/10.3390/fire1030047
  2. Characteristics of Sundowner Winds Near Santa Barbara, CA, From a Dynamically Downscaled Climatology: Environment and Effects Aloft and Offshore vol.123, pp.23, 2017, https://doi.org/10.1029/2018jd029065
  3. Regions of influence and environmental effects of Santa Ana wind event vol.12, pp.9, 2017, https://doi.org/10.1007/s11869-019-00719-3
  4. Evaluating the Ability of FARSITE to Simulate Wildfires Influenced by Extreme, Downslope Winds in Santa Barbara, California vol.3, pp.3, 2017, https://doi.org/10.3390/fire3030029