The 2018 Camp Fire: Meteorological Analysis Using In Situ Observations and Numerical Simulations

The November 2018 Camp Fire quickly became the deadliest and most destructive wildfire in California history. In this case study, we investigate the contribution of meteorological conditions and, in particular, a downslope windstorm that occurred during the 2018 Camp Fire. Dry seasonal conditions pr...

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Main Authors: Matthew J. Brewer, Craig B. Clements
Format: Article
Language:English
Published: MDPI AG 2019-12-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/1/47
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author Matthew J. Brewer
Craig B. Clements
author_facet Matthew J. Brewer
Craig B. Clements
author_sort Matthew J. Brewer
collection DOAJ
description The November 2018 Camp Fire quickly became the deadliest and most destructive wildfire in California history. In this case study, we investigate the contribution of meteorological conditions and, in particular, a downslope windstorm that occurred during the 2018 Camp Fire. Dry seasonal conditions prior to ignition led to 100-h fuel moisture contents in the region to reach record low levels. Meteorological observations were primarily made from a number of remote automatic weather stations and a mobile scanning Doppler lidar deployed to the fire on 8 November 2018. Additionally, gridded operational forecast models and high-resolution meteorological simulations were synthesized in the analysis to provide context for the meteorological observations and structure of the downslope windstorm. Results show that this event was associated with mid-level anti-cyclonic Rossby wave breaking likely caused by cold air advection aloft. An inverted surface trough over central California created a pressure gradient which likely enhanced the downslope winds. Sustained surface winds between 3&#8722;6 m s<sup>&#8722;1</sup> were observed with gusts of over 25 m s<sup>&#8722;1</sup> while winds above the surface were associated with an intermittent low-level jet. The meteorological conditions of the event were well forecasted, and the severity of the fire was not surprising given the fire danger potential for that day. However, use of surface networks alone do not provide adequate observations for understanding downslope windstorm events and their impact on fire spread. Fire management operations may benefit from the use of operational wind profilers to better understand the evolution of downslope windstorms and other fire weather phenomena that are poorly understood and observed.
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spelling doaj.art-8f84f30dadf54fc9812ad0c2209c73aa2022-12-22T03:41:19ZengMDPI AGAtmosphere2073-44332019-12-011114710.3390/atmos11010047atmos11010047The 2018 Camp Fire: Meteorological Analysis Using In Situ Observations and Numerical SimulationsMatthew J. Brewer0Craig B. Clements1Fire Weather Research Laboratory, Department of Meteorology and Climate Science, San José State University, San Jose, CA 95192, USAFire Weather Research Laboratory, Department of Meteorology and Climate Science, San José State University, San Jose, CA 95192, USAThe November 2018 Camp Fire quickly became the deadliest and most destructive wildfire in California history. In this case study, we investigate the contribution of meteorological conditions and, in particular, a downslope windstorm that occurred during the 2018 Camp Fire. Dry seasonal conditions prior to ignition led to 100-h fuel moisture contents in the region to reach record low levels. Meteorological observations were primarily made from a number of remote automatic weather stations and a mobile scanning Doppler lidar deployed to the fire on 8 November 2018. Additionally, gridded operational forecast models and high-resolution meteorological simulations were synthesized in the analysis to provide context for the meteorological observations and structure of the downslope windstorm. Results show that this event was associated with mid-level anti-cyclonic Rossby wave breaking likely caused by cold air advection aloft. An inverted surface trough over central California created a pressure gradient which likely enhanced the downslope winds. Sustained surface winds between 3&#8722;6 m s<sup>&#8722;1</sup> were observed with gusts of over 25 m s<sup>&#8722;1</sup> while winds above the surface were associated with an intermittent low-level jet. The meteorological conditions of the event were well forecasted, and the severity of the fire was not surprising given the fire danger potential for that day. However, use of surface networks alone do not provide adequate observations for understanding downslope windstorm events and their impact on fire spread. Fire management operations may benefit from the use of operational wind profilers to better understand the evolution of downslope windstorms and other fire weather phenomena that are poorly understood and observed.https://www.mdpi.com/2073-4433/11/1/47camp firefire weatherdownslope windstormwrfobservationsdoppler lidar
spellingShingle Matthew J. Brewer
Craig B. Clements
The 2018 Camp Fire: Meteorological Analysis Using In Situ Observations and Numerical Simulations
Atmosphere
camp fire
fire weather
downslope windstorm
wrf
observations
doppler lidar
title The 2018 Camp Fire: Meteorological Analysis Using In Situ Observations and Numerical Simulations
title_full The 2018 Camp Fire: Meteorological Analysis Using In Situ Observations and Numerical Simulations
title_fullStr The 2018 Camp Fire: Meteorological Analysis Using In Situ Observations and Numerical Simulations
title_full_unstemmed The 2018 Camp Fire: Meteorological Analysis Using In Situ Observations and Numerical Simulations
title_short The 2018 Camp Fire: Meteorological Analysis Using In Situ Observations and Numerical Simulations
title_sort 2018 camp fire meteorological analysis using in situ observations and numerical simulations
topic camp fire
fire weather
downslope windstorm
wrf
observations
doppler lidar
url https://www.mdpi.com/2073-4433/11/1/47
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