Wildfire Pyroconvection and CAPE: Buoyancy’s Drying and Atmospheric Intensification—Fort McMurray

The accurate prediction of wildfire behavior and spread is possible only when fire and atmosphere simulations are coupled. In this work, we present a mechanism that causes a small fire to intensify by altering the atmosphere. These alterations are caused by fire-related fluxes at the surface. The fi...

Full description

Bibliographic Details
Published in:Atmosphere
Main Authors: Atoossa Bakhshaii, Edward A. Johnson, Kiana Nayebi
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/atmos11070763
id ftmdpi:oai:mdpi.com:/2073-4433/11/7/763/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2073-4433/11/7/763/ 2023-08-20T04:06:35+02:00 Wildfire Pyroconvection and CAPE: Buoyancy’s Drying and Atmospheric Intensification—Fort McMurray Atoossa Bakhshaii Edward A. Johnson Kiana Nayebi agris 2020-07-18 application/pdf https://doi.org/10.3390/atmos11070763 EN eng Multidisciplinary Digital Publishing Institute Meteorology https://dx.doi.org/10.3390/atmos11070763 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 11; Issue 7; Pages: 763 wildfire pyroconvection weather Skew-T Text 2020 ftmdpi https://doi.org/10.3390/atmos11070763 2023-07-31T23:47:40Z The accurate prediction of wildfire behavior and spread is possible only when fire and atmosphere simulations are coupled. In this work, we present a mechanism that causes a small fire to intensify by altering the atmosphere. These alterations are caused by fire-related fluxes at the surface. The fire plume and fluxes increase the convective available potential energy (CAPE) and the chance of the development of a strong pyroconvection system. To study this possible mechanism, we used WRF-Fire to capture fire line propagation as the result of interactions between heat and moisture fluxes, pressure perturbations, wind shear development and dry air downdraft. The wind patterns and dynamics of the pyroconvection system are simulated for the Horse River wildfire at Fort McMurray, Canada. The results revealed that the updraft speed reached up to 12 m/s. The entrainment mixed the mid and upper-level dry air and lowered the atmospheric moisture. The mid-level and upper-level dew point temperature changed by 5–10 ∘ C in a short period of time. The buoyant air strengthened the ascent as soon as the nocturnal inversion was eliminated by daytime heating. The 887 J/kg total increase of CAPE in less than 5 h and the high bulk Richardson number (BRN) of 93 were indicators of the growing pyro-cumulus cell. The presented simulation has not improved the original model or supported leading-edge numerical weather prediction (NWP) achievements, except for adapting WRF-Fire for Canadian biomass fuel. However, we were able to present a great deal of improvements in wildfire nowcasting and short-term forecasting to save lives and costs associated with wildfires. The simulation is sufficiently fast and efficient to be considered for a real-time operational model. While the project was designed and succeeded as an NWP application, we are still searching for a solution for the intractable problems associated with political borders and the current liable authorities for the further development of a new generation of national ... Text Fort McMurray MDPI Open Access Publishing Canada Fort McMurray Horse River ENVELOPE(-111.385,-111.385,56.717,56.717) Atmosphere 11 7 763
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic wildfire
pyroconvection
weather
Skew-T
spellingShingle wildfire
pyroconvection
weather
Skew-T
Atoossa Bakhshaii
Edward A. Johnson
Kiana Nayebi
Wildfire Pyroconvection and CAPE: Buoyancy’s Drying and Atmospheric Intensification—Fort McMurray
topic_facet wildfire
pyroconvection
weather
Skew-T
description The accurate prediction of wildfire behavior and spread is possible only when fire and atmosphere simulations are coupled. In this work, we present a mechanism that causes a small fire to intensify by altering the atmosphere. These alterations are caused by fire-related fluxes at the surface. The fire plume and fluxes increase the convective available potential energy (CAPE) and the chance of the development of a strong pyroconvection system. To study this possible mechanism, we used WRF-Fire to capture fire line propagation as the result of interactions between heat and moisture fluxes, pressure perturbations, wind shear development and dry air downdraft. The wind patterns and dynamics of the pyroconvection system are simulated for the Horse River wildfire at Fort McMurray, Canada. The results revealed that the updraft speed reached up to 12 m/s. The entrainment mixed the mid and upper-level dry air and lowered the atmospheric moisture. The mid-level and upper-level dew point temperature changed by 5–10 ∘ C in a short period of time. The buoyant air strengthened the ascent as soon as the nocturnal inversion was eliminated by daytime heating. The 887 J/kg total increase of CAPE in less than 5 h and the high bulk Richardson number (BRN) of 93 were indicators of the growing pyro-cumulus cell. The presented simulation has not improved the original model or supported leading-edge numerical weather prediction (NWP) achievements, except for adapting WRF-Fire for Canadian biomass fuel. However, we were able to present a great deal of improvements in wildfire nowcasting and short-term forecasting to save lives and costs associated with wildfires. The simulation is sufficiently fast and efficient to be considered for a real-time operational model. While the project was designed and succeeded as an NWP application, we are still searching for a solution for the intractable problems associated with political borders and the current liable authorities for the further development of a new generation of national ...
format Text
author Atoossa Bakhshaii
Edward A. Johnson
Kiana Nayebi
author_facet Atoossa Bakhshaii
Edward A. Johnson
Kiana Nayebi
author_sort Atoossa Bakhshaii
title Wildfire Pyroconvection and CAPE: Buoyancy’s Drying and Atmospheric Intensification—Fort McMurray
title_short Wildfire Pyroconvection and CAPE: Buoyancy’s Drying and Atmospheric Intensification—Fort McMurray
title_full Wildfire Pyroconvection and CAPE: Buoyancy’s Drying and Atmospheric Intensification—Fort McMurray
title_fullStr Wildfire Pyroconvection and CAPE: Buoyancy’s Drying and Atmospheric Intensification—Fort McMurray
title_full_unstemmed Wildfire Pyroconvection and CAPE: Buoyancy’s Drying and Atmospheric Intensification—Fort McMurray
title_sort wildfire pyroconvection and cape: buoyancy’s drying and atmospheric intensification—fort mcmurray
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/atmos11070763
op_coverage agris
long_lat ENVELOPE(-111.385,-111.385,56.717,56.717)
geographic Canada
Fort McMurray
Horse River
geographic_facet Canada
Fort McMurray
Horse River
genre Fort McMurray
genre_facet Fort McMurray
op_source Atmosphere; Volume 11; Issue 7; Pages: 763
op_relation Meteorology
https://dx.doi.org/10.3390/atmos11070763
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos11070763
container_title Atmosphere
container_volume 11
container_issue 7
container_start_page 763
_version_ 1774717793207320576