• Factors including extreme winds, topogra

    From ScienceDaily@1:317/3 to All on Thu Apr 14 22:30:44 2022
    Factors including extreme winds, topography and vegetation influenced
    the severity of burns from Oregon's devastating 2020 megafires

    Date:
    April 14, 2022
    Source:
    Portland State University
    Summary:
    In a new study examining burn patterns from the 2020 Labor Day
    fires, researchers studied the influence of weather, topography,
    vegetation and other factors on burn severity in areas where the
    fires killed more than 75% of the trees. Their research confirms
    that extreme winds over the Labor Day holiday were the primary
    driver of the destructive force of the fires yet demonstrates
    how forest vegetation structure (e.g., canopy height, the age
    of trees, etc.) and topography played a significant role in burn
    severity patterns.



    FULL STORY ==========================================================================
    In early September 2020, severe winds, high heat, and prolonged drought conditions led to the explosive growth of wildfires along the western
    slopes of the Cascades Mountains in the Pacific Northwest. The fires
    engulfed enormous tracts of forestland, destroyed communities, took
    dozen of lives, and cost hundreds of millions to fight.


    ==========================================================================
    In a first-of-its-kind study examining burn patterns from the 2020 Labor
    Day fires, researchers at Portland State University studied the influence
    of weather, topography, vegetation and other factors on burn severity in
    areas where the fires killed more than 75% of the trees. Their research confirms that extreme winds over the Labor Day holiday were the primary
    driver of the destructive force of the fires yet demonstrates how forest vegetation structure (e.g., canopy height, the age of trees, etc.) and topography played a significant role in burn severity patterns.

    The paper, "Extreme Winds Alter Influence of Fuels and Topography on
    Megafire Burn Severity in Seasonal Temperate Rainforests under Record
    Fuel Aridity," was recently published in the journal Fire.

    According to the study's co-author, Andre's Holz, associate professor of geography at Portland State, the wet temperate forests of the Cascade
    Mountains in the Pacific Northwest have a history of experiencing
    megafires of the scale of those that burned in 2020, but none had occurred since the early twentieth century. Because the scope and scale of the
    burns were unprecedented in modern times, they provided the research team
    a unique opportunity to gain a better understanding of the factors that influence the high severity of burns in these rainforests, including
    those on the western slopes of the Cascades. That understanding can
    inform planning for future land-use management in forestlands and the
    social and ecological impacts of extreme fire events in the context of
    a warming planet.

    The research team developed maps for the extent and burn severity for five megafires and examined fire activity over two time periods: September 7-9, 2020, during which extreme winds fueled the explosive growth of the fires,
    and September 10-17, 2020, during which the fires continued burning under
    calm wind conditions. They then examined how the forest structure and topography influenced high-burn severity patterns, whether winds affected
    the relationship between those factors, and how high burn severity was
    affected by land management practices associated with land ownership.

    "90% of the burning occurred during high winds," said Dr. Cody Every,
    a Research Associate in the Department of Environmental Science and
    Management at Portland State and the study's lead author. "But we also
    found that vegetation structure and canopy height were significant in determining where the fire burned more severely." The research team
    found that areas with younger trees and low canopy height and cover were particularly susceptible to high mortality rates. As Holz pointed out,
    this finding is of particular consequence to lumber production in the
    state, where trees grown on plantations are typically younger, uniformly
    spaced and located near communities and critical infrastructure.

    Drawing on the historical record, the team, which included Portland
    State researchers Dr. Sebastian Busby and Associate Professor Max Nielsen-Pincus, also suggests that wildfire managers should anticipate
    re-burns in some areas affected by the 2020 megafires. Recently burned
    forests typically have higher flammability than unburned areas until
    the younger forest canopy closes again and finer fuels are shaded.

    Given the composition of the temperate rainforests of the western slopes
    of the Cascade Mountains, where fuel proliferates, and the relationships between factors that contribute to megafires, the research team suggests
    that treatments such as prescribed fires and fuel reduction are not
    a practical approach to preventing future conflagrations. Instead,
    the team argues that we should focus on promoting resilient forests,
    increasing community preparedness, early suppression response, and
    hardening infrastructure.


    ========================================================================== Story Source: Materials provided by Portland_State_University. Original
    written by Shaun McGillis. Note: Content may be edited for style and
    length.


    ========================================================================== Journal Reference:
    1. Cody Evers, Andre's Holz, Sebastian Busby, Max
    Nielsen-Pincus. Extreme
    Winds Alter Influence of Fuels and Topography on Megafire Burn
    Severity in Seasonal Temperate Rainforests under Record Fuel
    Aridity. Fire, 2022; 5 (2): 41 DOI: 10.3390/fire5020041 ==========================================================================

    Link to news story: https://www.sciencedaily.com/releases/2022/04/220414125031.htm

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