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Washburn Post-Fire BAER

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Yosemite National Park
National Park Service
P.O. Box 577
Yosemite National Park, CA 95389

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Phone: 707-853-4243
Hours: 8am-8pm

Washburn Post-Fire Soil Burn Severity Map Released

Washburn Post-Fire BAER Burned Area Emergency Response
News – 7/29/2022



Interagency BAER team specialists completed its field data gathering on National Park Service and Sierra National Forest lands burned by the Washburn Fire on July 24, 2022. The team’s post-fire soil burn severity (SBS) map analyzes 4,835 acres of the South Fork Merced River Watershed. The map and the data display soil burn severity (SBS) categories of unburned/very low, low, moderate, and high.

Approximately 47% of the total acres are either unburned/very low or low SBS, while 48% are moderate SBS and only 5% are high SBS.

The BAER team’s assessment shows the acreage for land ownership for the 4,835 acres to be:

  • 1,957 acres for the Sierra National Forest (NF), and
  • 2,878 acres for Yosemite National Park land.

The BAER assessment team used preliminary remote sensing data based on satellite imagery of the fire perimeter from July 21, 2022, with field-validated data collected over several days to produce the final Washburn Post-Fire SBS map. Since that date, the fire has grown to 4,883 acres as of July 28, 2022.

The BAER assessment team coordinates with other local and federal agencies such as county and state officials, Natural Resources Conservation Service (NRCS), National Weather Service (NWS), and USGS to share information about burned watershed conditions and their predicted response during certain rain events.

The SBS map product is an estimate of fire effects on soils and not a measure of direct effects to vegetation. SBS characterizes the soil surface and below-ground impact, whereas effects on vegetation are estimates of mortality based primarily on changes in vegetation canopy. The Rapid Assessment of Vegetation Condition after Wildfire (RAVG) program produces data describing post-fire vegetation conditions on federal lands. Changes in overhead and understory vegetation canopy are often used as initial indicators of overall burn severity, but do not necessarily coincide with SBS.

Changes in soil cover, water repellency, and soil physical/biological conditions guide the interpretations to determine the severity burn level of the soil. Water repellency can occur naturally in soil and may change as a function of fire. Fire can increase the strength and thickness (or depth) of water-repellent layers in soil, considerably affecting post-fire water runoff and possibly extending time for recovery of the burned area.

Soil burn severity indicators can be found within the Rocky Mountain Research Station’s General Technical Report 243 – Field Guide for Mapping Post-Fire Soil Burn Severity and are described below.

Low SBS generally occurs where surface organic layers are not completely consumed and are still recognizable. Structural aggregate stability is not changed from its unburned condition, and roots are generally unchanged because the heat pulse below the soil surface was not great enough to consume or char any underlying organics. The ground surface, including any exposed mineral soil, may appear brown or black (lightly charred), and the canopy and understory vegetation will likely appear “green.” Lower risk for accelerated runoff, erosion, flooding and debris flows is expected within and below these areas compared to moderate and high SBS.

In areas with moderate SBS, up to 80% of the pre-fire ground cover (litter and ground fuels) is consumed. Fine roots may be scorched but are rarely completely consumed over much of the area. The color of the ash on the surface is generally blackened with possible gray patches. There may be potential for recruitment of effective ground cover from scorched needles or leaves remaining in the canopy that will soon fall to the ground. The prevailing color of the site is often “brown” due to canopy needle and other vegetation scorch. Soil structure is generally unchanged. Where greater amounts of reduced soil cover and increased water repellency occur, increased overland flow of water from precipitation is expected, most notably in locations where the overstory canopy no longer exists.

High SBS occurs where all or nearly all the pre-fire ground cover and surface organic matter (litter, duff, and fine roots) are consumed, and charring may be visible on larger roots. The prevailing color of the site is often “black” due to extensive charring. Bare soil or ash is exposed and susceptible to erosion, and aggregate structure may be less stable. White or gray ash (up to several centimeters in depth) indicates that considerable ground cover or fuels were consumed. Sometimes very large tree roots are entirely burned extending from a charred stump hole. Soil is often gray, orange, or reddish at the ground surface where large fuels were concentrated and consumed.

Generally, there is 100% tree mortality in high SBS, and tree recovery will take many years without planting. In high SBS, the exposed bare soil is very prone to post-fire impacts. Rain events on damaged soil can cause excessive soil erosion, resulting in higher volumes of sediment delivery to adjacent creeks and rivers. There is increased likelihood for flooding and debris flows. These threats can individually or cumulatively increase the risk to human life and safety, property, infrastructure, and important critical natural and cultural resources.

The BAER team will use the Washburn SBS data to analyze and model post-fire hydrologic response for each of the watershed to determine if there are any threats or risks to BAER critical values. The team shares its analysis with cooperating agencies who have the authority to work with private property owners downstream from the burned area that potentially may have post-fire threats from increased water and debris flows. The BAER team’s assessment and findings will be documented in two reports, one for the Yosemite National Park and one for the Sierra National Forest that will be posted to the Washburn Post-Fire BAER InciWeb page after both reports have been reviewed and approved by leadership of both agencies.

The Washburn Fire SBS map can be downloaded at the “Washburn Post-Fire BAER” InciWeb site ( as a JPEG or PDF version under the “Maps” tab.

For addition information about understanding SBS, see: Post-Fire Effects Understanding Soil Burn Severity - InciWeb the Incident Information System (

BAER SAFETY MESSAGEEveryone near and downstream from the burned areas should remain alert and stay updated on weather conditions that may result in heavy rains and increased water runoff. Flash flooding may occur quickly during heavy rain events – be prepared to act. Current weather and emergency notifications can be found at the National Weather Service websites: and

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