First Advisor

Kelly Gleason

Term of Graduation

Fall 2024

Date of Publication

12-12-2024

Document Type

Thesis

Degree Name

Master of Science (M.S.) in Environmental Science and Management

Department

Environmental Science and Management

Language

English

Subjects

Black Carbon, Burn Severity, Forest Fire Impacts on Hydrology, Postfire Snowpack Dynamics, Radiative Forcing, Snow Albedo Recovery

Physical Description

1 online resource (ix, 67 pages)

Abstract

Burned forests that remain standing following fire release light-absorbing particles (LAPs), including black carbon (BC), into winter snowpacks, reducing snow surface albedo and accelerating snowmelt timing for decades postfire. Although the role of LAPs in seasonal snow has been extensively studied, the spatiotemporal variability of LAPs' contributions to snowmelt relative to time-since-fire and burn severity remains unknown. This study aimed to quantify the spatiotemporal variability of forest fire effects on LAPs in snow and associated snow albedo in the Triple Divide region of western Wyoming, headwaters of the Colorado, Columbia, and Missouri rivers. Using geochemical analysis and radiative transfer modeling, we measured BC concentrations across a chronosequence of eight burned forests, examining how fire age and burn severity impact snowpack albedo. We hypothesized that radiative forcing due to BC in snow would be highest immediately after fire in high-severity burned forests and that snow albedo in burned areas would gradually recover to resemble open meadow conditions over decades. Our results confirmed that BC concentrations were highest in high-severity burned forests, peaking at 154.5 ppb in surface snow and remaining elevated for up to 20 years postfire. Elevated BC concentrations also extended beyond burned perimeters into adjacent unburned forests and open meadows. Seasonal analysis showed that near-surface samples in February had the highest mean BC concentration, reaching 78.4 ppb. Radiative forcing values were greatest in high-severity burned forests, peaking at 54.2 W/m², which indicates significant energy absorption and likely accelerated snowmelt in these regions.

Rights

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Persistent Identifier

https://archives.pdx.edu/ds/psu/43007

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