Quantifying the Impacts of Fire-Related Perturbations in WRF-Hydro Terrestrial Water Budget Simulations in California's Feather River Basin

IF 3.2 3区 地球科学 Q1 Environmental Science Hydrological Processes Pub Date : 2024-11-10 DOI:10.1002/hyp.15314
Ronnie Abolafia-Rosenzweig, David Gochis, Andrew Schwarz, Thomas H. Painter, Jeffery Deems, Aubrey Dugger, Matthew Casali, Cenlin He
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Abstract

Wildfire activity in the western United States (WUS) is increasingly impacting water supply, and land surface models (LSMs) that do not explicitly account for fire disturbances can have critical uncertainties in burned areas. This study quantified responses from the Weather Research and Forecasting Hydrological modelling system (WRF-Hydro) to a suite of fire-related perturbations to hydrologic soil and runoff parameters, vegetation area, land cover classifications and associated vegetation properties, and snow albedo across the heavily burned Feather River Basin in California. These experiments were used to quantify the impacts of fire-related perturbations in model simulations under the observed meteorological conditions during the 2000–2022 water years and determine whether applying these fire-related perturbations enhanced post-fire model accuracy across the 11–12 post-fire months evaluated herein. The most comprehensive fire-aware simulation consistently modelled enhanced annual catchment streamflow (by 8%–37%), subsurface flow (by 72%–116%), and soil moisture (by 4%–9%), relative to the baseline simulation which neglected fire impacts. Simulated fire-enhanced streamflow was predominately attributable to fire-induced vegetation area reductions that reduced transpiration. Simulated streamflow enhancements occurred throughout the water year, excluding early-summer (e.g., May–June) when the baseline simulation modelled relatively more snowmelt and streamflow because fire perturbations caused earlier model snow depletion. Vegetation area reductions favoured increased model ground snow accumulation and enhanced snow ablation while imposed snow albedo darkening enhanced ablation, ultimately resulting in similar peak SWE and earlier snow disappearance (on average by 8-days) from the most comprehensive fire-aware simulation relative to the baseline simulation. The baseline simulation had large degradations in streamflow accuracy following major fire events that were likely partially attributable to neglecting fire disturbances. Applying fire-related perturbations reduced post-fire streamflow anomaly biases across the three study catchments. However, remaining large post-fire streamflow uncertainties in the fire-perturbed simulation underscores the importance of additional observationally constrained fire-disturbance model developments.

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量化加利福尼亚费瑟河流域 WRF-Hydro 陆地水预算模拟中与火灾有关的扰动的影响
美国西部(WUS)的野火活动对供水的影响与日俱增,而没有明确考虑火灾干扰的地表模型(LSM)可能会在烧毁地区产生严重的不确定性。本研究量化了天气研究与预报水文模拟系统(WRF-Hydro)对加利福尼亚州被严重烧毁的费瑟河流域的水文土壤和径流参数、植被面积、土地覆被分类和相关植被特性以及积雪反照率等一系列火灾相关扰动的响应。这些实验用于量化在 2000-2022 水年期间观测到的气象条件下,与火灾相关的扰动对模型模拟的影响,并确定应用这些与火灾相关的扰动是否能在本文评估的火灾后 11-12 个月内提高火灾后模型的准确性。与忽略火灾影响的基线模拟相比,最全面的火灾感知模拟始终模拟出增强的年度集水区溪流(8%-37%)、地下水流(72%-116%)和土壤湿度(4%-9%)。模拟火灾增加的溪流主要归因于火灾引起的植被面积减少,从而降低了蒸腾作用。模拟的溪流增大发生在整个水年,但不包括初夏(如 5-6 月),此时基线模拟模拟的融雪和溪流相对较多,因为火灾扰动导致模型积雪消耗较早。植被面积的减少有利于增加模型的地面积雪并增强积雪消融,而施加的积雪反照率变暗则增强了消融,最终导致最全面的火灾感知模拟与基线模拟相比,具有相似的峰值 SWE 和更早的积雪消失(平均 8 天)。基线模拟在发生重大火灾事件后,流体流量的准确性大幅下降,部分原因可能是忽略了火灾扰动。应用与火灾相关的扰动可减少三个研究流域火灾后的溪流异常偏差。然而,在火灾扰动模拟中,火灾后的溪流仍存在较大的不确定性,这凸显了开发更多观测约束的火灾扰动模型的重要性。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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