ELM‐Wet: Inclusion of a Wet‐Landunit With Sub‐Grid Representation of Eco‐Hydrological Patches and Hydrological Forcing Improves Methane Emission Estimations in the E3SM Land Model (ELM)

环境科学 湿地 强迫(数学) 焊剂(冶金) 涡度相关法 甲烷 水文学(农业) 大气科学 生态系统 地质学 生态学 化学 生物 有机化学 岩土工程
作者
Theresia Yazbeck,Gil Bohrer,Madeline E. Scyphers,Justine Missik,Oleksandr Shchehlov,Eric J. Ward,Sergio Merino,Robert Bordelon,Diana Taj,Jorge A. Villa,Kelly Wrighton,Qing Zhu,W. J. Riley
出处
期刊:Journal of Advances in Modeling Earth Systems [Wiley]
卷期号:17 (2) 被引量:1
标识
DOI:10.1029/2024ms004396
摘要

Abstract Wetlands are the largest emitters of biogenic methane (CH 4 ) and represent the highest source of uncertainty in global CH 4 budgets. Here, we aim to improve the realism of wetland representation in the U.S. Department of Energy's Exascale Earth System Model land surface model, ELM, thereby reducing uncertainty of CH 4 flux predictions. We develop an updated version, ELM‐Wet, where we activate a separate landunit for wetlands that handles multiple wetland‐specific eco‐hydrological patch functional types. We introduce more realistic hydrological forcing through prescribing site‐level constraints on surface water elevation, which allows resolving different sustained inundation depth for different patches, and if data exists, prescribing inundation depth. We modified the calculation of aerenchyma transport diffusivity based on observed conductance per leaf area for different vegetation types. We use Bayesian Optimization to parameterize CO 2 and CH 4 fluxes in the developed wet‐landunit. Site‐level simulations of a coastal non‐tidal freshwater wetland in Louisiana were performed with the updated model. Eddy covariance observations of CO 2 and CH 4 fluxes from 2012 to 2013 were used to train the model and data from 2021 were used for validation. Patch‐specific chamber flux observations and observations of CH 4 concentration profiles in the soil porewater from 2021 were used for evaluation of the model performance. Our results show that ELM‐Wet reduces the model's CH 4 emission root mean squared error by up to 33% and is able to represent inter‐daily CO 2 and CH 4 flux variability across the wetland's eco‐hydrological patches, including during periods of extreme dry or wet conditions.
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