Theresia Yazbeck, Gil Bohrer, Madeline E. Scyphers, Justine E. C. Missik, Oleksandr Shchehlov, Eric J. Ward, Sergio L. Merino, Robert Bordelon, Diana Taj, Jorge A. Villa, Kelly Wrighton, Qing Zhu, William J. Riley
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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<sub>2</sub> and CH<sub>4</sub> 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<sub>2</sub> and CH<sub>4</sub> 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<sub>4</sub> concentration profiles in the soil porewater from 2021 were used for evaluation of the model performance. 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引用次数: 0
摘要
湿地是生物甲烷(CH4)的最大排放源,也是全球CH4预算的最大不确定性来源。本研究旨在提高美国能源部百亿亿次地球系统模型(eascale Earth System Model)地表模型(ELM)中湿地表征的真实性,从而降低CH4通量预测的不确定性。我们开发了一个更新版本,ELM-Wet,其中我们为湿地激活一个单独的土地单元,处理多个湿地特定的生态水文斑块功能类型。我们通过规定地表水海拔的场地水平约束来引入更现实的水文强迫,这允许解决不同斑块的不同持续淹没深度,如果有数据,则规定淹没深度。在不同植被类型下,基于观测到的每叶面积电导修正了空气组织输运扩散系数的计算方法。利用贝叶斯优化方法对发达湿陆单元的CO2和CH4通量进行参数化。利用更新后的模型对路易斯安那州沿海非潮汐淡水湿地进行了场地水平模拟。利用2012 - 2013年的CO2和CH4通量涡动相关观测数据对模型进行训练,并利用2021年的数据对模型进行验证。利用2021年土壤孔隙水CH4浓度剖面和不同区域的室内通量观测值对模型的性能进行了评价。我们的研究结果表明,ELM-Wet将模型的CH4排放均方根误差降低了33%,并且能够代表湿地生态水文斑块的CO2和CH4通量的日际变化,包括在极端干燥或潮湿的条件下。
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)
Wetlands are the largest emitters of biogenic methane (CH4) and represent the highest source of uncertainty in global CH4 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 CH4 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 CO2 and CH4 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 CO2 and CH4 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 CH4 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 CH4 emission root mean squared error by up to 33% and is able to represent inter-daily CO2 and CH4 flux variability across the wetland's eco-hydrological patches, including during periods of extreme dry or wet conditions.
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