Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California, USA.
Climate Change Science Institute, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA.
Glob Chang Biol. 2023 Aug;29(15):4298-4312. doi: 10.1111/gcb.16755. Epub 2023 May 15.
The recent rise in atmospheric methane (CH ) concentrations accelerates climate change and offsets mitigation efforts. Although wetlands are the largest natural CH source, estimates of global wetland CH emissions vary widely among approaches taken by bottom-up (BU) process-based biogeochemical models and top-down (TD) atmospheric inversion methods. Here, we integrate in situ measurements, multi-model ensembles, and a machine learning upscaling product into the International Land Model Benchmarking system to examine the relationship between wetland CH emission estimates and model performance. We find that using better-performing models identified by observational constraints reduces the spread of wetland CH emission estimates by 62% and 39% for BU- and TD-based approaches, respectively. However, global BU and TD CH emission estimate discrepancies increased by about 15% (from 31 to 36 TgCH year ) when the top 20% models were used, although we consider this result moderately uncertain given the unevenly distributed global observations. Our analyses demonstrate that model performance ranking is subject to benchmark selection due to large inter-site variability, highlighting the importance of expanding coverage of benchmark sites to diverse environmental conditions. We encourage future development of wetland CH models to move beyond static benchmarking and focus on evaluating site-specific and ecosystem-specific variabilities inferred from observations.
大气甲烷 (CH ) 浓度的最近升高加速了气候变化,并抵消了缓解努力。尽管湿地是最大的自然 CH 源,但自下而上 (BU) 基于过程的生物地球化学模型和自上而下 (TD) 大气反演方法所采用的方法之间,全球湿地 CH 排放估计值差异很大。在这里,我们将现场测量、多模型集合和机器学习扩展产品整合到国际土地模型基准系统中,以研究湿地 CH 排放估计值与模型性能之间的关系。我们发现,通过观测约束识别出表现更好的模型,可以将 BU 和 TD 方法的湿地 CH 排放估计值的差异分别缩小 62%和 39%。然而,当使用前 20%的模型时,全球 BU 和 TD CH 排放估计差异增加了约 15%(从 31 到 36TgCH 年),尽管考虑到全球观测分布不均,我们认为这一结果存在中度不确定性。我们的分析表明,由于站点间的巨大变异性,模型性能排名受到基准选择的影响,这突出了扩大基准站点覆盖范围以适应不同环境条件的重要性。我们鼓励未来开发湿地 CH 模型,超越静态基准测试,专注于评估从观测中推断出的特定地点和特定生态系统的可变性。