ESD评论:地球系统模型中陆地和海洋生态系统表现之间多重不一致的证据

F. Pellerin, P. Porada, I. Hense
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摘要

摘要陆地和海洋生态系统通过不同的生物圈-气候反馈与地球系统的其他组成部分相互作用,这些反馈在生态系统类型之间非常相似。尽管有这些相似之处,在地球系统模型(ESM)中,陆地系统和海洋系统往往相对分开处理。在这些ESM中,生态系统由一系列生物过程代表,这些生物过程能够通过影响环境的化学和物理性质来影响气候系统。虽然大多数与气候有关的过程在生态系统类型之间是共享的,但陆地和海洋生态系统的模式表示往往不同。这就提出了一个问题,即陆地和海洋生态系统模型之间是否存在不一致,并可能扭曲我们对每种生态系统对气候的相对影响的认识。本文比较了17个地球系统模型的陆地和海洋模块,以确定两种生态系统类型之间的不一致性。我们将ESM中包含的生物过程对气候的影响整理为生物圈-气候反馈的三种类型(即生物地球化学泵、生物地球物理机制和气体和粒子穿梭),并批判性地比较了它们在不同生态系统模块中的表现。总体而言,我们发现了ESM中陆地和海洋生态系统模型在过程表征方面存在不合理差异的多个证据。这些不一致可能导致对生物圈在气候系统中的作用的错误预测。我们认为,目前的比较可以被地球系统模拟界用来增加生态系统模型之间的一致性。我们进一步呼吁制定一个共同框架,以便在ESM的生态系统模块中统一表示与气候相关的过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ESD Reviews: Evidence of multiple inconsistencies between representations of terrestrial and marine ecosystems in Earth System Models
Abstract. Terrestrial and marine ecosystems interact with other Earth system components through different biosphere-climate feedbacks that are very similar among ecosystem types. Despite these similarities, terrestrial and marine systems are often treated relatively separately in Earth System Models (ESM). In these ESM, the ecosystems are represented by a set of biological processes that are able to influence the climate system by affecting the chemical and physical properties of the environment. While most of the climate-relevant processes are shared between ecosystem types, model representations of terrestrial and marine ecosystems often differ. This raises the question whether inconsistencies between terrestrial and marine ecosystem models exist and potentially skew our perception of the relative influence of each ecosystem on climate. Here we compared the terrestrial and marine modules of 17 Earth System Models in order to identify inconsistencies between the two ecosystem types. We sorted out the biological processes included in ESM regarding their influence on climate into three types of biosphere-climate feedbacks (i.e. the biogeochemical pumps, the biogeophysical mechanisms and the gas and particle shuttles), and critically compare their representation in the different ecosystem modules. Overall, we found multiple evidences of unjustified differences in process representations between terrestrial and marine ecosystem models within ESM. These inconsistencies may lead to wrong predictions about the role of biosphere in the climate system. We believe that the present comparison can be used by the Earth system modeling community to increase consistency between ecosystem models. We further call for the development of a common framework allowing the uniform representation of climate-relevant processes in ecosystem modules of ESM.
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