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Representation of dissolved organic carbon in the JULES land surface model (vn4.4_JULES-DOCM)

机译:JULES陆地表面模型(vn4.4_JULES-DOCM)中溶解有机碳的表示

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Current global models of the carbon (C) cycle consider only vertical gas exchanges between terrestrial or oceanic reservoirs and the atmosphere, thus not considering the lateral transport of carbon from the continents to the oceans. Therefore, those models implicitly consider all of the C which is not respired to the atmosphere to be stored on land and hence overestimate the land C sink capability. A model that represents the whole continuum from atmosphere to land and into the ocean would provide a better understanding of the Earth's C cycle and hence more reliable historical or future projections. A first and critical step in that direction is to include processes representing the production and export of dissolved organic carbon in soils. Here we present an original representation of dissolved organic C (DOC) processes in the Joint UK Land Environment Simulator (JULES-DOCM) that integrates a representation of DOC production in terrestrial ecosystems based on the incomplete decomposition of organic matter, DOC decomposition within the soil column, and DOC export to the river network via leaching. The model performance is evaluated in five specific sites for which observations of soil DOC concentration are available. Results show that the model is able to reproduce the DOC concentration and controlling processes, including leaching to the riverine system, which is fundamental for integrating terrestrial and aquatic ecosystems. Future work should include the fate of exported DOC in the river system as well as DIC and POC export from soil.
机译:当前的全球碳(C)循环模型仅考虑陆地或海洋储层与大气之间的垂直气体交换,因此未考虑碳从各大洲向海洋的横向传输。因此,这些模型隐含地将所有未被呼吸到大气中的碳储存在陆地上,从而高估了土地C的下沉能力。代表从大气到陆地再到海洋的整个连续体的模型将提供对地球C循环的更好理解,从而提供更可靠的历史或未来预测。朝这个方向迈出的第一步也是至关重要的一步,那就是包括代表土壤中溶解有机碳的生产和输出的过程。在这里,我们介绍了联合英国土地环境模拟器(JULES-DOCM)中溶解有机C(DOC)过程的原始表示,该过程基于有机物的不完全分解,土壤中的DOC分解,整合了陆地生态系统中DOC生产的表示形式柱,DOC通过浸出导出到河网。在可获得土壤DOC浓度观测值的五个特定地点对模型性能进行了评估。结果表明,该模型能够再现DOC浓度和控制过程,包括淋溶到河流系统,这对于整合陆生和水生生态系统至关重要。未来的工作应包括河流系统中DOC的出口以及土壤DIC和POC的出口。

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