Estimating the lateral transfer of organic carbon through the European river network using a land surface model

Haicheng Zhang, R. Lauerwald, P. Régnier, P. Ciais, K. Van Oost, V. Naipal, B. Guenet, Wenping Yuan
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引用次数: 2

Abstract

Abstract. Lateral carbon transport from soils to the ocean through rivers has been acknowledged as a key component of global carbon cycle, but is still neglected in most global land surface models (LSMs). Fluvial transport of dissolved organic carbon (DOC) and CO2 has been implemented in the ORCHIDEE LSM, while erosion-induced delivery of sediment and particulate organic carbon (POC) from land to river was implemented in another version of the model. Based on these two developments, we take the final step towards the full representation of biospheric carbon transport through the land-river continuum. The newly developed model, called ORCHIDEE-Clateral, simulates the complete lateral transport of water, sediment, POC, DOC and CO2 from land to sea through the river network, the deposition of sediment and POC in the river channel and floodplains, and the decomposition of POC and DOC in transit. We parameterized and evaluated ORCHIDEE-Clateral using observation data in Europe. The model satisfactorily reproduces the observed riverine discharges of water and sediment, bankfull flows and sediment delivery rate from land to river, as well as the observed concentrations of organic carbon in rivers. Application of ORCHIDEE-Clateral for Europe reveals that the lateral carbon transfer affects land carbon dynamics in multiple ways and omission of this process in LSMs may result in significant biases in the simulated regional land carbon budgets. Overall, this study presents a useful tool for simulating large scale lateral carbon transfer and for predicting the feedbacks between lateral carbon transfer and future climate and land use changes.
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利用陆地表面模型估算有机碳通过欧洲河流网络的横向转移
摘要通过河流从土壤向海洋的横向碳传输已被公认为全球碳循环的关键组成部分,但在大多数全球陆地表面模型中仍然被忽视。溶解有机碳(DOC)和二氧化碳的河流输送已在ORCHDEE LSM中实施,而侵蚀诱导的沉积物和颗粒有机碳(POC)从陆地输送到河流则在该模型的另一个版本中实施。基于这两个发展,我们朝着充分代表陆地-河流连续体的生物圈碳传输迈出了最后一步。新开发的模型名为ORCHIDEE Clatrial,模拟了水、沉积物、POC、DOC和CO2通过河网从陆地到海洋的完全横向运输,沉积物和POC在河道和泛滥平原的沉积,以及POC和DOC在运输过程中的分解。我们使用欧洲的观测数据对ORCHIDEE Clatrial进行了参数化和评估。该模型令人满意地再现了观测到的河流水和沉积物的排放量、河岸流量和从陆地到河流的沉积物输送速率,以及观测到的河中有机碳浓度。ORCHIDEE Clatrial for Europe的应用表明,横向碳转移以多种方式影响土地碳动态,LSM中省略这一过程可能会导致模拟的区域土地碳预算存在重大偏差。总的来说,这项研究为模拟大规模横向碳转移以及预测横向碳转移与未来气候和土地利用变化之间的反馈提供了一个有用的工具。
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