Three-Dimensional Hindcast of Nitrogen and Phosphorus Biogeochemical Dynamics in Lake Onego Ecosystem, 1985–2015. Part I: Long-Term Dynamics and Spatial Distribution

A. Isaev, O. Savchuk, N. Filatov
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引用次数: 1

Abstract

Despite a wide-ranging research, there is almost no information regarding the major biogeochemical fluxes that could characterize the past and present state of the European Lake Onego ecosystem and be used for reliable prognostic estimates of its future. To enable such capacity, we adapted and implemented a three-dimensional coupled hydrodynamical biogeochemical model of the nutrient cycles in Lake Onego. The model was used to reconstruct three decades of Lake Onego ecosystem dynamics with daily resolution on a 2 × 2 km grid. A comparison with available information from Lake Onego and other large boreal lakes proves that this hindcast is plausible enough to be used as a form of reanalysis. This model will be used as a form of studies of Lake Onego ecosystem, including long-term projections of ecosystem evolution under different scenarios of climate change and socio-economic development.
1985-2015年奥涅戈湖生态系统氮磷生物地球化学动态三维反演第一部分:长期动态和空间分布
尽管进行了广泛的研究,但几乎没有关于主要生物地球化学通量的信息,这些信息可以表征欧洲奥涅戈湖生态系统过去和现在的状况,并用于对其未来进行可靠的预测估计。为了实现这种能力,我们调整并实施了一个三维耦合的水动力生物地球化学模型,用于Onego湖的营养循环。利用该模型在2 × 2 km网格上以日分辨率重建了Onego湖30年的生态系统动态。与奥涅戈湖和其他大型北方湖泊的现有资料的比较证明,这种后预报是可信的,足以作为一种再分析的形式。该模型将作为奥涅戈湖生态系统研究的一种形式,包括在不同气候变化和社会经济发展情景下的生态系统演变的长期预测。
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