再现拉多加湖生态系统的气候现状

A. V. Isaev, V. Ryabchenko, A. Konik
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引用次数: 0

摘要

根据圣彼得堡波罗的海富营养化模型(SPBEM),提出了拉多加湖三维生态流体力学模型。与现有的拉多加湖生态系统模型不同,所提出的模型是在高分辨率球形网格(水平网格大小≈1 公里)上实现的,包含一个底栖层模块,并描述了水体和底层沉积物中氮和磷的循环。在水文热力学模块中以大气影响和流入拉多加湖的河流径流为动力,在生物地球化学模块中以来自大气和陆地的养分供应为动力,运行了 1979-2018 年期间拉多加湖状态的季节和年际变化。将拉多加湖当前气候状态的计算结果与现有的卫星和历年观测数据进行比较后发现,该模型正确再现了地表温度场的气候季节变化、垂直分布、平均值以及湖泊生态系统主要特征的变化范围。所提出的模型可用于研究外部自然和人为因素对拉多加湖生物地球化学过程和生态系统功能的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reproduction of the Current Climatic State of the Lake Ladoga Ecosystem
A three-dimensional ecohydrodynamic model of Lake Ladoga based on the St. Petersburg Baltic Eutrophication Model (SPBEM) is proposed. Unlike existing models of the Lake Ladoga ecosystem, the proposed model is implemented on a high-resolution spherical grid (horizontal grid size ≈1 km), contains a benthic layer module and describes the cycles of nitrogen and phosphorus in the water column and bottom sediments. A run of the seasonal and interannual variability of the state of Lake Ladoga in the period 1979–2018 was carried out when setting as forcing the atmospheric influence and runoff of rivers flowing into Lake Ladoga for the hydrothermodynamic module and the supply of nutrients from the atmosphere and from land for the biogeochemical module. A comparison of the results of calculating the current climatic state of Lake Ladoga with the available satellite andexpeditionary observation data showed that the model correctly reproduces the climatic seasonal variation of the surface temperature field, its vertical distribution, average values and range of changes in the main characteristics of the lake’s ecosystem. The proposed model can be used to study the influence of external natural and anthropogenic factors on biogeochemical processes and the functioning of the Lake Ladoga ecosystem.
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