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A modelling approach to assess the effects of atmospheric nitrogen deposition on the marine ecosystem in the Bohai Sea, China

机译:评估大气氮沉积对渤海海洋生态系统影响的建模方法

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Atmospheric deposited nitrogen (AD-N) approximates or exceeds riverine input in many coastal ecosystems, such as the Bohai Sea (BHS) which is one of the most eutrophic coastal waters in China. We construct a three-dimensional (3D) physical-biogeochemical model to understand the influence of atmospheric dissolved inorganic nitrogen (DIN) on the infra- and inter-annual variations of phytoplankton blooms and nutrient dynamics in the BHS. The biological component, which is coupled to the Regional Ocean Modelling System (ROMS), is a simple but widely used Nutrient-Phytoplankton-Zooplankton-Detritus (NPZD) model with eight state variables. The model simulation successfully reproduces the spatial and temporal variations of observed DIN and dissolved inorganic phosphorus (DIP) and the climatological features of phytoplankton biomasses (chlorophyll a), which confirms the major role of air-transported nutrients in controlling standing stocks and nutrient limitations. The modelling results show that the relative contributions of deposited nitrogen to the total DIN in the seawater for the Bohai, Laizhou and Liaodong Bays and Central Bohai Basin reach 84.8%, 49.3%, 37.4% and 44.4% on average, respectively. The relative contribution ratio is approximately 54% for the entire Bohai region, causing a 56.5% increase in the phytoplankton biomass on average. These results also indicate that the effects of AD-N on nutrient and phytoplankton dynamics vary widely in regional areas because of the uneven spatial distribution of nitrogen deposition fluxes and also partially because of the hydrodynamic conditions, shortwave radiation and water temperatures.
机译:在许多沿海生态系统中,例如中国最富营养的沿海水域之一的渤海(BHS),大气沉积氮(AD-N)接近或超过河流输入。我们构建了一个三维(3D)物理生物地球化学模型,以了解大气中溶解的无机氮(DIN)对BHS浮游植物绽放的年际和年际变化以及养分动态的影响。生物成分与区域海洋建模系统(ROMS)耦合,是一种简单但广泛使用的具有八个状态变量的营养-浮游植物-浮游动物-碎屑(NPZD)模型。该模型模拟成功地再现了观察到的DIN和溶解的无机磷(DIP)的时空变化以及浮游植物生物量(叶绿素a)的气候特征,这证实了空气中输送的养分在控制常规种群和养分限制方面的主要作用。模拟结果表明,渤海,莱州湾,辽东湾和渤海中部海域沉积氮对总DIN的相对贡献分别达到84.8%,49.3%,37.4%和44.4%。整个环渤海地区的相对贡献率约为54%,使浮游植物生物量平均增加56.5%。这些结果还表明,由于氮沉积通量的空间分布不均匀,以及部分由于水动力条件,短波辐射和水温,AD-N对养分和浮游植物动力学的影响在区域区域差异很大。

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