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Hypoxia in the Lower St. Lawrence Estuary: How physics controls spatial patterns

机译:下劳伦斯河口缺氧:物理学如何控制空间格局

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[1] A laterally integrated advection-diffusion two-dimensional model was implemented to simulate the spatial distribution of dissolved oxygen and the development of hypoxic conditions in the deep waters of the Laurentian Channel (Estuary and Gulf of St. Lawrence, Eastern Canada). Our simulations reveal that the horizontal distribution of dissolved oxygen in the bottom waters of the Laurentian Channel is determined by a combination of physical and biogeochemical processes, whereas its vertical distribution is governed by the deep water circulation. This result strongly suggests that the physics of the system and the source water properties are mostly responsible for the generation of a mid-water column oxygen minimum and the oxygen distribution pattern in the deep water column.
机译:[1]采用横向整合的对流扩散二维模型来模拟溶解氧的空间分布和劳伦斯海峡(加拿大东部海口和圣劳伦斯湾)深水处的低氧条件的发展。我们的模拟显示,Laurentian海峡底部水中溶解氧的水平分布是由物理和生物地球化学过程共同决定的,而其垂直分布则由深水循环控制。该结果有力地表明,系统的物理性质和源水性质是造成中间水塔最低氧气含量和深水塔中氧气分布规律的主要原因。

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