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Estuarine Transport versus Vertical Movement and Mixing of Water Masses in the Gulf of Finland (Baltic Sea)

机译:芬兰海湾(波罗的海)的河口运输与垂直运动和水群体混合

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Weekly mapping of vertical temperature and salinity fields was carried out across the Gulf of Finland in summer 2006 and spring 2007. Using successive cross-gulf vertical sections of salinity and wind data from the region the variations of estuarine and transverse circulation are described. Changes of deep layer phosphate-phosphorus concentrations are found to be related to the described variations in circulation patterns in a season with strong vertical stratification of water column. Cumulative volume transport estimates were obtained using the results of a 3D baroclinic circulation model (HIROMB). We suggest that the north-easterly winds, which intensify the estuarine circulation and lead to the upwelling events along the southern coast of the Gulf of Finland, could have a major impact to the Gulf's ecosystem by importing more saline and phosphorus rich waters. These events with many-fold more intense upward movement and mixing of deep waters (upward diapycnal transport) could contribute significantly to the ventilation of deep layers of the northern Baltic Proper.
机译:垂直温度和盐度场的每周映射在夏季2006和弹簧2007横跨芬兰湾进行从河口和横向流通变化中描述的区域使用盐度和风力数据的连续横海湾垂直部分。发现深层磷酸 - 磷浓度的变化与水柱的强的垂直分层涉及到在循环模式所描述的变型在一个赛季中。使用3D斜压环流模式(HIROMB)的结果得到累积体积传输的估计。我们建议东北风,这加剧了河口循环,导致沿芬兰湾的南部海岸上涌活动,可以通过进口更多的盐,磷丰富的水域拥有海湾的生态系统产生重大影响。这些事件与许多倍更加激烈向上运动和深水混合(向上diapycnal运输)可能波罗的海北部正确的深层通风显著贡献。

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