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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Tidal stirring and its impact on water column stability and property distributions in a semi-enclosed shelf sea (Seto Inland Sea, Japan)
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Tidal stirring and its impact on water column stability and property distributions in a semi-enclosed shelf sea (Seto Inland Sea, Japan)

机译:半封闭式货架海(日本濑户内海)中的潮汐搅拌及其对水柱稳定性和性能分布的影响

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The Seto Inland Sea is a partially enclosed shallow sea with a complex bathymetry involving several basins, separated by narrow straits, and numerous islands. The influence of tidal stirring on density stratification and on the distribution of nutrients and chlorophyll in this region has been investigated using a combination of a numerical model of the tidal flow and the results of two extensive surveys of property distributions in the summer regime. The Princeton Ocean Model (POM) has been used to determine the spatial structure of the tidal flow and the results have been verified by comparison with an extensive database of current and elevation measurements. The model indicates a large difference in total energy flux between the western entrance section, which is controlled by a progressive wave regime, and the eastern entrance section which is associated with a predominantly standing wave regime. The combined energy flux input matches the total energy dissipation for the M-2 in the Inland Sea which is found to be similar to 3.4 x 10(9)W. Two ship surveys in August 2002 and 2003 along a central section show a highly differentiated pattern of vertical structure. The potential energy anomaly phi, an index of vertical stability based on density, exhibits a marked inverse correlation with tidal energy dissipation (D) over bar thus confirming the control of stratification by tidal stirring. In most straits, vertical differences of nutrients and chlorophyll are small or negligible while in the low-energy basins there are pronounced vertical differences associated with density stratification. These sluggish basins exhibit oligotrophic conditions in the Surface layer but large nitrate concentrations below the pycnocline and significant chlorophyll maxima in subsurface layer. The physical pattern of varying stratification and fronts is reflected to a considerable degree in the distributions of biochemical properties. (c) 2006 Elsevier Ltd. All rights reserved.
机译:濑户内海是部分封闭的浅海,其复杂的测深仪涉及由狭窄海峡分隔的多个盆地和众多岛屿。结合潮汐流数值模型和两次夏季性质分布广泛调查的结果,研究了该地区潮汐搅拌对密度分层以及养分和叶绿素分布的影响。普林斯顿海洋模型(POM)已用于确定潮汐流的空间结构,并且通过与大量的当前和海拔测量数据库进行比较,对结果进行了验证。该模型表明,由渐进波型控制的西侧入口部分和与主要为驻波型的东侧入口部分之间的总能量通量存在较大差异。组合的能量通量输入与内陆M-2的总能量耗散相匹配,发现其类似于3.4 x 10(9)W。 2002年8月和2003年在中部进行的两次船舶调查显示,垂直结构的模式差异很大。势能异常phi是基于密度的垂直稳定性指标,与整个bar上的潮汐能耗散(D)呈显着负相关,因此确认了通过潮汐搅拌进行的分层控制。在大多数海峡,养分和叶绿素的垂直差异很小或可以忽略不计,而在低能流域,密度分层明显地存在垂直差异。这些缓慢的盆地在表层表现出贫营养条件,但在比可可啉以下的硝酸盐浓度较高,而在表层下的叶绿素最大值较高。分层和前沿变化的物理模式在生化特性的分布中得到了相当大的反映。 (c)2006 Elsevier Ltd.保留所有权利。

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