首页> 外文会议>2014 IEEE/OES Baltic International Symposium : Measuring and modeling of multi-scale interactions in the marine environment: Book of abstracts >Spatial variability of location of the boundaries of the cold intermediate layer and its thickness in the Baltic Sea in spring 2006
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Spatial variability of location of the boundaries of the cold intermediate layer and its thickness in the Baltic Sea in spring 2006

机译:2006年春季波罗的海中冷中间层边界位置及其厚度的空间变异性

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On the basis of field measurement data obtained simultaneously in late April — early May 2006 in the expeditions of the Russian and the German research vessels in the northern and southern parts of the Baltic Proper, the south-north (along the major axis of the sea) variability of the location of the upper and the lower boundaries of the cold intermediate layer is considered. The highest variability of the boundaries from station to station is pointed out, as well as the lack of any clear south-north trend in their changes. This speaks in favor of the independence of the formation of CIL at any particular place — as opposed to the existence of a common sea-scale transport of cold intermediate waters from some common source.
机译:根据2006年4月下旬至2006年5月上旬同时从俄罗斯和德国研究船在波罗的海南部,北部(沿着海的长轴)北部和南部进行的考察获得的实地测量数据)考虑了冷中间层上下边界位置的变化。指出了各站之间边界的最大可变性,以及其变化中没有明显的南北趋势。这表明,在任何特定地点,CIL的形成都是独立的,这与从某些共同来源来的海平面中间冷水的共同海平面运输相反。

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