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In/out-flow of coastal water in Vestfjorden

机译:韦斯特峡湾的沿海水流入/流出

摘要

Hydrographic sections in Vestfjorden, Northern Norway, during winter1977 showed strong horizontal temperature gradients on thewest side of the fjord indicating an outflow of cold coastalwater. Analysis of sea thermograph records from the ship routecrossing the fjord between Stamsund and Bodø in the years back to1936 shows that this hydrographic structure is a permanentphenomenon in the wintertime. Mean temperatures along thethermograph section for February, March and April are presented.A method is suggested for the estimation of the residence time ofcoastal water in the fjord by using data from standard meteorologicalstations combined with the thermograph data and data from a fixedhydrographic station.
机译:1977年冬季,挪威北部Vestfjorden的水文剖面显示,峡湾西侧的水平温度梯度很强,表明沿海冷水流出。对自1936年以来跨越Stamsund和Bodø之间峡湾的船舶航路进行的海洋温度记录分析的结果表明,这种水文结构是冬季的永久现象。给出了2月,3月和4月沿热成像仪部分的平均温度。建议使用标准气象站的数据,热成像仪的数据和固定水文站的数据估算峡湾沿海水的停留时间。

著录项

  • 作者

    Sundby Svein;

  • 作者单位
  • 年度 1978
  • 总页数
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类

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