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Ice-induced seasonal variability of tidal constants in the Arctic Ocean

机译:冰引起的北冰洋潮汐季节变化

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The results for three-dimensional (3D) winter and summer tidal flows in the homogeneous Arctic Ocean, obtained with the use of a modified version of the 3D finite-element hydrothermodynamic model QUODDY-4, are presented. It is shown that seasonal variability of the M-2 tidal constants (amplitudes and phases of tidal sea surface level elevations) in the Central and Canadian parts of the Arctic Ocean is less than the error in the predicted tidal sea surface level elevations. This means that the seasonal variability can be neglected at least as a first approximation. A different situation is encountered in the Siberian continental shelf, where seasonal changes of tidal amplitude are +/-5 cm, while those of tidal phase vary from 15 degrees to several tens of degrees. (C) 2009 Elsevier Ltd. All rights reserved.
机译:给出了使用3D有限元流体热力学模型QUODDY-4的修改版获得的北冰洋均匀冬季和夏季潮汐流的三维(3D)结果。结果表明,北冰洋中部和加拿大部分M-2潮汐常数的季节性变化(潮汐海平面高度的幅度和相位)小于预报的潮汐海平面高度误差。这意味着季节性变化至少可以作为一阶近似值而忽略。在西伯利亚大陆架遇到了另一种情况,潮汐振幅的季节变化为+/- 5 cm,而潮汐相的季节变化范围为15度至几十度。 (C)2009 Elsevier Ltd.保留所有权利。

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