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Assessment of shelf sea tides and tidal mixing fronts in a global ocean model

机译:在全球海洋模型中评估货架海报和潮汐混合前线

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摘要

Tidal mixing fronts, which represent boundaries between stratified and tidally mixed waters, are locations of enhanced biological activity. They occur in summer shelf seas when, in the presence of strong tidal currents, mixing due to bottom friction balances buoyancy production due to seasonal heat flux. In this paper we examine the occurrence and fidelity of tidal mixing fronts in shelf seas generated within a global 3-dimensional simulation of the HYbrid Coordinate Ocean Model (HYCOM) that is simultaneously forced by atmospheric fields and the astronomical tidal potential. We perform a first order assessment of shelf sea tides in global HYCOM through comparison of sea surface temperature, sea surface tidal elevations, and tidal currents with observations. HYCOM was tuned to minimize errors in M-2 sea surface heights in deep water. Over the global coastal and shelf seas (depths < 200 m) the area-weighted root mean square error of the M-2 sea surface amplitude in HYCOM represents 35% of the 50 cm root mean squared M-2 sea surface amplitude when compared to satellite constrained models TPXO8 and FES2014. HYCOM and the altimeter constrained tidal models TPXO8 and FES2014 exhibit similar skill in reproducing barotropic tidal currents estimated from in-situ current meter observations. Through comparison of a global HYCOM simulation with tidal forcing to a global HYCOM simulation with no tides, and also to previous regional studies of tidal mixing fronts in shelf seas, we demonstrate that HYCOM with embedded tides exhibits quite high skill in reproducing known tidal mixing fronts in shelf seas. Our results indicate that the amount of variability in the location of the tidal mixing fronts in HYCOM, estimated using the Simpson-Hunter parameter, is consistent with previous studies when the differences in the net downward heat flux, on a global scale, are taken into account. We also provide evidence of tidal mixing fronts on the North West Australian Shelf for which we have
机译:潮汐混合前线,其代表分层和整个混合水之间的边界,是增强生物活性的位置。它们发生在夏季保质海洋时,在强烈的潮流存在下,由于季节性热通量,由于底部摩擦余量的浮力生产。在本文中,我们研究了在混合坐标海洋模型(Sycom)的全局三维模拟中产生的潮汐混合前沿的发生和保真度,其同时由大气领域和天文潮汐潜力。我们通过对海面温度,海面潮汐升高和潮流进行观测,在全球性胰赛人中对全球性赛道的一级评估进行了一阶评估。调整察加科以最小化深水中M-2海面高度的误差。在全球沿海和货架上(深度<200米),Hycom中M-2海面幅度的区域加权根均方误差表示与...相比卫星约束模型TPXO8和FES2014。 Hycom和高度计约束的潮汐模型TPXO8和FES2014表现出类似于原位当前仪表观测的波高的潮流的同类技能。通过对全球性Hycom模拟的比较拓展到全球性察科仿真,没有潮汐,以及以前的潮汐混合阵线在保质期的区域研究中,我们证明了嵌入式潮汐的喀康康表现出相当高的技能在再现已知的潮汐混合前线方面具有相当高的技能在货物海洋中。我们的结果表明,使用SIMPSON-HUNTER参数估计,使用SIMPSON-HUNTER参数估计的潮汐混合前沿的变化量与先前的研究符合全球规模的净向量的差异帐户。我们还提供了我们拥有的西北澳大利亚货架上的潮汐混合前线的证据

著录项

  • 来源
    《Ocean modelling》 |2019年第2019期|共19页
  • 作者单位

    Royal Meteorol Soc Welsh Local Ctr Reading Berks England;

    Univ Michigan Dept Earth &

    Environm Sci Ann Arbor MI 48109 USA;

    UK Met Off Exeter Devon England;

    Florida State Univ Ctr Ocean Atmospher Predict Studies Tallahassee FL 32306 USA;

    Florida State Univ Ctr Ocean Atmospher Predict Studies Tallahassee FL 32306 USA;

    UK Met Off Exeter Devon England;

    Florida State Univ Ctr Ocean Atmospher Predict Studies Tallahassee FL 32306 USA;

    Naval Res Lab Stennis Space Ctr MS USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 海洋学;
  • 关键词

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