Seasonality of Internal Tides in the Strait of Hormuz: Observations and Modeling

IF 3.3 2区 地球科学 Q1 OCEANOGRAPHY
M. P. Subeesh, Hajoon Song, Yacine Addad, Jeffery R. Scott, John Marshall, Maryam R. Al Shehhi
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Abstract

The seasonality of internal tides in shallow seas is primarily controlled by changes in stratification. This study explores how semidiurnal and diurnal internal tides respond differently to seasonal stratification, using mooring observations and numerical modeling in the Strait of Hormuz, the gateway for hypersaline Arabian Gulf waters. Semidiurnal internal tides are weak during winter, which is attributed to relatively weak stratification, whereas diurnal internal tides are enhanced. In the remaining seasons, internal tides are strong in both bands. Estimates of energy flux and barotropic-to-baroclinic conversion rates from observations and modeling show a likely generation site near the mooring location. In winter, this generation site turns subcritical at semidiurnal frequencies and supercritical at diurnal frequencies. In addition, barotropic tides show significant amplification at the diurnal frequency during winter. Thus, supercritical topography along with strong barotropic tidal forcing enhances the diurnal internal tides. In the remaining seasons, the topography becomes either critical or supercritical for the semidiurnal frequency and supercritical for the diurnal frequency, resulting in strong internal tide generation. The results of our model show that low-frequency currents significantly influence stratification in the strait, thus playing a crucial role in modulating internal tides. In turn, vertical mixing orchestrated by those tides may be important in setting water mass transformation rates, stratification, and exchange through the strait.

Abstract Image

浅海内潮的季节性主要受分层变化的控制。本研究利用在霍尔木兹海峡(阿拉伯湾高盐度水域的门户)进行的系泊观测和数值建模,探讨了半日和昼夜内潮对季节性分层的不同反应。冬季的半日内潮汐较弱,这归因于相对较弱的分层,而昼夜内潮汐则增强。在其余季节,两个波段的内潮都很强。通过观测和建模估算的能量通量和气压-气压转换率显示,锚泊点附近可能有一个内潮生成点。在冬季,该发电站在半昼夜频率时处于亚临界状态,而在昼夜频率时则处于超临界状态。此外,在冬季,气压潮在昼夜频率上有明显的放大现象。因此,超临界地形和强大的向气压潮汐作用增强了昼夜内潮。在其余季节,地形在半日频变得临界或超临界,在昼频变得超临界,从而产生强烈的内潮。我们的模型结果表明,低频洋流对海峡的分层有显著影响,因此在调节内潮方面起着至关重要的作用。反过来,这些潮汐所协调的垂直混合可能在确定海峡的水质转化率、分层和交换方面起着重要作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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