首页> 外文期刊>Journal of marine systems: journal of the European Association of Marine Sciences and Techniques >Observed internal tides and near-inertial waves on the continental shelf and slope off Jaigarh, central west coast of India
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Observed internal tides and near-inertial waves on the continental shelf and slope off Jaigarh, central west coast of India

机译:在印度中西部海岸斋加尔附近的大陆架和斜坡上观测到的内潮和近惯性波

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The characteristics of internal tides (ITs) and near-inertial waves (NIWs) on the continental shelf and slope off Jaigarh (17 degrees N), central west coast of India were studied. Eight-month (March-October) long Acoustic Doppler Current Profiler (ADCP) measurements made in the year 2008 were used in the present study. Analysis of sea surface heights from satellite altimeter data, where the tracks of the satellites are oriented nearly in the direction of the semimajor axis of barotropic tides, reveals the presence of diurnal and semidiurnal internal tides with surface amplitudes of about 2 cm. Baroclinic current spectra of horizontal velocities show peaks in IT frequencies of M-2, S-2, K-1 and O-1 and in inertial frequency (f). The observed current spectra show higher energies than those in Garrett-Munk reference spectra by about 2-3 times. Based on the estimates of "critical topography" (where the topographic slope is equal to the slope of IT) and computed barotropic body force (Baines, 1982), the shelf-edge, mid-slope and deep part of the slope region are found to be the possible generation sites of internal tides in the region. Over the period of observation, the IT on the slope is found to be energetic, with a strong IT during March to mid-April (pre-monsoon period). Whereas, on the shelf, IT is weak during the pre-monsoon and found to be strong in the southwest monsoon. The available hydrographic data and model simulated hydrography suggest that this difference is linked with the stratification changes on the shelf and slope during these seasons, where the stratification is found to be weak on the shelf and strong on the slope during pre-monsoon. Strong low-mode NIW is observed on the shelf associated with the storm events while the NIW is found to be less energetic on the slope. (C) 2015 Elsevier B.V. All rights reserved.
机译:研究了印度中西部沿海Jaigarh(北纬17度)的大陆架和斜坡上的内潮(IT)和近惯性波(NIW)的特征。本研究使用了在2008年进行的八个月(三月至十月)长的声学多普勒电流剖面仪(ADCP)测量。从卫星高度计数据分析海面高度时,卫星的轨道几乎指向正压潮汐的半长轴方向,揭示了存在日潮和半日潮的内部潮汐,其表面振幅约为2 cm。水平速度的斜压电流谱显示出M-2,S-2,K-1和O-1的IT频率以及惯性频率(f)的峰值。所观察到的电流光谱显示出比Garrett-Munk参考光谱更高的能量约2-3倍。根据“临界地形”(地形坡度等于IT坡度)的估计值和计算出的正压体力(Baines,1982年),可以找到斜坡区域的陆缘,中坡和深部成为该地区内部潮汐的可能发源地。在观察期内,发现斜坡上的IT充满活力,在3月至4月中旬(季风前期)期间,IT表现强劲。而在架子上,IT在季风前很弱,而在西南季风中很强。现有的水文学数据和模型模拟水文学表明,这种差异与这些季节在陆架和斜坡上的分层变化有关,在季风期间,在陆架和斜坡上发现分层很弱,而在斜坡上则分层很强。在与风暴事件相关的架子上观察到强的低模态NIW,而NIW在斜坡上的能量较低。 (C)2015 Elsevier B.V.保留所有权利。

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