
海山宽度调控下近惯性内波的产生与耗散
Generation and dissipation of near-inertial internal waves under the regulation of seamount width
深海中地转流与海山相互作用可激发产生近惯性内波,该内波强度与海山高度相关,与海山宽度的关系尚不明确。本文采用二维MITgcm非静力数值模型探究了地转流与深海海山的相互作用以及海山宽度对近惯性内波产生与耗散的影响。结果表明,地形强迫在海山背流面顶部边缘产生强非线性波-波相互作用,产生近惯性内波并得到发展,使得能量从地转流向近惯性内波传递;在海山高度不变的条件下,海山宽度越小,近惯性内波的强度越大,发展和衰减更快;相较海山的迎流面,背流面的近惯性内波的垂直切变更强,产生的湍流耗散更强。因此,除了海山高度,海山宽度也是调控近惯性内波生成和演化的关键因素。
The interaction between deep-ocean geostrophic current and seamounts can generate near-inertial internal waves (NIWs). While the intensity of these waves relates to the seamount height, its dependence on seamount width remains elusive. This study employs a two-dimensional, non-hydrostatic numerical model based on MITgcm to investigate the interaction of geostrophic current with deep-sea seamounts and examine how differing seamount widths influence the generation and dissipation of NIWs. Our results demonstrate that topographic forcing triggers robust nonlinear wave-wave interactions along the summit edges on the downstream flank of the seamount. This process generates energetic near-inertial internal waves that radiate away and develop, facilitating energy transfer from the geostrophic mean flow to the NIWs. For a fixed seamount height, narrower seamounts induce stronger near-inertial waves, characterized by more rapid wave development and decay. Moreover, the downstream flank exhibits significantly enhanced vertical shears within the near-inertial internal waves, driving greater turbulent dissipation compared to the upstream flank. Therefore, our findings highlight that, in addition to seamount height, seamount width is also a critical factor governing the generation and subsequent evolution of near-inertial internal waves.
深海 / 地转流 / 近惯性内波 / 湍流混合 / 流与地形相互作用 / 非线性波-波相互作用 / MITgcm模型 / 海山宽度
deep ocean / geostrophic current / near-inertial internal waves / turbulent mixing / current-topography interactions / nonlinear wave-wave interactions / MITgcm model / seamount width
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We review the physics of near-inertial waves (NIWs)in the ocean and the observations, theory, and models that have provided our present knowledge. NIWs appear nearly everywhere in the ocean as a spectral peak at and just above the local inertial period f, and the longest vertical wavelengths can propagate at least hundreds of kilometers toward the equator from their source regions; shorter vertical wavelengths do not travel as far and do not contain as much energy, but lead to turbulent mixing owing to their high shear. NIWs are generated by a variety of mechanisms, including the wind, nonlinear interactions with waves of other frequencies, lee waves over bottom topography, and geostrophic adjustment; the partition among these is not known, although the wind is likely the most important. NIWs likely interact strongly with mesoscale and submesoscale motions, in ways that are just beginning to be understood.
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The direct response of the tropical mixed layer to near-inertial waves (NIWs)has only rarely been observed. Here, we present upper-ocean turbulence data that provide evidence for a strongly elevated vertical diffusive heat flux across the base of the mixed layer in the presence of a NIW, thereby cooling the mixed layer at a rate of 244 W m over the 20 h of continuous measurements. We investigate the seasonal cycle of strong NIW events and find that despite their local intermittent nature, they occur preferentially during boreal summer, presumably associated with the passage of atmospheric African Easterly Waves. We illustrate the impact of these rare but intense NIW induced mixing events on the mixed layer heat balance, highlight their contribution to the seasonal evolution of sea surface temperature, and discuss their potential impact on biological productivity in the tropical North Atlantic.
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