Observations over an annual cycle and simulations of wind-forced oscillations near the critical latitude for diurnal-inertial resonance

被引:28
作者
Hyder, P. [1 ]
Simpson, J. H. [2 ]
Xing, J. [3 ]
Gille, S. T. [4 ,5 ]
机构
[1] Met Off, Exeter EX1 3PB, Devon, England
[2] Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Anglesey, Wales
[3] Natl Oceanog Ctr, Liverpool L3 5DA, Merseyside, England
[4] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
[5] Univ Calif San Diego, Dept Mech & Aerosp Engn, La Jolla, CA 92093 USA
关键词
Diurnal current; Inertial current; Sea breeze; Diurnal wind; Namibia; Benguela current; SEA-BREEZE; CONTINENTAL-SHELF; VERTICAL STRUCTURE; QUIKSCAT SCATTEROMETRY; STRESS MEASUREMENTS; INTERNAL WAVES; OCEAN RESPONSE; MIXED-LAYER; WEST-COAST; CURRENTS;
D O I
10.1016/j.csr.2011.06.001
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Sea breezes are characteristic features of coastal regions that can extend large distances from the coastline. Oscillations close to the inertial period are thought to account for around half the kinetic energy in the global surface ocean and play an important role in mixing. In the vicinity of 30 degrees N/S, through a resonance between the diurnal and inertial frequencies, diurnal winds could force enhanced anti-cyclonic rotary motions that contribute to near-inertial energy. Observations of strong diurnal anti-cyclonic currents in water of depth 175 m off the Namibian coastline at 28.6 degrees S are analysed over the annual cycle. Maxima in the diurnal anti-cyclonic current and wind stress amplitudes appear to be observed during the austral summer. Both the diurnal anticyclonic current and wind stress components have approximately constant phase throughout the year. These observations provide further evidence that these diurnal currents may be wind forced. Realistic General Ocean Turbulence Model (GOTM) 1-D simulations of diurnal wind forcing, including the first order coast-normal surface slope response to diurnal wind forcing, represent the principal features of the observed diurnal anti-cyclonic current but do not replicate the observed vertical diurnal current structure accurately. Cross-shelf 2-D slice simulations suggest that the first order surface slope response approximation applies away from the coast (> 140 km). However, nearer to the coast, additional surface slope variations associated with spatial variations in the simulated velocity field (estimated from Bernoulli theory) appear to be significant and also result in transfer of energy to higher harmonics. Evidence from 3-D simulations at similar latitude in the northern hemisphere suggests that 3-D variations, including propagating near-inertial waves, may also need to be considered. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1576 / 1591
页数:16
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