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Observations of near-surface ocean currents at varying depths usinga new multifrequency HF radar

机译:利用观测不同深度的近地表海流。新型多频HF雷达

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A new multifrequency (4-25 MHz) HF radar was installed at the LongMarine Lab. (University of California at Santa Cruz) on the north coastof Monterey Bay CA in July, 1996. This radar is capable of observingnear-surface currents at varying depths in the top two meters of theocean. Observations were made over a ten day period in March, 1997during which there was a strong land-sea breeze circulation overMonterey Bay. Radial current measurements corresponding to depths ofabout 0.3, 0.5, 1.0 and 1.4 m were made during this period using HFradar data from four operating frequencies. Fourier analysis of thesedata shows that very near the surface the strongest periodic componentis a diurnal one corresponding to the diurnally varying surface stressfrom the land-sea breeze. At deeper depths the diurnal componentremains, but a semi-diurnal component grows in strength with increasingdepth of the current measurement. Thus, multifrequency HF radar combinedwith deeper current measurements from buoys and moorings are able toinvestigate the upper layer of the coastal ocean where wind and tidallydriven currents struggle for dominance
机译:朗格机场安装了新的多频(4-25 MHz)HF雷达 海洋实验室(加利福尼亚大学圣克鲁斯分校)在北海岸 于1996年7月在加利福尼亚蒙特利湾(Monterey Bay CA)发射。 在顶部两米深处不同深度的近地表电流 海洋。在1997年3月进行了十天的观察 在此期间,强烈的陆海风环流 蒙特利湾。对应于深度的径向电流测量 在此期间使用HF制作了约0.3、0.5、1.0和1.4 m 来自四个工作频率的雷达数据。这些的傅立叶分析 数据表明,在表面附近,最强的周期性成分 是一个与昼夜变化的表面应力相对应的昼夜 从陆海风。日深部分 仍然存在,但半昼夜部分的强度会随着强度的增加而增加 当前测量的深度。因此,多频HF雷达组合 从浮标和系泊设备获得的更深的电流测量值能够 调查风和潮汐沿岸的沿海海洋的上层 激流争夺主导地位

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