海气边界风流关系的高频雷达观测

J. Vesecky, L. Meadows, Y. Fernandez, C. Teague, J. Daida, J. Paduan, R. R. Delgado, P. Hansen
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引用次数: 2

摘要

1997年6月,一对新的多频率(4-25 MHz)高频雷达分别安装在蒙特利湾北部和东部海岸的Long海洋实验室(加州大学圣克鲁斯分校)和Moss Landing海洋实验室(加州州立大学)。这些雷达使用四种频率来观察海洋顶部三米不同深度的近表面洋流。据报告,1997年6月进行了为期一周的观测,期间蒙特雷湾上空有强烈的陆海微风环流。在海湾口附近的MBARI M1浮标上进行了风速测量。对这些数据的分析表明,近地面流和风型之间存在明显的耦合,并有证据表明,动量通过水柱的垂直转移随时间而变化。这些和其他高频雷达观测为地面风速和风向的有限检索提供了基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
HF radar observations of wind-current relationships at the air-sea boundary
In June, 1997 a pair of new multifrequency (4-25 MHz) HF radars were installed at the Long Marine Laboratory (University of California at Santa Cruz) and Moss Landing Marine Laboratory (California State Universities) on the north and east coasts of Monterey Bay, respectively. These radars use four frequencies to observe near-surface currents at varying depths in the top three meters of the ocean. Observations, reported, were made over a one-week period in June, 1997 during which there was a strong land-sea breeze circulation over Monterey Bay. Wind measurements were made at the MBARI M1 buoy near the mouth of the bay. Analysis of these data show that a distinct coupling exists between the near-surface current and wind pattern with evidence of the time-dependent vertical transfer of momentum through the water column. These and other HF radar observations provide a basis for limited retrieval of both surface wind speed and direction.
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