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A study of surface currents in the coastal ocean outside Chesapeake Bay using HF radar

机译:利用高频雷达研究切萨皮克湾外沿海海洋的地表电流

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Surface circulation in the coastal ocean outside of the Chesapeake Bay was studied using high frequency radar. Radar data were collected and analyzed from three long range HF radar sites operating at 5 MHz: 1) LISL located at Little Island Park in Virginia Beach 2) CEDR on Cedar Island, a barrier island offshore of Wachapreague, Virginia and 3) DUCK located in Duck, NC. These sites are long-term monitoring stations, part of a regional ocean observing system funded under the Mid-Atlantic Regional Association Coastal Ocean Observing System (MARACOOS). This study reports on surface current data collected from mid-August to mid-September 2011. Radial data were compared with ADCP current data measured at NOAA National Data Buoy Center station 44014. R2 correlation values ranged from 0.61 to 0.76 and rms differences ranged from 12 to 14 cm/s. Total velocity data were also compared with the ADCP data. A complex correlation analysis of the ADCP data compared with radar total vector currents yielded a correlation amplitude of 0.6 and a correlation angle of 8 degrees. Circulation patterns during the study period, before the passage of Hurricane Irene, are illustrated with particle trajectories. Subtidal circulation has been described in terms of principal direction of flow. Locally averaged coastal surface subtidal currents were correlated with winds measured at the NDBC CHLV2 station (Chesapeake Light Tower). East-west (across-shelf) subtidal currents in the area offshore of the Bay are highly correlated with north-south winds (R2 = 0.85).
机译:使用高频雷达研究了切萨皮克湾以外沿海海洋的表面循环。从3个工作在5 MHz的远距离高频雷达站点收集并分析了雷达数据:1)LISL位于弗吉尼亚海滩的小岛公园2)CEDR位于锡达岛,位于弗吉尼亚州Wachapreague的近海障壁岛,以及3)DUCK位于北卡罗来纳州的鸭子。这些站点是长期监测站,是由中大西洋区域协会海岸海洋观测系统(MARACOOS)资助的区域海洋观测系统的一部分。这项研究报告了从2011年8月中旬到9月中旬收集的地面电流数据。将径向数据与在NOAA国家数据浮标中心站44014上测量的ADCP当前数据进行了比较。R 2 相关值的范围为0.61至0.76,均方根差为12至14 cm / s。总速度数据也与ADCP数据进行了比较。与雷达总矢量电流相比,对ADCP数据进行了复杂的相关性分析,得出相关幅度为0.6,相关角度为8度。用粒子轨迹说明了飓风“艾琳”通过之前研究期间的循环模式。潮汐环流已根据主要流动方向进行了描述。局部平均的沿海地表潮汐流与在NDBC CHLV2站(切萨皮克灯塔)测得的风相关。海湾近海区域的东西向(跨架)潮流与南北风高度相关(R 2 = 0.85)。

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