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Calibration and Validation of Direction-Finding High-Frequency Radar Ocean Surface Current Observations

机译:测向高频雷达海面电流观测值的校准与验证

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摘要

This paper focuses on the validation of remotely sensed ocean surface currents from SeaSonde-type high-frequency (HF) radar systems. Hourly observations during the period July 22, 2003 through September 9, 2003 are used from four separate radar sites deployed around the shores of Monterey Bay, CA. Calibration of direction-finding techniques is addressed through the comparisons of results obtained using measured and ideal (i.e., perfect) antenna patterns. Radial currents are compared with observations from a moored current meter and from 16 surface drifter trajectories. In addition, four overwater baselines are used for radar-to-radar comparisons. Use of measured antenna patterns improves system performance in almost all cases. Antenna-pattern measurements repeated one year later at three of the four radar locations exhibit only minor changes indicating that pattern distortions are stable. Calibrated results show root-mean-square (rms) radial velocity differences in the range of 9.8-13.0 cm/s, which suggest radar observation error levels in the range of 6.9-9.2 cm/s. In most cases, clear evidence of bearing errors can be seen, which range up to 30deg for uncalibrated radar-derived radial currents and up to 15deg for currents obtained using measured antenna patterns. Bearing errors are not, however, constant with angle. The results recommend use of measured antenna patterns in all SeaSonde-type applications. They also recommend an expanded simulation effort to better describe the effects of antenna-pattern distortions on bearing determination under a variety of ocean conditions
机译:本文着重于验证来自SeaSonde型高频(HF)雷达系统的遥感海面电流。 2003年7月22日至2003年9月9日期间的每小时观测值是从部署在加利福尼亚州蒙特雷湾沿岸的四个单独的雷达站点使用的。测向技术的校准通过比较使用实测和理想(即完美)天线方向图获得的结果来解决。将径向电流与来自系泊电流计和16条地面漂移器轨迹的观测值进行比较。此外,四个水上基准线用于雷达与雷达的比较。在几乎所有情况下,使用测得的天线方向图都会改善系统性能。一年后在四个雷达位置中的三个位置重复进行的天线方向图测量仅显示微小变化,表明方向图失真是稳定的。校准结果显示径向均方根(rms)径向速度差异在9.8-13.0 cm / s的范围内,这表明雷达观测误差水平在6.9-9.2 cm / s的范围内。在大多数情况下,可以看到清晰的轴承误差证据,对于未经校准的雷达衍生径向电流,误差范围高达30deg,对于使用测量天线方向图获得的电流,误差范围高达15deg。但是,轴承误差并非随角度恒定。结果建议在所有SeaSonde类型的应用中使用测得的天线方向图。他们还建议扩展仿真工作,以更好地描述各种海洋条件下天线方向图失真对方位确定的影响

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