摘要
受外部磁场、底质流动及仪器性能等因素影响,利用声学多普勒流速剖面仪(ADCP)自带的磁罗经及底跟踪技术难以为流速确定提供准确的方位和船速基准,从而降低了ADCP流速测量精度并限制了其应用。为此,借助GPS和罗经等外部传感器,提出了一种ADCP流速精确测量方法和全套数据处理模型,替代了ADCP测量中的速度和方位基准,显著提高了ADCP成果精度。实验验证了该方法的有效性。
Influenced by external magnetic interference,bottom tracking bias due to bedload movement and instrument precision,the accurate azimuth and reference of boat velocity are difficult to establish and even incorrect when measured by a acoustic Doppler current profiler(ADCP),which causes ADCP flow measurement to be invalid and thus limit ADCP application.To overcome the shortcomings of the traditional ADCP measurement,this paper puts forward a new method of high-accuracy ADCP measurement by means of an external sensor array.The assignment of the external sensors such as GPS compass array or fiber optic gyrocompass was studied and the resettlement program determined.Calculation models for parameters such as the installation error of ADCP transducer,the attitude parameters(roll,pitch and heading)of vessel,the absolute vessel velocity and the azimuth of ADCP transducer are provided.Based on these parameters in reference to the ADCP measurement principles,a set of new models for determining ADCP flow velocity by replacing the absolute vessel velocity,azimuth and attitude provided by ADCP with those provided by the external sensors were developed.The proposed method and models are validated by an experiment conducted on the Yangtze Estuary.These experimental results show that this proposed method improves the accuracy of the measurement of flow velocity,and enhances the range of applications for ADCP measurement.
出处
《武汉大学学报(信息科学版)》
EI
CSCD
北大核心
2016年第8期1131-1136,共6页
Geomatics and Information Science of Wuhan University
基金
国家自然科学基金(41176068
41376109
41576107)~~