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GPS estimation of atmospheric water vapour from a moving platform

机译:GPS估算移动平台中的大气水蒸气

摘要

Measuring water vapour content, and its variability, in the atmosphere is important for meteorological and climatological research. Recently, a technique for the remote sensing of water vapour in the atmosphere using ground-based GPS has been rapidly developed. An estimation accuracy for integrated water vapour content of 1– has been routinely available from such ground-based GPS networks (Dodson and Baker, Proceedings of the ION National Technical Meeting, Navigation 2000, California, January 21–23). Extending this technique into the sea on a moving platform would be greatly beneficial for meteorological research, such as the calibration of satellite data and the investigation of the sea/air interface as well as forecasting and climate studies. However, whether the water vapour can be separated from the motion of the GPS receiver in the estimation process itself, is still an open question. In this paper, a new method, based on a Kalman filter, has been developed to deal with this problem. The initial experiment shows that the accuracy of estimated tropospheric delay from a moving platform is comparable to that from (static) land based receivers.
机译:测量大气中的水蒸气含量及其变化性对于气象和气候研究很重要。近年来,利用地面GPS对大气中的水蒸气进行遥感的技术得到了迅速发展。通常可以从这样的地面GPS网络(Dodson和Baker,ION国家技术会议论文集,2000年,加利福尼亚,导航,1月21日至23日)获得1–的综合水蒸气含量的估算精度。将该技术扩展到移动平台上的海中,将对气象研究非常有益,例如卫星数据的校准,海/空界面的研究以及预报和气候研究。但是,在估计过程本身中,是否可以将水蒸气与GPS接收器的运动分开,这仍然是一个悬而未决的问题。本文提出了一种基于卡尔曼滤波器的新方法来解决这一问题。初始实验表明,从移动平台估计的对流层延迟的精度与(静态)陆基接收器的估计精度相当。

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