Non-uniform Sampling Issues Arrising in Shallow Angle 
        Wave Profiling Lidar 
      M.R.Belmont 
      Status: Accepted  
       
        North park Avenue, Exeter University  
           
          Exeter , Devon United Kingdom  
          EX4 4QF  
        Phone: (0)1392 263622  
          Email: M.R.Belmont@exeter.ac.uk 
           
       
      Co-Authors: 
       
       
        Non-umiform Sampling Issues Arrising in Shallow Angle Wave Profiling Lidar 
         
        M.R.Belmont, J.M.K.Horwood and R.W.F.Thurley 
        School of Engineering and Computer Science, 
        University of Exeter. 
        November 2002 
         
         
        Abstract 
         
        The stochastic view of sea-waves developed by Pierson and Neumann, Ref[1,2,3], 
        has provided the only viable framework for sea state forecasting in the 
        range hours to days which reflect the operational planning needs of marine 
        activities. In contrast real time dynamical vessel operations require 
        deterministic sea profile information. The potential advantages offered 
        by technologies able to provide predictive wave input in such real time 
        operations have aroused recent interest in so called deterministic sea-wave 
        prediction (DSWP), Ref[4 - 11], and consequent vessel motion prediction, 
        Ref[6]. Given the relationship between the maximum possible prediction 
        horizon, Ref[5,7,8], and the time factors involved in measurement, data 
        quality assessment and prediction model building DSWP is effectively restricted 
        to situations where linear algorithms, Ref[5,8], can be justified.  
         
        For fixed site applications typically found in the offshore oil and gas 
        industry the wave measurements required to build prediction models can 
        be obtained from developments of existing floating directional wave sensors, 
        Ref[12]. However for moving vessels involved in activities such as aircraft 
        recovery remote sensing ship-based sensors are needed. As will be shown 
        in the full article practical restrictions mean that the radars commonly 
        used for sea state estimation, i.e., surface roughness statistics and 
        wave direction measurements, cannot make the required profile measurements 
        and some form of grazing incidence LIDAR is needed.  
         
        In addition to the marine operations the profiling LIDAR can also be used 
        as a research and monitoring tool in oceanography and in shore environmental 
        studies. One interesting possibility is its use in measuring the spatial 
        and temporal behavior of breaking wave systems that are attracting special 
        attention in coastal erosion investigations. 
         
        The grazing incidence requirement stems from a combination of the sensing 
        range needed, typically 0.5km to 1.0km, and the likely available mast 
        elevations. The geometry of the resulting metrology problem constitutes 
        one of the few examples in large scale engineering where spatial non-uniform 
        sampling becomes critically important. Even if the LIDAR is scanned in 
        uniform angular increments the sea surface shape means that the interception 
        sites of the sensing radiation are highly non-uniformly distributed along 
        the space axis and typical DSWP algorithms, Ref[5,8], require uniformly 
        sampled data. Given that the optimum DSWP mode of operation requires a 
        snapshot of the sea surface acquired in the shortest possible time, consistent 
        with signal to noise ratio considerations, it is vital to require no more 
        samples than the minimum demanded by the Nyquist criterion. Thus it is 
        not possible to substantially oversample and use simple interpolation. 
         
        The general problem of mapping from a set of non-uniform to uniform samples 
        is equivalent to transforming from a non-orthogonal to an orthogonal basis. 
        Given the number of samples involved methods such as direct inversion 
        or the Gram-Schmidt process are far to computationally demanding for the 
        time available in DSWP work. Thus specialist techniques are required. 
        The proposed article examines the aspects of nonuniform sampling relevant 
        to the DSWP wave profiling application, Ref[13 - 21]. As the distribution 
        of non-uniform sample locations varies from one set of measurements to 
        another it is vital to have methods for estimating the computational cost 
        associated with building a prediction model from any given data. Such 
        estimating techniques are examined and appropriate algorithms developed. 
         
        References in full text 
       
      Submitted on November 07, 2002 
       
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