Subtleties in forcing eddy resolving ocean models with satellite wind data
Subtleties in forcing eddy resolving ocean models with satellite wind data
 
  Using new global satellite remote sensing data, we show that ignoring the ocean current dependence in the wind stress artificially increases global wind power input to the oceanic general circulation by about 32%, and more than doubles the input in the regions of strong ocean current systems. Scatterometer-derived wind stress naturally accounts for the moving ocean that is not included in traditional wind stress products. However, forcing an ocean model with a scatterometer-derived wind stress cannot actually account for the ocean current effect on the wind power input. The difference between the real and modeled surface eddy fields can reduce the damping associated with the ocean current dependence in wind stress, leading to a positive bias in global wind power input of about 23%. Most of this spurious energy flux goes directly to the fluctuation eddy field and is several times larger than the energy flux to real ocean eddies.
  Ocean circulation, Wind power, World ocean, Modeling, Satellites, Parameterization
  
  
  240-251
  
    
      Xu, Yongsheng
      
        e058b027-51a7-49c5-8f53-4f73cbb49e64
      
     
  
    
      Scott, Robert B.
      
        f82756a5-f04c-41f1-a6c8-12574b9814cf
      
     
  
  
   
  
  
    
      2008
    
    
  
  
    
      Xu, Yongsheng
      
        e058b027-51a7-49c5-8f53-4f73cbb49e64
      
     
  
    
      Scott, Robert B.
      
        f82756a5-f04c-41f1-a6c8-12574b9814cf
      
     
  
       
    
 
  
    
      
  
  
  
  
  
  
    Xu, Yongsheng and Scott, Robert B.
  
  
  
  
   
    (2008)
  
  
    
    Subtleties in forcing eddy resolving ocean models with satellite wind data.
  
  
  
  
    Ocean Modelling, 20 (3), .
  
   (doi:10.1016/j.ocemod.2007.09.003). 
  
  
   
  
  
  
  
  
   
  
    
      
        
          Abstract
          Using new global satellite remote sensing data, we show that ignoring the ocean current dependence in the wind stress artificially increases global wind power input to the oceanic general circulation by about 32%, and more than doubles the input in the regions of strong ocean current systems. Scatterometer-derived wind stress naturally accounts for the moving ocean that is not included in traditional wind stress products. However, forcing an ocean model with a scatterometer-derived wind stress cannot actually account for the ocean current effect on the wind power input. The difference between the real and modeled surface eddy fields can reduce the damping associated with the ocean current dependence in wind stress, leading to a positive bias in global wind power input of about 23%. Most of this spurious energy flux goes directly to the fluctuation eddy field and is several times larger than the energy flux to real ocean eddies.
        
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      Published date: 2008
 
    
  
  
    
  
    
  
    
  
    
  
    
  
    
     
        Keywords:
        Ocean circulation, Wind power, World ocean, Modeling, Satellites, Parameterization
      
    
  
    
  
    
  
  
  
    
  
  
        Identifiers
        Local EPrints ID: 65652
        URI: http://eprints.soton.ac.uk/id/eprint/65652
        
          
        
        
        
          ISSN: 1463-5003
        
        
          PURE UUID: 2d93a9c0-e3d5-4ba1-ab80-3b442e27117e
        
  
    
        
          
        
    
        
          
        
    
  
  Catalogue record
  Date deposited: 03 Mar 2009
  Last modified: 13 Mar 2024 17:47
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      Contributors
      
          
          Author:
          
            
            
              Yongsheng Xu
            
          
        
      
          
          Author:
          
            
            
              Robert B. Scott
            
          
        
      
      
      
    
  
   
  
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