Waves and climate change in the north-east Atlantic
Waves and climate change in the north-east Atlantic
 
  Wave height in the North Atlantic has been observed to increase over the last quarter-century, based on monthly-mean data derived from observations. Empirical models have linked a large part of this increase in wave height with the North Atlantic Oscillation. Wave models provide a tool to study impacts of various climate change scenarios and investigate physical explanations of statistical results. In this case we use a wave model of the NE Atlantic. Model tests were carried out, using synthetic wind fields, varying the strength of the prevailing westerly winds and the frequency and intensity of storms, the location of storm tracks and the storm propagation speed. The strength of the westerly winds is most effective at increasing mean and maximum monthly wave height. The frequency, intensity, track and speed of storms have little effect on the mean wave height but intensity, track and speed significantly affect maximum wave height.
  
  
  L06604
  
  
    
      Wolf, J.
      
        13cf5067-f460-4851-9a09-d6bf7efe575b
      
     
  
    
      Woolf, D.K.
      
        aeb210e8-5fd5-4dd4-903e-6d4ef2df9abe
      
     
  
  
   
  
  
    
      2006
    
    
  
  
    
      Wolf, J.
      
        13cf5067-f460-4851-9a09-d6bf7efe575b
      
     
  
    
      Woolf, D.K.
      
        aeb210e8-5fd5-4dd4-903e-6d4ef2df9abe
      
     
  
       
    
 
  
    
      
  
  
  
  
  
  
    Wolf, J. and Woolf, D.K.
  
  
  
  
   
    (2006)
  
  
    
    Waves and climate change in the north-east Atlantic.
  
  
  
  
    Geophysical Research Letters, 33 (6), .
  
   (doi:10.1029/2005GL025113). 
  
  
   
  
  
  
  
  
   
  
    
      
        
          Abstract
          Wave height in the North Atlantic has been observed to increase over the last quarter-century, based on monthly-mean data derived from observations. Empirical models have linked a large part of this increase in wave height with the North Atlantic Oscillation. Wave models provide a tool to study impacts of various climate change scenarios and investigate physical explanations of statistical results. In this case we use a wave model of the NE Atlantic. Model tests were carried out, using synthetic wind fields, varying the strength of the prevailing westerly winds and the frequency and intensity of storms, the location of storm tracks and the storm propagation speed. The strength of the westerly winds is most effective at increasing mean and maximum monthly wave height. The frequency, intensity, track and speed of storms have little effect on the mean wave height but intensity, track and speed significantly affect maximum wave height.
        
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      Published date: 2006
 
    
  
  
    
  
    
  
    
  
    
  
    
  
    
  
    
     
        Organisations:
        National Oceanography Centre,Southampton
      
    
  
    
  
  
  
    
  
  
        Identifiers
        Local EPrints ID: 32875
        URI: http://eprints.soton.ac.uk/id/eprint/32875
        
          
        
        
        
          ISSN: 0094-8276
        
        
          PURE UUID: 3bb57ede-95b0-44b1-95ea-c9bc3dc7bd68
        
  
    
        
          
        
    
        
          
        
    
  
  Catalogue record
  Date deposited: 12 May 2006
  Last modified: 15 Mar 2024 07:39
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      Contributors
      
          
          Author:
          
            
            
              J. Wolf
            
          
        
      
          
          Author:
          
            
            
              D.K. Woolf
            
          
        
      
      
      
    
  
   
  
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