hdl:10013/epic.22247
      
      
      
      How to Compute Geoid Undulations (Geoid Height Relative to a Given Reference Ellipsoid) from Spherical Harmonic Coefficients for Satellite Altimetry Applications
              Contact
            
            
              mlosch [ at ] awi-bremerhaven.de
            
          
        
        Abstract
      
      This document describes in a cookbook-fashion how to obtain geoid height at a given location on the Earth from spherical harmonic coefficients of a gravity model. The document is intended to aid ``the uninitiated oceanographer'' in constructing geoid undulations relative to a given reference ellipsoid, defined by semi-major axis and flattening parameter, to be used with satellite altimetry products.
          Item Type
        
        
          Miscellaneous
          
          
          
        
      
      
        
          Authors
        
        
      
      
        
          Divisions
        
        
          AWI Organizations > Climate Sciences > Climate Dynamics
AWI Organizations > Climate Sciences > Physical Oceanography of the Polar Seas
AWI Organizations > Climate Sciences > Sea Ice Physics
      
      
      
        AWI Organizations > Climate Sciences > Physical Oceanography of the Polar Seas
AWI Organizations > Climate Sciences > Sea Ice Physics
          Programs
        
        
      
      
      
      
      
      
      
        
          Publication Status
        
        
          Published
        
      
      
      
        
          Eprint ID
        
        
          11802
        
      
    
        Cite as
      
      
        
 
	   
		
Losch, M. 			
		
				
					and
				
					
Seufer, V. 			
		
				
					
		
	
	
  
	(2003):	
	How to Compute Geoid Undulations (Geoid Height Relative to a Given Reference Ellipsoid) from Spherical Harmonic Coefficients for Satellite Altimetry Applications
		
	,	
 
	    [Miscellaneous]
	  
	
      
      
      
        
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