Robert Koslover
                                                                                                                                                    Certified Consultant
                                                         
                            
                         
                                                
    
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                                                Posted:
                            
                                5 years ago                            
                            
                                5 sept. 2020, 12:18 UTC−4                            
                        
                        
                                                    In regard to definitions, see http://www.antenna-theory.com/definitions/axial.php or https://en.wikipedia.org/wiki/Elliptical_polarization .
In regard to checking the handedness of circular polarization, or for a quick/qualitative view of the orientation and ellipticity of the polarization, I usually just plot an animation using Comsol's arrow-plot on a surface capability, and watch the E vector sweep around as the wave phase varies.  You can do this with the fields in/on your model volume, or you can even do it for far-field plots on finite surfaces.  For example, you can do an arrow plot of Efarx, Efary, and Efarz on a hemispherical surface around the origin.
    -------------------
    Scientific Applications & Research Associates (SARA) Inc.
www.comsol.com/partners-consultants/certified-consultants/sara                                                 
                                                
                            In regard to definitions, see http://www.antenna-theory.com/definitions/axial.php or https://en.wikipedia.org/wiki/Elliptical_polarization .
In regard to checking the handedness of circular polarization, or for a quick/qualitative view of the orientation and ellipticity of the polarization, I usually just plot an animation using Comsol's arrow-plot on a surface capability, and watch the E vector sweep around as the wave phase varies.  You can do this with the fields in/on your model volume, or you can even do it for *far-field* plots on finite surfaces.  For example, you can do an arrow plot of Efarx, Efary, and Efarz on a hemispherical surface around the origin.