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From: Eberhard Traenkle (traenkle_at_hidden_email_address.net)
Date: 10/21/1996


Dear Marko,                    (Marko Pekkola)
I am not sure that all members of the metopitics discussion forum are interested in our discussion. I appreciate your paper on elliptical halos in weather. So, I wonder why you do not write a paper on the explanation of elliptical halos by pyramidal crystals. I guess, the reason is that you do not trust your computersimulations. I am sorry, but I prefer to continue the discussion of the details after having analysed the photo of the colored elliptical halos by myself and after having read an English version of your article on elliptical halos in the Finish journal.

    But I like to clarify two points of the previous discussion: 1) In our paper we write that from a critical review of the 23 reports and from interviews of the Finish observers in June 1995 it is evident that most of the elliptical halos occured in the snowy virga of altocumulus clouds. Is this still correct ? 2) I wrote in my last email that our model does not predict color separation of the rings because they are produced by multiple reflections. Indeed, multiple reflections is the main rayclass. However, there are small
contributions from other rayclasses including refraction. Unfortunately we did not check in the simulations the amount of these contributions. So, the
model is consistent with the observation of slightly colored rings.

By the way, there are a few displays which directly show the effect of multiple scattering. I have a slide of the 18.2.88 display showing that the intensity of the ring varies along the ring. The intensity decreases
towards the horizon. This is easily explained by multiple scattering without specifying a detailed model of the ice cloud. The rays with small altitude angle cannot leave the horizontally extended cloud but are scattered
once more before they leave the cloud. I wonder why you did not publish this
interesting photopraph of the 18.2.88 display but another one that only shows
the upper part of the ring.

  Best regards to all of you

                            Eberhard Traenkle