Abstract
This paper is concerned with depolarization caused by rain due to nonsphericity of drops and the distribution of their axes orientations. The drops are assumed to be oblate spheroids having canting angles distribution obtained by Saunders. Differential phase shift as well as differential attenuation is important in the calculation of depolarization and the values proposed by Oguchi and Hosoya are utilized. In the first part expression to calculate depolarization amount for a uniform precipitation rate are presented. But communication engineers are usually interested on statistical variations of depolarization amount, so the second part of this paper is concerned with statistical distribution of depolarization. The rain cell proposed by Misme and Fimbel is used to describe the rain model over a path. If the precipitation rate distribution is known in one point of the path, the depolarization distribution is obtained by assuming only one rain cell along the path where, for a long time observation, the precipitation rate distribution for all points is the same.
Analyse
Cet article analyse la dépolarisation par la pluie due à la nonsphéricité des gouttes et à la distribution des orientations de leurs axes. On suppose que les gouttes sont des sphéroïdes aplatis dont les angles d’inclinaison obéissent à la distribution de Saunders. Pour la rotation différentielle de phase et l’affaiblissement différentiel qui sont également importants dans le calcul de la dépolarisation, on utilise les valeurs proposées par Oguchi et Hosoya. Dans la première partie on présente les expressions de la dépolarisation due à une précipitation uniforme. La deuxième partie analyse la distribution statistique de la dépolarisation, d’un plus grand intérêt pour les ingénieurs chargés des télécommunications. La cellule de pluie proposée par Misme et Fimbel est utilisée pour décrire le modèle de pluie sur un trajet. Si la répartition de l’intensité de précipitation est connue en un point, la répartition de la dépolarisation est obtenue en supposant une seule cellule de pluie dans un trajet le long duquel la répartition de la précipitation serait la même qu’en ce point pour un temps d’observation suffisamment long.
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References
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Pontes, M.S. A method to estimate statistics of rain depolarization. Ann. Télécommunic. 32, 372–376 (1977). https://doi.org/10.1007/BF03003481
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DOI: https://doi.org/10.1007/BF03003481