Abstract
A two-tier Gaussian model for raindrops, which assumes Gaussian distributions both for instantaneous canting angle and time-varying mean canting angle, together with gross features of ice particles, provide a theoretical framework to organize the experimental data and to yield functional dependence of cross-polarization on frequency, polarization and elevation angle. Agreement has been obtained between measured depolarization data and theoretical results which are essentially independent of details of ice clouds. In particular, a linear relation has been found between cross-polarization amplitude and frequency throughout the centimeter wavelengths for a given earth-space path.
Analyse
L’article présente un modèle doublement gaussien montrant l’influence des hydrométéores sur la transpolarisation et qui fournit un cadre théorique aux valeurs mesurées de la transpolarisation et permet de déterminer la transpolarisation en fonction de la fréquence, la polarisation et l’angle de site. Le modèle suppose que l’angle d’inclinaison suit une loi gaussienne dont la moyenne, variable dans le temps, suit elle-même une loi gaussienne; il ne tient compte que des caractéristiques principales des particules de glace. On obtient un bon accord entre la dépolarisation mesurée et les résultats théoriques. On trouve une relation linéaire entre le découplage de polarisation et la fréquence dans la gamme des ondes centimétriques pour un trajet Terre-espace.
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Chu, T.S. Analysis and prediction of cross-polarization on earth-space links. Ann. Télécommun. 36, 140–147 (1981). https://doi.org/10.1007/BF02997017
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DOI: https://doi.org/10.1007/BF02997017
Key words
- Wave propagation
- Wave depolarization
- Centimeter wave
- Satellite communication
- Rain
- Ice
- Statistical model
- Statistical prediction