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Comptes Rendus Physique
Volume 17, n° 9
pages 995-1002 (novembre 2016)
Doi : 10.1016/j.crhy.2016.07.017
Scattering properties of a stratified air/snow/sea ice medium. Small slope approximation
Diffusion par un milieu stratifié air/neige/mer glacée. Modèle des faibles pentes

Fig. 1

Fig. 1 : 

Structure with several 2D rough interfaces.

Fig. 2

Fig. 2 : 

Backscattered incoherent intensities for isotropic and uncorrelated interfaces. Left: (hh )-polarization, right: (vv )-polarization.

Fig. 3

Fig. 3 : 

Backscattered incoherent intensities for isotropic/anisotropic/correlated/uncorrelated configurations. Left: (hh )-polarization, right: (vv )-polarization. ϕ =ϕ 0 =0°.

Fig. 4

Fig. 4 : 

Backscattered incoherent intensities in the incidence planes Oxz (ϕ =ϕ 0 =0°) and Oyz (ϕ =ϕ 0 =90°) for anisotropic configurations. Left: (hh )-polarization, right: (vv )-polarization.

Fig. 5

Fig. 5 : 

Incoherent intensities for isotropic/anisotropic/correlated/uncorrelated configurations under normal incidence. Left: (hh )-polarization, right: (vv )-polarization. ϕ =ϕ 0 =0°.

Fig. 6

Fig. 6 : 

Incoherent intensities for anisotropic/uncorrelated configurations under normal incidence in three incidence planes. Left: (hh )-polarization, right: (vv )-polarization.

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