Infrared emissivity of icy surfaces - Sensitivity to regolith properties and water-ice contaminants

Open Access

Fig. 6

Hemispherical emissivity $ε_{h}^{*} (w_{n})$ $\varepsilon _{\rm{h}}^ * \left( {{w_{\rm{n}}}} \right)$ as a function of average asymmetry factor ξ for a size distribution of gains with a_min = 1 µm , a_max = 5 mm, and p=2 (dashed line) or p=3 (solid line). The grain composition is water ice Ih90 with intra-mixing of 5% AmC. esa diffraction correction is used.

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