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Fig. 1 Upward emission functions used to compute the maps.

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Presentation on theme: "Fig. 1 Upward emission functions used to compute the maps."— Presentation transcript:

1 Fig. 1 Upward emission functions used to compute the maps.
Upward emission functions used to compute the maps. The polar graph shows the three different light intensity distributions used to compute the three map versions: the Lambertian distribution with a peak toward the zenith (map A; blue), the function with peak intensity at low angles above the horizon plane (map B; green), and the function with peak at intermediate angles, 30° above the horizon plane (map C; yellow). The thick red line shows the overall best-fitting function. Fabio Falchi et al. Sci Adv 2016;2:e Copyright © 2016, The Authors

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