|
165 | 165 | # Rayleigh scattering coefficients are anchored to cloudtop altitudes, assumed to be 64 km. |
166 | 166 | # At 64 km, the coefficients are: [ 0.00154417 0.00366592 0.00917735 ] |
167 | 167 | # These are scaled to reach the surface. |
| 168 | + # Fudge factor: 1/π |
168 | 169 | Rayleigh [ 0.0011651 0.002766 0.0069244 ] |
169 | 170 | MieScaleHeight 27 |
170 | 171 |
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|
232 | 233 | # "Rayleigh-scattering calculations for the terrestrial atmosphere" |
233 | 234 | # https://opg.optica.org/ao/abstract.cfm?uri=ao-34-15-2765 [Paywalled] |
234 | 235 | # R = 0.68 μm, G = 0.55 μm, B = 0.44 μm |
235 | | - # Currently, Rayleigh and Mie coefficients are multiplied by a fudge factor to correct appearance. |
| 236 | + # Currently, Rayleigh and Mie coefficients are multiplied by a fudge factor to correct appearance. |
236 | 237 | # Fudge factor: 1/π |
237 | 238 | #Rayleigh [ 0.004847 0.01149 0.02870 ] |
238 | 239 | Rayleigh [ 0.00154 0.00366 0.00914 ] |
|
379 | 380 | { |
380 | 381 | Height 80 |
381 | 382 |
|
382 | | - Rayleigh [ 0.003 0.0022 0.0015 ] |
| 383 | + # Rayleigh coefficients are hand-picked to emulate Martian daytime sky. |
| 384 | + Rayleigh [ 0.002 0.0015 0.001 ] |
383 | 385 | MieScaleHeight 11.1 # Rayleigh scale height |
384 | 386 |
|
385 | 387 | # Schneegans et al. (2024), COMPUTER GRAPHICS forum 43 (2) |
|
390 | 392 | # "Characterisation of Martian dust aerosol phase function from sky radiance measurements by MSL engineering cameras" |
391 | 393 | # https://ui.adsabs.harvard.edu/abs/2019Icar..330...16C/abstract |
392 | 394 | Mie 0.00028 |
393 | | - MieHGAnisotropy 0.76 |
| 395 | + MieHGAnisotropy 0.673 |
394 | 396 |
|
395 | 397 | CloudHeight 30 |
396 | 398 | CloudMap "mars-clouds.*" |
@@ -1094,15 +1096,13 @@ AltSurface "Limit of knowledge" "Sol/Jupiter/Callisto" |
1094 | 1096 | SpecularPower 1000 |
1095 | 1097 | SemiAxes [ 2575.164 2574.720 2574.314 ] |
1096 | 1098 | Mass<kg> 1.345180354e23 |
1097 | | - |
1098 | | - # Scale height is greater than in reality |
1099 | | - # though the value might apply to ground level and not cloud tops |
1100 | | - # reproduces Cassini views at low phase angles |
1101 | | - # the visible scale height at high phase angles seems larger |
1102 | 1099 | Atmosphere |
1103 | 1100 | { |
1104 | 1101 | Height 1000 |
1105 | 1102 |
|
| 1103 | + # Rayleigh coefficient multiplied by fudge factor to correct appearance. |
| 1104 | + # Fudge factor: 1/400 |
| 1105 | + # Scale height is arbitrary, but is larger than in reality. |
1106 | 1106 | Rayleigh [ 0.0000545 0.000129 0.0003218 ] |
1107 | 1107 | MieScaleHeight 150 |
1108 | 1108 |
|
@@ -1703,15 +1703,18 @@ AltSurface "Limit of knowledge" "Sol/Jupiter/Callisto" |
1703 | 1703 | Mass<kg> 2.14029e22 # GM = (1428.49546 ± 0.61603) km^3/s^2 |
1704 | 1704 | Atmosphere |
1705 | 1705 | { |
1706 | | - Height 30 |
| 1706 | + Height 100 |
1707 | 1707 |
|
| 1708 | + # Rayleigh coefficient multiplied by fudge factor to correct appearance. |
| 1709 | + # Fudge factor: 3 |
1708 | 1710 | # Rayleigh scale height and Mie anisotropy from Gao & Ohno (2024) |
1709 | 1711 | # "Clouds and Hazes in the Atmospheres of Triton and Pluto" |
1710 | 1712 | # https://arxiv.org/abs/2411.12031 |
1711 | 1713 | # Mie anisotropy assumed to be the same as discrete component's. |
1712 | 1714 | Rayleigh [ 0.0000016 0.0000037 0.0000093 ] |
1713 | 1715 | MieScaleHeight 16 # Rayleigh scale height |
1714 | 1716 |
|
| 1717 | + # Mie coefficient scaled from Pluto's, using optical depth from Gao & Ohno (2024). |
1715 | 1718 | Mie 0.00000007 |
1716 | 1719 | MieHGAnisotropy 0.6 |
1717 | 1720 | } |
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