| Solarkonstante (W/m2) | 9130 | 2620 | 1370 | 590 | 50,5 | 15,0 | 3,71 | 1,51
|
| Solarkonstante (W/m2) | 6300–14500 | 2580–2650 | 1320–1410 | 490–720 | 46,0–55,8 | 13,5–16,9 | 3,39–4,08 | 1,48–1,54
|
| bolometrische Albedo A | 0,056 | 0,77 | 0,30 | 0,14 | 0,343 | 0,342 | |
|
| Wolkenbedeckung | 0% | 100% | ≈50% | ≈3% | | | |
|
| Sonnentaglänge TSonne (d) | 175,9386 | 116,75 | 1,00000 | 1,02749 | 0,41370 | 0,44402 | 0,71833 | 0,67125
|
| Jahreslänge T
(Tage) | 87,969 | 224,696 | 365,256 | 686,965 | 4332,73 | 10755,5 | 30686,5 | 60190
|
| effektive Temperatur (K) | 400 | 230 | 255 | 216 | 124,4 | 95,0 | 60 | 60
|
| Oberflächendruck (bar) | 10−12 | 95 | 1 | 0,007–0,010 | | | |
|
| Treibhausinkrement (K) | 0 | 507 | 32 | 4 | | | |
|
| Oberflächentemperatur (K) | 100–700 | 737 | 288 | 220 | | | |
|
| Temperaturdifferenz Äquator-Pol (K) | 300 | 5–15 | 45 | 90 | | | |
|
| Adiabatischer Temperaturgradient (K/km) | | 10,5 | 9,8 | 4,5 | | | |
|
| Rossby-Zahl | | 23 | 0,1 | 0,1 | | | |
|
| Chemische Hauptkomponenten | He | CO2 96,5 | N2 78,1 | CO2 95,3 | H2 90 | H2 94 | H2 | H2
|
| (Volumen-%) | | N2 3,5 | O2 20,9 | N2 2,7 | He 9,9 | He 5 | He | He
|
| | | | Ar 0,9 | Ar 1,6 | CH4 0,09 | CH4 0,08 | CH4 | CH4
|
| | | | H2O ≤ 4 | O2 0,1 | NH3 0,02 | NH3 0,02 | NH3 | NH3
|
| Spurenkomponenten | | CO, SO2 | CO2, Ne | CO, H2O | | | |
|
| (≥ 10−7 Volumen-%) | | Ar, H2O | He, CH4 | Ne, Kr | | | |
|
| | | He, COS | Kr, H2 | Xe, O3 | | | |
|
| | | Ne, Kr | N2O, CO | NO | | | |
|
| | | HCl, HF | O3, Xe, HCl | | | | |
|
| Aerosol | | H2SO4 | H2O | H2O | | | |
|
| | | S2 | Salze, Staub | CO2 | | | |
|
| | | NOHSO4 | Organismen | Staub | | | |
|