by Chris Wayan, 2006
This page lists the physical characteristics of all the model worlds presented in Planetocopia. The home page of each planet or moon has more details than can possibly fit on a single chart, so this page focuses on factors affecting life. In most columns Earth=1.
| NAME | Mass | Diam. | Grav | Temp. | Air pressure | % O2 & avail. O2 | CO2: ppm | Surface area | Water by vol | % Land & Sea, and total land area | Day length | Character | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| EARTH as a benchmark | 1 | 12,750 km | 1 G = 10 m/s, 5 m/s2 | 288 K 15 C 60 F | 1 atm | O2: 20% Avail O2: 1 | CO2 350 ppm | 500 M km2, 196 M mi2 | ca. 109 km3 | 24 hrs | Interglacial. Many sentients; one ape has tech monopoly | ||
| TILT! | |||||||||||||
| SEAPOLE | 1 | 1 | 1 G | 293 K 20 C 68 F | 1 Atm | O2: (20%) | CO2 300 ppm | 1 | 1 | 24 hrs | Sea level up 110 m; mild maritime climate | ||
| SHIVERIA | 1 | 1 | 1 G | 283 K 10 C 50 F | Avg 1 atm but up to 2 in Medit. Abyss | 20% O2, avail O2 2 in Abyss | CO2: 250 ppm | 1 | 1 | 24 hrs | Ice; sea drops 140 m; sapient birds evolve in Mediterranean Abyss | ||
| TURNOVIA | 1 | 1 | 1 G | 288 K 15 C 59 F | 1 atm | O2 20% | CO2 250-300 ppm | 1 | 1 | 24 hrs | green Sahara, dry China, Scandinavian icecap | ||
| JAREDIA | 1 | 1 | 1 G | 286 K 13 C 56 F) | 1 atm | O2 20% | CO2: 300 ppm | 1 | 1 | 24 hrs | Tropical supercontinent, ice-free Antarctica | ||
| FUTURES | |||||||||||||
| DUBIA | 1 | 1 | 1 G | 294 K 21 C 70 F | 1 atm | O2 22% Avail O2 1.1 | CO2: 700 ppm! | 1 | 1 | 24 hrs | Greenhoused! Sea up 110 m; coasts flooded, poles fertile | ||
| MARS REBORN | 0.11 | 0.53 (6800 km) | 0.38 G | 282 K 9 C 48 F | Avg: 0.5 Hellas: 1 Tharsis 0.2 | O2 30%. Avail. O2: avg. 0.7 Hellas 1.5 | CO2 3000 ppm | 0.28 (140 M km2) | 0.05? Ice imports probably unneeded | 24.6 hrs | terraformed; many sentient species | ||
| VENUS UNVEILED | 0.8 | 0.95 (12,100 km) | 0.9 G | 298 K 25 C 77 F | 3.6! | 7.5% O2 avail O2 1.4 | CO2 70 ppm? | 0.9 (450 M km2) | 0.3, all imported ice | 336 hrs (14 days) | terraformed, ring-shielded; dozens of sentient species | ||
| THE BIOSPHERE VARIATIONS | |||||||||||||
| SERRANA | 0.33 | 0.75 (9600 km) | 0.65 G | 292 K 19 C 66 F | 0.67 atm | O2 21% Avail O2 0.7 | CO2: 900 ppm | 0.56 (280 M km2) | 0.07 | 16 hrs | 6-8 sapients, cooperative anarchism | ||
| LYR | 7.0! | 2.2 (29,600 km at equator) | tropics 1.23 G poles 1.4 G | 294 K 21 C 70 F | 6 atm | O2 12% Avail O2 3.5 | CO2: 150 ppm | 5 Earths! (109 km2) | 13 | 12 hrs | Scattered lands in vast world-sea, 19 sapients (mostly fliers) | ||
| OISIN | 0.04 | 0.39 (5000 km) | 0.3 G | 203 K -70 C -94 F (air) | .034 atm | 50% O2 Avail O2 0.1 | CO2: 1200 ppm | 0.15 (77 M km2) | 0.2! Wet, for a tiny moon | 128 hours (5.3 days) | Europa plus light! Abundant sea life under thin ice | ||
| THARN | 0.25 | 0.66 (8300 km) | 0.59 G | trenches 27 C, plains 17 C, uplands 2 C | 0.67 atm | 21% O2 Avail O2: trenches .5 plains .25 uplands 0.1 | CO2: 3000 ppm | 0.43 (216 M km2) | 0.002! Dry! 1/500 of Earth's | 48 hrs | 13 sapients in Earthlike trenches and Martian uplands | ||
| PEGASIA | 0.5 | 0.9 (11,300 km) | 0.63 G | 293 K 20 C 68 F | 1.6 atm | O2 22% Avail O2: 1.76 | CO2: 200 ppm | 0.82 (415 M km2) | 0.25 | 48 hrs | Unknown; invent a species! | ||
| XANADU | 0.06 | 0.48 (6120 km) | 0.26 G | 120 K -153 C -244 F | 2 atm | O2 0.1%. Reducing atmosphere | CO2: 0 ppm | 0.22 (115 M km2) | ethane not water 0.01 | 18 hrs | Cold ecology, ethane not water: a wetter Titan | ||
| CAPRICES | |||||||||||||
| INVERSIA | 1 | 1 | 1 G | 286 K 13 C 55 F | sea basins 1.8 atm, uplands .65 | O2 24% avail O2 2.2 in basins | CO2: 300 ppm | 1 | 0.08 | 24 hrs | Our continents are Inversia's seas | ||
| SIPHONIA | 1 | 1 | 1 G | 289 K 16 C 62 F | Basins 1.6 atm, uplands .7 | O2: 20% | CO2: 350 ppm | 1 | 0.1? | 24 hrs | steamy, rugged abysses, cold ex-continents | ||
| ABYSSIA | 1 | 1 | 1 G | 293 K 20 C 68 F | 1 atm | O2: 22%; avail O2 1.1 | CO2: 300 ppm | 1 | 1 | 24 hrs | low island-continents in coral seas | ||
| SUMMARY | |||||||||||||
| Extremes among the 16 worlds, then the ratio between high & low | Mass: 0.04 to 7.0 Ratio: 180 | Diam.: 0.39 to 2.2 Ratio: 5.64 | Gravity: 0.26 to 1.41 Ratio: 5.4 | Temp: -153 C to 25 C (-244 to 77 F) | Air pressure 0.034 to 6.0 Ratio: 176! | Oxygen: 0 to 24% Avail O2: 0 to 3.5 | CO2: 70 to 3000 ppm Ratio: 43 | Area: 0.15 to 5 Ratio: 33.3 | Water: 0.002 to 13 Ratio: 6500! | Land: 4.5-94% Ratio: 22 Land area: 0.2-2.25 earths Ratio 11.25 | Day: 12 to 336 hrs Ratio: 28 | Wide ranges of wet/dry, air pressure, mass. Gravity and temp narrower. No truly hot world! | |
A table like this is poetry to nerds like me. Well, more than poetry. Striptease! The illustrated web tours are like a floral-print dress; here are the naked numbers underneath. And I'm as shy about them as I am of my naked skin. Be gentle on me, O my Nerdish people! These figures are inevitably rough.
Particularly problematic are the many factors contributing to average temperature: insolation (solar output and mean distance), albedo (amount of sun absorbed: affected by the different reflectivity of clouds, bare rock, water, ice), and greenhouse effects (air pressure and content, especially methane, water vapor and CO2).
And "average worldwide temperature" can be deceptive. Some worlds have wide temperature spreads that the average conceals; a few are sharply two-tier (Inversia, Serrana, Siphonia) or even three-tier (Tharn). But the chart reveals one definite hole: I need to try a hot world. Blisteria?
One apparent inconsistency isn't. CO2 levels don't always correlate with the strength of the greenhouse effect. If it looks like an error, check the total air pressure! 3,000 ppm of nothing much is still nothing much. Another culprit is insolation (solar energy), not listed above; several high-CO2 worlds are fairly far from their suns, preventing a runaway greenhouse effect: less sunlight to trap.
Though the problems don't show on this chart, I have geographic doubts, too. As I've studied better maps of Earth's sea floor and learned how rugged it is (and how most atlases smooth it out) I've come to doubt my drier worlds have enough volcanoes on their basaltic plains. Worlds with extensive shallow seas, like Pegasia, should be richer in islands; those with wide dry plains, like Serrana and Tharn, should have more rain-catching, freestanding peaks and ranges. I over-relied on Venus's picture: many vents, but few high peaks. But Venus is so hot, the rock's more elastic and lava's slow to cool; so most volcanoes are broad and low. On my much cooler worlds, it ain't necessarily so. Rather than go back and alter the earlier worlds, Siphonia (under construction) will show Earth's true undersea complexity.
I'm contemplating more Biosphere Variations, but they're still just ideas: