Earth's obliquity would vary chaotically from 0 degrees to 85 degrees
were it not for the presence of the Moon (J. Laskar, F. Joutel, and P.
Robutel, 1993, Nature 361, 615-617). The Moon itself is thought to be
an accident of accretion, formed by a glancing blow from a Mars-sized
planetesimal. Hence, planets with similar moons and stable obliquitie
s may be extremely rare. This has lead Laskar and colleagues to sugges
t that the number of Earth-like planets with high obliquities and temp
erate, life-supporting climates may be small. To test this proposition
, we have used an energy-balance climate model to simulate Earth's cli
mate at obliquities up to 90 degrees. We show that Earth's climate wou
ld become regionally severe in such circumstances, with large seasonal
cycles and accompanying temperature extremes on middle-and high-latit
ude continents which might be damaging to many forms of life. The resp
onse of other, hypothetical, Earth-like planets to large obliquity flu
ctuations depends on their land-sea distribution and on their position
within the habitable zone (HZ) around their star. Planets with severa
l modest-sized continents or equatorial supercontinents are more clima
tically stable than those with polar supercontinents. Planets farther
out in the HZ are less affected by high obliquities because their atmo
spheres should accumulate CO2 in response to the carbonate-silicate cy
cle. Dense, CO2-rich atmospheres transport heat very effectively and t
herefore limit the magnitude of both seasonal cycles and latitudinal t
emperature gradients. We conclude that a significant fraction of extra
solar Earth-like planets may still be habitable, even if they are subj
ect to large obliquity fluctuations. (C) 1997 Academic Press.