Planet weather
Q: Do other planets have weather? If so, what kind,
what planets? Natalie, Somewhere, USA
Jupiter's
Great Red Spot, a gigantic storm, persisting for hundreds of years. The white
oval storm below the Red Spot has about the same diameter as Earth.
1979. Courtesy of NASA and Wikipedia.
A: Yes, other planets endure such weather that Earth's worst seems
balmy.
All planets, except Mercury, in our solar system have an atmosphere and, therefore, weather.
Mercury is the exception.
"I'm not sure it's fair to describe Mercury as having 'weather'. With
virtually no atmosphere, the planet's temperature change is driven entirely by
the (extremely slow 176-Earth-days from one sunrise to the next) rotation of
the planet beneath the near Sun," says astronomer
Robert Massey of the
Royal Observatory Greenwich in London.
For the rest, let me mention a few weather extremes. Pluto, for instance, turns
into a planet frostball every so often. A red-tinted frost
probably covers Pluto — a
methane-nitrogen-carbon-monoxide frost. Pluto moves in a greatly elongated
orbit about the Sun in 248 years. During the 20 years she is closest to
the Sun, temperatures rise, and ice turns to gas.
Moreover, when Pluto orbits away from the Sun, and the gases freeze, her atmosphere
may collapse, and a planet-wide frost ensues: a
frostball Pluto.
Venus, on the other hand, has a surface
literally hot
enough to melt lead: 860° F (460° C). The closer Sun shines more
intensely on Venus than on Earth, but thick clouds high in the atmosphere
reflect much of the light. The
surface converts the sunlight filtering through the clouds into thermal energy,
which heats the surface, which then emits infrared radiation. The
atmosphere absorbs this infra-red radiation, transforms it again, radiates
mostly in the infrared and heats the surface below, even more.
Furthermore, the enormous amount of carbon dioxide in Venus' extraordinarily thick atmosphere
generates more heating through this atmospheric heating process than on any
other planet in our solar system. That is why Venus is so hot, say
physicist
Craig
Bohren, author of Clouds in a glass of beer, and atmospheric scientist
Peter Pilewskie of the
University of Colorado, Boulder.
Her atmosphere is so thick it exerts a surface pressure
about 90 times Earth's. She's covered with sulphuric-acid clouds whose
tops race across her skies at triple Earth
hurricane speed, while surface zephyrs waft at only a couple of miles an hour.
We've been watching what may be the solar system's longest lasting storm — Jupiter's Great Red Spot — on and off for 340 years, since Cassini
first discovered it in 1665, shortly after Hans Lippershey invented the
telescope in 1608. The high-pressure storm gyrates (in the opposite
direction from low-pressure Earth hurricanes) due to Coriolis effects (just as
on Earth) making a complete rotation every 6 days (2.5 times faster than storms
rotate on Earth).
Click for animation of the swirling storm, courtesy of Wikipedia and the
American Museum of Natural History.
Jupiter's extremely rapid rotation rate (a 10-hour day) helps drive the large
storms, says Massey. For example, consider a point on our equator — Quito, Ecuador. A corresponding point on Juniper's equator whips around 27 times faster
than Quito does.
The windiest spot under the Sun may be Neptune. We've clocked blasts
over 1500 mph (2400 km/h).
Scientists have been making a "big thing" about
the analogies of Titan's weather (Saturn's biggest moon) to Earth's, says
James
F. Kasting of Pennsylvania State
University, Distinguished Professor of Geosciences. It rains
methane on Titan instead of water but otherwise has Earthlike weather processes,
smog, for example. The Sun's ultraviolet light breaks up methane in
Titan's atmosphere, which produces the orange haze: a smog worse than LA's on
its worst day.
If you and I could land on Titan, we would descend through a
colorful nitrogen atmosphere denser than Earth's: a violet outer
layer, next, a thin blue layer, a yellow band, and finally deepening shades of orange
until we settled on her cold (-290° F, -180° C) surface — perhaps a sticky, cold sand made from ice grains. Scattered
clouds would float above in the orange hazy distance.
Martian dust devils can tower to five miles (8
km) above its terrain, dwarfing our half-mile high tornados. Global-wide dust storms can last for several months.
The major factor driving dust storms, says Massey, is the small dust-particle
size. Even Mars' thin atmosphere can lift these tiny motes.
Immense
(1000-miles across) hurricane gyrating just off the Martian
North Pole, 1999. Courtesy of
J. Bell (Cornell), S. Lee (Univ. Colorado), M. Wolff (SSI), et al.,
NASA. Drawing modified by author.
Total darkness shrouds the Martian winter pole,
creating such cold that up to 25% of Mars' atmosphere condenses into
thick slabs of dry ice. When summer comes, the dry ice sublimates, and
generates vast hurricanes.
Unlike Earth, Mars' changing distance from the
Sun affects its seasons, especially in the southern hemisphere. Mars is
closest to the Sun in the southern summer and farthest away in the southern
winter. Consequently the south has more extreme seasons than the north.
"The
very fact that we can see planetary weather is a testament to the technological
advances of the last four centuries. We've moved from seeing planets as bright
dots to being able to see storms brewing on Jupiter, find out which gases
surround Pluto and watch the Martian ice caps sublime. So much of this can even
be seen using telescopes on or near the Earth — although, too often, they just
whet our appetite for further space missions," says Massey.
Planet temperatures, winds and atmosphere
|
|
Planets |
Temperatures (°F) |
Hurricane type winds (mph) |
Atmosphere constituents (%) |
|
Low |
Average |
High |
| Mercury |
-300 |
|
800 |
|
|
hydrogen and helium |
(escapes into space but is constantly replenished) |
| Venus |
|
|
860 |
220 |
96
4 |
carbon dioxide
nitrogen |
|
| Earth |
-130 |
60 |
135 |
75-190 |
78
21 |
nitrogen
oxygen |
|
| Mars |
-170 |
|
32 |
300 |
95
3 |
carbon dioxide
nitrogen |
|
| Jupiter |
-235 |
|
400 |
290-340 |
90
10 |
hydrogen
helium |
|
| Saturn |
|
-310 |
|
1100 |
94
6 |
hydrogen
helium |
|
| Uranus |
|
-350 |
|
90-360 |
83
15
2 |
hydrogen
helium
methane |
|
| Neptune |
|
-350 |
|
1500 |
80
19
1 |
hydrogen
helium
methane |
|
| Pluto |
|
-350 |
|
|
|
nitrogen, methane, and carbon dioxide |
(temporary atmosphere) |
Further Reading:
Planets, Royal Observatory Greenwich
The Weather Centre, planets: BBC
The
Great Red Spot, Wikipedia
Perfect storm on Mars, Hubble space telescope site
Hans
Lippershey, The Galileo Project, Rice University
Titan, Royal Observatory Greenwich
Titan,
Wikipedia
(Answered July 4, 2006; updated Aug. 20, 2007)
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