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Clouds and atmospheric structure

The clouds of Jupiter ( [link] ) are among the most spectacular sights in the solar system, much beloved by makers of science-fiction films. They range in color from white to orange to red to brown, swirling and twisting in a constantly changing kaleidoscope of patterns. Saturn shows similar but much more subdued cloud activity; instead of vivid colors, its clouds have a nearly uniform butterscotch hue ( [link] ).

Jupiter’s colorful clouds.

Jupiter’s Dynamic Clouds. The oranges, reddish browns, taupes and beiges of Jupiter’s dynamic atmosphere are seen swirling around the Great Red Spot in this close-up image of Jupiter.
The vibrant colors of the clouds on Jupiter present a puzzle to astronomers: given the cool temperatures and the composition of nearly 90% hydrogen, the atmosphere should be colorless. One hypothesis suggests that perhaps colorful hydrogen compounds rise from warm areas. The actual colors are a bit more muted, as shown in [link] . (credit: modification of work by Voyager Project, JPL, and NASA)

Different gases freeze at different temperatures. At the temperatures and pressures of the upper atmospheres of Jupiter and Saturn, methane remains a gas, but ammonia can condense and freeze. (Similarly, water vapor condenses high in Earth’s atmosphere to produce clouds of ice crystals.) The primary clouds that we see around these planets, whether from a spacecraft or through a telescope, are composed of frozen ammonia crystals. The ammonia clouds mark the upper edge of the planets’ tropospheres; above that is the stratosphere, the coldest part of the atmosphere. (These layers were initially defined in Earth as a Planet .)

Saturn over five years.

The Changing Angle of Saturn’s Rings. Five images clearly illustrating the 27° tilt of Saturn’s rings. At lower left, the rings are seen nearly edge on, and the Cassini division is difficult to see. Moving toward the upper right, the rings tilt to their maximum angle as seen from Earth, with the planet obscuring only a small portion of the rings.
These beautiful images of Saturn were recorded by the Hubble Space Telescope between 1996 and 2000. Since Saturn is tilted by 27°, we see the orientation of Saturn’s rings around its equator change as the planet moves along its orbit. Note the horizontal bands in the atmosphere. (credit: modification of work by NASA and The Hubble Heritage Team (STScI/AURA))

The diagrams in [link] show the structure and clouds in the atmospheres of all four jovian planets. On both Jupiter and Saturn, the temperature near the cloud tops is about 140 K (only a little cooler than the polar caps of Mars). On Jupiter, this cloud level is at a pressure of about 0.1 bar (one tenth the atmospheric pressure at the surface of Earth), but on Saturn it occurs lower in the atmosphere, at about 1 bar. Because the ammonia clouds lie so much deeper on Saturn, they are more difficult to see, and the overall appearance of the planet is much blander than is Jupiter’s appearance.

Atmospheric structure of the jovian planets.

This plot has four panels, with the vertical axis labeled “Altitude (km)”, ranging from -300 km at the bottom to 200 km at the top in increments of 100 km. The horizontal axis is labeled “Temperature (K)”, ranging from zero at left to 300 at right, in increments of 100 K. The left panel is of Jupiter. A yellow curve showing the variation of temperature with altitude is plotted, and begins at 300 K at -100 km. The curve moves upward to the left and reaches the minimum temperature of 100 K at zero km. The curve then moves to the right, and stops at about 150 K at 150 km. Also plotted are various cloud types and their composition, drawn as irregular blobs. At -100 km “H2O” clouds are plotted, “NH4HS” clouds are plotted at about -50 km, “NH3” clouds are drawn at about -25 km, finally “N2H4(?)” clouds are shown above 100 km. Next is Saturn. A yellow curve showing the variation of temperature with altitude is plotted, and begins at 300 K at -300 km. The curve moves upward to the left and reaches the minimum temperature of about 100 K at zero km. The curve then moves to the right, and stops at about 150 K at 200 km. Also plotted are various cloud types and their composition, drawn as irregular blobs. At -250 km “H2O” clouds are plotted, “NH4HS” clouds are plotted at about -150 km, “NH3” clouds are drawn at about -100 km, finally “P2H4(?)” clouds are shown above 100 km. Next is Uranus. A yellow curve showing the variation of temperature with altitude is plotted, and begins at 150 K at -150 km. The curve moves upward to the left and reaches the minimum temperature of about 50 K at zero km. The curve then moves to the right, and stops at about 100 K at 150 km. Also plotted are various cloud types and their composition, drawn as irregular blobs. At -100 km “H2S?” clouds are plotted, “CH4” clouds are plotted at about -50 km, finally “Hydrocarbon ices” are shown above zero km. Finally, at right, is Neptune. A yellow curve showing the variation of temperature with altitude is plotted, and begins at 280 K at -300 km. The curve moves upward to the left and reaches the minimum temperature of about 50 K at zero km. The curve then moves to the right, and stops at about 80 K at 200 km. Also plotted are various cloud types and their composition, drawn as irregular blobs. At -100 km “H2S?” clouds are plotted, “CH4” clouds are plotted at about -50 km, finally “Hydrocarbon ices” are shown above zero km.
In each diagram, the yellow line shows how the temperature (see the scale on the bottom) changes with altitude (see the scale at the left). The location of the main layers on each planet is also shown.

Within the tropospheres of these planets, the temperature and pressure both increase with depth. Through breaks in the ammonia clouds, we can see tantalizing glimpses of other cloud layers that can form in these deeper regions of the atmosphere—regions that were sampled directly for Jupiter by the Galileo probe that fell into the planet.

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Source:  OpenStax, Astronomy. OpenStax CNX. Apr 12, 2017 Download for free at http://cnx.org/content/col11992/1.13
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