This is an image of Uranus.
Click on image for full size
Image from: NASA
Uranus' Mesosphere
The mesosphere of Uranus is a region of balance between warming and cooling. That essentially means that nothing happens there. Except for
diffusion, the atmosphere is still. Upper reaches of the atmosphere, such as the mesosphere, can sometimes be detected by looking at the limb of a planet, as shown in this image. Unfortunately, nothing of the mesosphere can be seen in this image. For a picture showing how the temperature changes in the mesosphere, click
here.
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This is the temperature profile of Uranus' mesosphere. The temperature is the same at all heights until the mesopause, or "top" of the mesosphere is reached. As shown in the figure, the mesopause is placed
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As on Earth, the atmosphere of Uranus consists of a troposphere, stratosphere, mesosphere, and thermosphere. The troposphere is the region where the visible clouds are to be found. The stratosphere, as
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Besides methane, Uranus' atmosphere contains more sophisticated atmospheric molecules such as ethane gas, acetylene, and diacetylene. All these molecules form layers of haze at different altitudes high
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The mesosphere of Uranus is a region of balance between warming and cooling. That essentially means that nothing happens there. Except for diffusion, the atmosphere is still. Upper reaches of the atmosphere,
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On Uranus, as on Jupiter, the winds in the belts and zones blow first in one direction, then in the opposite direction. Wind blows east in a belt, and west in a zone. The clouds rise up in a belt, and
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The striped cloud bands on Uranus, like Jupiter, are divided into belts and zones. On Uranus the belts and zones are hard to distinquish. The left picture shows the north pole of Uranus. In this picture
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The clouds of Uranus, composed of methane crystals, are found very low in the troposphere, and are difficult to distinquish below the smog haz es of the planet's atmosphere. False color is used, in the
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