Predicting Weather By The Moon - Xavier University Libraries

Predicting Weather By The Moon - Xavier University Libraries Predicting Weather By The Moon - Xavier University Libraries

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Weather By The Moon to run lunar-based factories. The Moon has a crust, about 60-150 km thick. The interior composition of a moon can be guessed from density measurements, and also determined more exactly from spacecraft navigation data when a spacecraft passes by or goes into orbit around a planet or moon. The density of iron is about 5 g/cm3. The density of silicate rock is about 3 g/cm3. The density of the Earth’s Moon is about 3.3 . This density is close to that of silicate rock, suggesting that the Moon has a large mantle made mostly of rock. Has the Moon an atmosphere? In decades past it was accepted that moons such as the Earth’s moon or the moons of Jupiter were airless bodies with no atmosphere whatsoever. Now, however, measurements have shown that most of these moons, including our own, are surrounded by a thin atmospheric region of molecules. The atmosphere may come from the release of gases such as nitrogen and carbon dioxide and carbon monoxide, and radon, which originate deep within the Moon’s interior. Another source are molecules which are loosened from the surface by bombardment of the surface by other molecules from space. These molecules may migrate across the surface of the Moon, to colder regions where they recondense into the ground, or they may fly off into space. This mechanism is a source of water and helium. Was there ever lunar water and if so does some still lie under the Moon’s poles? For once it was believed that the Moon contained 12

Formation of the Moon no water. Moon rocks collected by Apollo astronauts (at lunar equatorial regions) contained no water traces. Lunar mapping performed by the orbiting Galileo spacecraft at coarse resolution, also found no vestige of water. But the more recent Clementine mission made measurements which do suggest that small, frozen pockets of water ice may be embedded in shadowed regions of the lunar crust. Although the pockets are thought to be small, the overall amount of water might be quite significant. This water may come from comets which may continually bombard the Moon, or water in the form of molecules which migrate to the coldest regions of the Moon where they refreeze on the surface, trapped inside enormous craters -some 1,400 miles (2,240 km) across and nearly 8 miles (13 km) deep - at the lunar poles. Due to the very slight tilt of the Moon’s axis, only 1.5 degrees, some of these deep craters never receive any light from the Sun - they are permanently shadowed. This means that the frozen water must remain there, otherwise energy from sunlight would split much of this water into its constituent elements hydrogen and oxygen, both of which would fly off into space immediately. HOW LARGE AND FAR IS IT? The Moon is unusually large. Its diameter is 2,163 miles, compared to 7,927 miles for the mean diameter of Earth. The Earth is three and a half to four times bigger than the Moon and 81 times as massive(as heavy) as the Moon. For our solar system this is an extremely high ra- 13

<strong>Weather</strong> <strong>By</strong> <strong>The</strong> <strong>Moon</strong><br />

to run lunar-based factories.<br />

<strong>The</strong> <strong>Moon</strong> has a crust, about 60-150 km thick. <strong>The</strong><br />

interior composition of a moon can be guessed from density<br />

measurements, and also determined more exactly from<br />

spacecraft navigation data when a spacecraft passes by or<br />

goes into orbit around a planet or moon. <strong>The</strong> density of<br />

iron is about 5 g/cm3. <strong>The</strong> density of silicate rock is about<br />

3 g/cm3. <strong>The</strong> density of the Earth’s <strong>Moon</strong> is about 3.3 .<br />

This density is close to that of silicate rock, suggesting<br />

that the <strong>Moon</strong> has a large mantle made mostly of rock.<br />

Has the <strong>Moon</strong> an atmosphere? In decades past it<br />

was accepted that moons such as the Earth’s moon or the<br />

moons of Jupiter were airless bodies with no atmosphere<br />

whatsoever. Now, however, measurements have shown that<br />

most of these moons, including our own, are surrounded<br />

by a thin atmospheric region of molecules.<br />

<strong>The</strong> atmosphere may come from the release of gases<br />

such as nitrogen and carbon dioxide and carbon monoxide,<br />

and radon, which originate deep within the <strong>Moon</strong>’s interior.<br />

Another source are molecules which are loosened<br />

from the surface by bombardment of the surface by other<br />

molecules from space. <strong>The</strong>se molecules may migrate<br />

across the surface of the <strong>Moon</strong>, to colder regions where<br />

they recondense into the ground, or they may fly off into<br />

space. This mechanism is a source of water and helium.<br />

Was there ever lunar water and if so does some still lie<br />

under the <strong>Moon</strong>’s poles?<br />

For once it was believed that the <strong>Moon</strong> contained<br />

12

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