Predicting Weather By The Moon - Xavier University Libraries
Predicting Weather By The Moon - Xavier University Libraries Predicting Weather By The Moon - Xavier University Libraries
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
- Page 1 and 2: FREE PDF BOOK The Original PREDICTI
- Page 3 and 4: Despite requests to desist, this pr
- Page 5 and 6: Contents THE FORMATION OF THE MOON
- Page 7 and 8: LOOKING DIRECTLY AT THE MOON ......
- Page 9 and 10: Formation of the Moon OTHELLO: ‘I
- Page 11: Formation of the Moon day as the Lu
- Page 15 and 16: Formation of the Moon tennis ball.
- Page 17 and 18: Formation of the Moon so, then the
- Page 19 and 20: The Moon in Ancient History Mesopot
- Page 21 and 22: The Moon in Ancient History Indo-Eu
- Page 23 and 24: The Moon in Ancient History could i
- Page 25 and 26: The Moon in Ancient History the 28
- Page 27 and 28: The Moon in Ancient History is usua
- Page 29 and 30: The Moon in Ancient History To the
- Page 31 and 32: The Moon in Ancient History land to
- Page 33 and 34: The Moon in Ancient History Charles
- Page 35 and 36: The Moon in Ancient History strual
- Page 37 and 38: Early Moon Watchers lore was Aristo
- Page 39 and 40: Early Moon Watchers And as Bartolom
- Page 41 and 42: Early Moon Watchers inhabitants of
- Page 43 and 44: Early Moon Watchers Diana...Diana..
- Page 45 and 46: Planting by the Moon Moon, her char
- Page 47 and 48: 1 Whiro 2 Tirea 3 Hoata 4 Oue 5 Oko
- Page 49 and 50: Maori and the Moon Seven Sisters. T
- Page 51 and 52: MADNESS, ILL-WINDS, AND THE MOON On
- Page 53 and 54: Madness and the Moon it is conceiva
- Page 55 and 56: Madness and the Moon erly wind in s
- Page 57 and 58: Madness and the Moon 6.00pm news. R
- Page 59 and 60: Madness and the Moon is as predicta
- Page 61 and 62: ible and where to look. This applie
<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