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 or depressions occur. That is why cyclones vary from year to year. The only time when comparisons can be made between one year and the next is when the Moon is at maximum or minimum declination of 18° or 28°, because for about 3 years around these points the Moon’s declination is relatively stationary. Recent stationary years were 1995- 1999(18°) and coming up, 2005-2008(28°) Direction of anticyclones and cyclonics can demonstrate the influence of the Moon. As the Moon travels from east to west, it tries to drag the atmosphere with it. The Moon exerts its pull along its path that has been between the tropics. A band of atmosphere around the Earth’s equator is pulled east to west. But the Earth is rotating west to east underneath it. The lighter and more numerous waterladen-free gases move the easiest. The southern edge of a northern anticyclone and the northern edge of a southern anticyclone, are moving westwards, into the direction of the Moon’s pull, which is why in the Northern Hemisphere anticyclones rotate clockwise, and anticlockwise in the Southern Hemisphere The cyclonics form in the low pressure areas between the ‘gaps’ in the anticyclones. 142
The Barometer In 1638 Galileo noticed that a suction pump used to pull water from a well could not raise water more than 34 feet. His pupil, Torricelli, realised that this was due to the weight of the atmosphere, and confirmed his theory with an experiment. Knowing that mercury is 14 times heavier than water, he realised that if 34 feet of water was held up by the atmosphere in a column(such as a well, or a tube) then an amount of mercury one fourteenth that of water could also be held up. So he took a tube three feet long and filled it with mercury, sealed the end momentarily with his finger, inverted the tube and immersed the end in a bowl of mercury. The health hazards of this were not of course known. The level of mercury in the tube was about 30 inches. The empty space at the top was a vacuum. Watching it and recording over several days, Torricelli discovered that there were variations in the height. Without realising the full implications, he had demonstrated the existence of air pressure and invented the barometer and altimeter. The French scientist Blaise Pascal repeated Torricelli’s experiment, and realised that any air closer to earth would be compressed by the weight of air immedi- 143
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<strong>The</strong> Barometer<br />
In 1638 Galileo noticed that a suction pump used to<br />
pull water from a well could not raise water more than 34<br />
feet. His pupil, Torricelli, realised that this was due to the<br />
weight of the atmosphere, and confirmed his theory with<br />
an experiment. Knowing that mercury is 14 times heavier<br />
than water, he realised that if 34 feet of water was held up<br />
by the atmosphere in a column(such as a well, or a tube)<br />
then an amount of mercury one fourteenth that of water<br />
could also be held up. So he took a tube three feet long<br />
and filled it with mercury, sealed the end momentarily with<br />
his finger, inverted the tube and immersed the end in a bowl<br />
of mercury. <strong>The</strong> health hazards of this were not of course<br />
known. <strong>The</strong> level of mercury in the tube was about 30<br />
inches. <strong>The</strong> empty space at the top was a vacuum. Watching<br />
it and recording over several days, Torricelli discovered<br />
that there were variations in the height. Without realising<br />
the full implications, he had demonstrated the existence<br />
of air pressure and invented the barometer and altimeter.<br />
<strong>The</strong> French scientist Blaise Pascal repeated<br />
Torricelli’s experiment, and realised that any air closer to<br />
earth would be compressed by the weight of air immedi-<br />
143