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 But then almost to the day (March 26, th to be exact) on another Full Moon day in 1812 there was an Earthquake in exactly the same place; Columbia. That was 187 years ago, which, being 18.6 x 10 is exactly 10 full maximum declination cycles of the Moon, earlier. Maximum declination cycles are described in the next chapter. Let’s look at another Earthquake, this time the gigantic Napier Earthquake in New Zealand, in 1931. Once again, a major quake occurred within a day or two of the northern declination for that month (January). The position of the Moon north or south seems to seriously affect most weather, and the northern or southern declination points are the touchstones. It is not just earthquakes; - thunderstorms, tornadoes, tsunamis, cyclones, hurricanes and floods are all part of the same process of increased gravitational pull. When we looking at a weather map, we want to know the direction of the weather; that is, whether or not an anticyclone(fine weather) that might be sitting north of the country at present, will pass over our country or skip us by. The rules are quite simple. If the Moon is at either its northern or southern monthly declination points, the weather situation will remain as it is for a few days. Mostly, the weather will move at this time along the latitude lines. This situation persists for a couple of days on either side of the declination point. Therefore, if the anticyclone in question is north of us, it will stay north and go slowly from west to east. Winds will be mainly westerlies. 114
Declination But if the Moon is not at either the northern or southern declination points, but is crossing the equator, it drags anticyclones with it in the same direction. So if the anticyclone is north of us and the Moon is travelling between north and south, the anticyclone will be pulled by the Moon down across the country on a diagonal across the latitude lines. On the weather map this will be southwest up to northeast when the Moon is travelling to its northern point and northwest to southeast when the Moon is travelling towards the southern declination point. More frequent and slower moving anticyclones, especially over the South Island of NZ, leads to brief periods of cold southerlies and in winter it leads to increased frostiness. Whether or not anticyclonic or cyclonic systems are generated depends on which way the moon is going. If coming up from the south, the airflow causes anticyclones to be formed to the left and cyclonics to the right. The cyclonics are short-lived, because they are already well to the east. Anticyclones will then typically move over the country. You will get this happening around almost every southern declination. Southern declinations are usually accompanied, in winter, by full moons. Colder weather more often applies around full moons, when the skies are clear overnight and heat gets lost from the day. In the opposite hemisphere, if coming down from the northern dec, the SE airflow would still cause anticyclones to be formed to the left (as viewed from space)and cyclonics to the right. The northern hemisphere would typically get this happening around a northern declination. Northern declinations in the northern hemisphere are usu- 115
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Declination<br />
But if the <strong>Moon</strong> is not at either the northern or southern<br />
declination points, but is crossing the equator, it drags<br />
anticyclones with it in the same direction. So if the anticyclone<br />
is north of us and the <strong>Moon</strong> is travelling between<br />
north and south, the anticyclone will be pulled by the <strong>Moon</strong><br />
down across the country on a diagonal across the latitude<br />
lines. On the weather map this will be southwest up to northeast<br />
when the <strong>Moon</strong> is travelling to its northern point and<br />
northwest to southeast when the <strong>Moon</strong> is travelling towards<br />
the southern declination point.<br />
More frequent and slower moving anticyclones, especially<br />
over the South Island of NZ, leads to brief periods<br />
of cold southerlies and in winter it leads to increased frostiness.<br />
Whether or not anticyclonic or cyclonic systems are<br />
generated depends on which way the moon is going. If coming<br />
up from the south, the airflow causes anticyclones to<br />
be formed to the left and cyclonics to the right. <strong>The</strong><br />
cyclonics are short-lived, because they are already well to<br />
the east. Anticyclones will then typically move over the<br />
country. You will get this happening around almost every<br />
southern declination. Southern declinations are usually accompanied,<br />
in winter, by full moons. Colder weather more<br />
often applies around full moons, when the skies are clear<br />
overnight and heat gets lost from the day.<br />
In the opposite hemisphere, if coming down from the<br />
northern dec, the SE airflow would still cause anticyclones<br />
to be formed to the left (as viewed from space)and<br />
cyclonics to the right. <strong>The</strong> northern hemisphere would typically<br />
get this happening around a northern declination.<br />
Northern declinations in the northern hemisphere are usu-<br />
115