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Predicting Weather By The Moon - Xavier University Libraries

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Declination<br />

month out, year in and year out as the monthly ‘declination<br />

cycle’. It gets complicated, as this cycle itself undergoes<br />

a gradual change.<br />

We can think of it starting around AB. Let’s call that<br />

the low-point. <strong>The</strong> <strong>Moon</strong> wobbles around the Earth all year,<br />

about 13 times. After a year of such monthly declinations,<br />

it has changed slowly, by 1°, either north or south depending<br />

on were it is in the cycle. That means the declination<br />

angle changes 1/13° or 0.08° per month. So after a year it<br />

has risen up into a slightly bigger wobble - still crossing<br />

AB to go underneath, still circling the Earth once per month<br />

with a northern and southern declination and two equatorial<br />

crossings. But its range of movement to the north and<br />

south along the eastern horizon is now slightly more than<br />

it was the previous year.<br />

Suppose BOD is already at low - point, This in angles<br />

is 18° above and below the equator each month(because<br />

the Earth’s tilt is 23° and the <strong>Moon</strong>’s minimum declination<br />

angle is 5° from the ecliptic(actually 5.145396° ). <strong>The</strong> last<br />

time the <strong>Moon</strong> was at its 18° declination point occurred<br />

on 16/3/97. After 9 years, after adding a degree per year,<br />

the new monthly declination is 28° above and below the<br />

equator - the maximum possible monthly declination. <strong>The</strong><br />

last high end was 29/9/87, which is when scientists first<br />

coined the term ‘Greenhouse Effect’. At 1° added per year,<br />

we will reach the upper level again in 22/3/06. 223 declinations<br />

is the whole cycle.<br />

As seen from the centre of the Earth the <strong>Moon</strong> drifts<br />

up and down slightly more than 5° in the course of each<br />

orbit. That’s because the Earth swings a little too, due to<br />

119

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