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Artic Home of the Aryans by Lokamanya Bal ... - Mandhata Global

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29<br />

summer and winter would be <strong>the</strong> longest, when <strong>the</strong> eccentricity <strong>of</strong> <strong>the</strong><br />

earth is at its maximum and according as <strong>the</strong> winter and summer<br />

occur at <strong>the</strong> points <strong>of</strong> perihelion or aphelion. It has been found that<br />

this difference is equal to 33 days at <strong>the</strong> highest, and that at <strong>the</strong><br />

present day it is about 7½ days. Thus if <strong>the</strong> winter in <strong>the</strong> nor<strong>the</strong>rn<br />

hemisphere occurs when <strong>the</strong> earth is at P in its orbit and <strong>the</strong><br />

eccentricity is at its maximum, <strong>the</strong> winter will be shorter <strong>by</strong> 33 days<br />

than <strong>the</strong> summer <strong>of</strong> <strong>the</strong> time. But this position will be altered after<br />

10,500 years when <strong>the</strong> winter, occurring at A, will, in its turn, be<br />

longer than <strong>the</strong> corresponding summer <strong>by</strong> <strong>the</strong> same length <strong>of</strong> time,<br />

viz. 33 days.<br />

Now, since <strong>the</strong> earth describes equal areas in equal times in its<br />

orbit, Herschel supposed that in spite <strong>of</strong> <strong>the</strong> difference between <strong>the</strong><br />

duration <strong>of</strong> summer and winter noticed above, <strong>the</strong> whole earth<br />

received equal amount <strong>of</strong> heat while passing from one equinox to<br />

ano<strong>the</strong>r, <strong>the</strong> “inequality in <strong>the</strong> intensities <strong>of</strong> solar radiation in <strong>the</strong> two<br />

intervals being precisely compensated <strong>by</strong> <strong>the</strong> opposite inequality in<br />

<strong>the</strong> duration <strong>of</strong> <strong>the</strong> intervals <strong>the</strong>mselves.” Accepting this statement Dr.<br />

Croll understated his ease to a certain extent. But Sir Robert <strong>Bal</strong>l,<br />

formerly <strong>the</strong> Astronomer Royal <strong>of</strong> Ireland, in his recent work On <strong>the</strong><br />

Cause <strong>of</strong> an Ice Age has demonstrated, <strong>by</strong> ma<strong>the</strong>matical calculation,<br />

that <strong>the</strong> above supposition is erroneous, and that <strong>the</strong> total amount <strong>of</strong><br />

heat received from <strong>the</strong> sun <strong>by</strong> each hemisphere in summer and<br />

winter varies as <strong>the</strong> obliquity <strong>of</strong> <strong>the</strong> earth or <strong>the</strong> inclination <strong>of</strong> its axis<br />

to <strong>the</strong> ecliptic, but is practically independent <strong>of</strong> <strong>the</strong> eccentricity <strong>of</strong> <strong>the</strong><br />

earth’s orbit. Taking <strong>the</strong> total sun-heat received in a year <strong>by</strong> each<br />

hemisphere to be 365 units, or on an average one unit a day, and<br />

taking <strong>the</strong> obliquity to be 23° 27', Sir Robert <strong>Bal</strong>l has calculated that<br />

each hemisphere would receive 229 <strong>of</strong> <strong>the</strong>se heat-units during<br />

summer and only 136 during winter, whatever <strong>the</strong> eccentricity <strong>of</strong> <strong>the</strong><br />

earth may be. But though <strong>the</strong>se figures are not affected <strong>by</strong> <strong>the</strong><br />

eccentricity <strong>of</strong> <strong>the</strong> orbit, yet we have seen that <strong>the</strong> duration <strong>of</strong> <strong>the</strong><br />

summer or winter does vary as <strong>the</strong> eccentricity.

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