<h2><SPAN name="CHAPTER_XXI" id="CHAPTER_XXI"></SPAN>CHAPTER XXI.</h2>
<p><SPAN id="question_440"></SPAN>440. <i>What is snow?</i></p>
<p>Snow is <i>congealed vapour</i>, which would have formed <i>rain</i>;
but,
through the coldness of the air, has been <i>frozen</i> in its descent
into <i>crystalline forms</i>. (<SPAN href="#i-053.jpg">Fig. 1</SPAN>.)</p>
<p><SPAN id="question_441"></SPAN>441. <i>Why is snow white?</i></p>
<p>Because it reflects all the component rays of <i>light</i>.</p>
<p><SPAN id="question_442"></SPAN>442. <i>Why is snow said to be warm, while white garments are worn for
coolness?</i></p>
<p>Snow is <i>warm</i> by virtue of its light and woolly texture. But it is
also warm on account of its <i>whiteness</i>;
for, had it been <i>black</i>, it
would have <i>absorbed the heat of the sun</i>, which would have <i>thawed
the snow</i>. Instead of which, it <i>reflects heat</i>;
and the reflected
heat <i>falls upon</i> bodies above the snow, while the <i>warmth of the
earth</i> is preserved <i>beneath it</i>. <i>White clothing is cool</i>, because
it reflects <i>from</i> the body of the wearer the heat of the sun. <i>White
snow</i> is <i>warm</i>, because it <i>reflects the sun's heat upon bodies</i>.</p>
<p class="bq">There are few persons but have felt the effect of the sun's rays
<i>reflected</i> by the white snow on a clear wintry day. And, as
regards the warmth of snow towards the earth, by preventing the
radiation of heat, it has been found that a thermometer buried
four inches deep in snow has shown a temperature of <i>nine degrees</i>
higher than at the surface.</p>
<p><SPAN id="question_443"></SPAN>443. <i>Why are lofty mountains always covered with snow?</i></p>
<p>Because the <i>upper regions</i> of the atmosphere are <i>intensely cold</i>.</p>
<p><SPAN id="question_444"></SPAN>444. <i>Why are the upper regions of the atmosphere intensely cold?</i></p>
<p>Because the <i>atmosphere</i> retains but <i>little of the heat of the
sun's
<span class="pagenum"><SPAN name="Page_106" id="Page_106">[Pg 106]</SPAN></span> rays</i> as they pass to the earth. Because at high altitudes the
air is <i>greatly rarefied</i>. And because the <i>radiation of heat from
the earth</i> does not materially affect such <i>high regions</i>.</p>
<hr class="bible-verse" />
<p class="center bq">"He causeth the vapours to ascend from the ends
of the earth: he maketh lightnings for the rain: he bringeth the wind
out of his treasuries."—<span class="smcap">Ps. xxxv.</span></p>
<hr class="bible-verse" />
<p><SPAN id="question_445"></SPAN>445. <i>What is meant by the snow line?</i></p>
<p>The <i>snow line</i> is the estimated altitude in <i>all countries</i> where
<i>snow would be formed</i>. Even at the equator, at an altitude of 15,000
to 16,000 feet from the level of the sea, snow is found upon the
mountain summits, where it perpetually lies. As we proceed north or
south from the equator the <i>snow line lessens in altitude</i>. Had we in
England a mountain 6,000 feet high, it would be perpetually <i>crowned
with snow</i>.</p>
<p><SPAN id="question_446"></SPAN>446. <i>Why do we hear of red snow?</i></p>
<p>Red snow is the name given to the snow in the arctic regions upon
which a minute vegetable (probably the <i>Protoccus nivalis</i>) grows,
imparting to the snow a red colour. Recent microscopic investigations
have shown it to consist of a minute vegetable cell, which secretes a
red colouring matter.</p>
<p class="bq">Snow is found to be of greater importance to man than is generally
supposed. But, although in this country we are enabled to
recognise the hand of Providence in the gift, there are latitudes
wherein the blessing thus conferred is more deeply felt. In such
countries as Canada, Sweden, and Russia, the falling of snow
is looked for with glad anticipations, quite equalling those
which herald the "harvest-home" of England, or the "vintage" of
France. No sooner is the ground covered with snow, than cranky
old vehicles that had been jolting over rough roads, and sticking
fast in deep ruts of mud, are wheeled aside, and swift sledges
take their place. Towns distant from each other find an easy mode
of communication; the markets are enlivened, and trade thrives.
Snow supplies a kind of railroad, covering the entire face of the
country, and sledges glide over it, almost with the speed of the
locomotive.</p>
<p><SPAN id="question_447"></SPAN>447. <i>What is sleet?</i></p>
<p><i>Sleet</i> is snow which, in falling, has met with a <i>warmer current of
air</i> than that in which it congealed. It therefore partially melts
and forms a kind of <i>wet snow</i>.</p>
<p><SPAN id="question_448"></SPAN>448. <i>What is hail?</i></p>
<p><i>Hail</i> is also the <i>frozen moisture of the clouds</i>. It is probably
formed by <i>rain drops</i> in their descent to the earth, meeting with
an <i>exceedingly cold current of air</i> by which they become <i>suddenly
frozen into hard masses</i>.</p>
<p><span class="pagenum"><SPAN name="Page_107" id="Page_107">[Pg 107]</SPAN></span></p>
<p>It is also supposed that the <i>electrical</i> state of the air and of the
clouds influences the formation of <i>hail</i>.</p>
<hr class="bible-verse" />
<p class="center bq">"If the clouds be full of rain, they shall empty
themselves upon the earth."—<span class="smcap">Eccles. xi.</span></p>
<hr class="bible-verse" />
<p><SPAN id="question_449"></SPAN>449. <i>Why is it supposed that the electrical state of the air and the
clouds affects the formation of hail?</i></p>
<p>Because hail is more common in the <i>summer</i> than at other seasons,
and is frequently attended by storms of <i>thunder and lightning</i>.</p>
<p><SPAN id="question_450"></SPAN>450. <i>Why do hail-storms most frequently occur by day?</i></p>
<p>Because the clouds, being charged with vapour to saturation, favour
the formation of hail by <i>sudden</i> electrical or atmospheric changes.
In the gradual cooling of night, the clouds would expend themselves
in rain.</p>
<p class="bq">Astonishing facts respecting hail-storms are upon record. In 1719
there fell at Kremo, hailstones weighing six pounds. In 1828 there
was a fall of ice at Horsley, in Staffordshire, some of the pieces
of which were three inches long, by one inch broad; and other
solid pieces were about three inches in circumference. Hail storms
are most frequent in June and July, and least frequent in April
and October. Hail clouds float much lower in the sky than other
clouds; their edges are marked by frequent heavy folds; and their
lower edges are streaked with white, the other portions being
massive and black. (<SPAN href="#i-098.jpg">Fig. 10</SPAN>.)</p>
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