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languid, and the atmosphere itself is very rare, the general condition of the planet will approximate rather to the lunar type than to the terrestrial, and the extremes, both of heat and cold, will approach those which would prevail on a planet without a regulating atmosphere. There is another way of considering the effect on the climate of Mars and its great distance from the Sun, which, though only rough and crude, may be helpful to some readers. If we take the Earth at noonday at the time of the equinox, then a square yard at the equator


Novelists who write tales of journeys to other worlds or of the inhabitants of other worlds visiting this one, usually assume that the atmosphere is of the same density on all planets, and the action of gravity unchanged. In their view it is only that men would have a little less ground to walk upon on Mars, and a good deal more on Jupiter. Dean Swift, in Gullivers Travels, made the Lilliputians take a truer view of the effect of the alteration of one dimension, for, finding that Gulliver was twelve


than the surface of the Moon—it certainly has for light—so that we may put his effective average temperature, on this supposition, some few degrees above 240 abs., and his equatorial temperature some degrees higher still. It appears as exceedingly probable, then, that whether we regard Mars as like the Earth or, going to the other extreme, as like the Moon, the 87 temperature of his surface is everywhere below the freezing-point of water.14 As the atmospheric circulation on Mars must be


whole planet. If, on the other hand, its atmosphere has no such regulating power, then under the zenith Sun the upper limit of the temperature of a portion of its surface reflecting one-eighth would be, as shown in the Table, 64C. This would imply that the temperature on the dark side of the planet was very nearly at the absolute zero. If we regard Mars as resembling our Moon, and take the Moons effective average temperature as 297 abs., the corresponding temperature for Mars is 240 abs., and the highest temperature is four-fifths of 337 = 270 abs. But the surface of Mars has probably a higher coefficient of absorption


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