Page:The Cornhill magazine (Volume 1).djvu/118

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the blocks of ice. We must now, therefore, be content with an hour or two's tramp alongside, or on our snow-covered deck under housing; and, during the remainder of the day, we sit below in our little cabin, which has now crystallized by the breath condensing and freezing on the bulkheads, and we endeavour to read and talk away the time. But our subjects of conversation are miserably worn out; our stories are old and oft-repeated; we start impossible theories, and we bet upon the results of our new observations as to our progress, as we unconsciously drift and drift before the gale. At night we retire to our beds, thankful that another day has passed; a deathlike stillness reigns around, broken only by the ravings of some sleep-talker, the tramp of the watch upon deck, a passing bear causing a general rousing of our dogs, or a simultaneous rush of these poor ravenous creatures at our cherished stores of seal-beef in the shrouds; and, as we listen to the distant groaning and sighing of the ice, we thank God that we have still a home in these terrible wastes.

December 28.—During Divine service yesterday, the wind increased, and towards the afternoon we had a gale from the north-westward, attended with an unusual rise of temperature; to-day the gale continues, with a warm wind from the N.N.W.

"The Danish settlers at Upernavik, in North Greenland, are at times startled by a similar sudden rise of temperature. During the depth of winter, when all nature has been long frozen, and the sound of falling water almost forgotten, rain will fall in torrents; and as rain in such a climate is attended with every discomfort, this is looked upon as a most unwelcome phenomenon. It is called the Warm South-east Wind. Now, if the Greenlanders at Upernavik are astonished at a warm South-east Wind, how much rather must the seamen, frozen up in the pack, be astonished at a warm North-west Wind. Various theories have been started to account for this phenomenon; but it appears most probable that a rotatory gale passes over the place, and that the rise in temperature is due to the direction from which the whole mass of air may come, viz. from the southward, and not to the direction of wind at the time."

Let us now return to the narrative, for our days were now becoming mere repetitions of each other. We saw no change, nor did we hope for any until the spring. Gale followed gale; and an occasional alarm of a disruption in the ice, a bear or seal hunt, formed our only excitement; indeed, we sometimes hoped for some crisis, were it only to break the dreadful monotony of our lives. Our walks abroad afforded us no recreation; on the contrary, it was really a trying task to spin out the time necessary for exercise. Talk of a dull turnpike-road at home! Are not the larks singing and the farm boys whistling? But with us what a contrast! Our walks were without an object; one had literally nothing to see or hear; turn north, south, east, or west, still snow and hummocks. You see a little black mark waving in the air: walk to it—it is a crack in a hummock. You think a berg is close to you; go to it—still a hummock, refracted through the gloom. The only thing to do is to walk to windward, so as