Outlines of a mechanical theory of storms : $b containing the true law of lunar influence, with practical instructions to the navigator, to enable him approximately to calculate the coming changes of the wind and weather, for any given day, and for any part of the oceanBassnett, Thomas
Science
Outlines of a mechanical theory of storms : $b containing the true law of lunar influence, with practical instructions to the navigator, to enable him approximately to calculate the coming changes of the wind and weather, for any given day, and for any part of the ocean
Bassnett, Thomas
Weather
The same year, the North Star with additional supplies was working up
Baffin's bay; but on account of the unusual quantities of ice, and the
frosts "which glued the floes together," she was unable to force a
passage through the middle ice, and wintered on the east side of
Baffin's bay, in latitude 76° 33′--her thermometer marking 64° below
zero, as the coldest of the winter. In 1850, the perigee of the moon
attained its northern limit, but the position of the node was bad; still
this year and 1851, were the best of the series. The North Star
succeeded in getting out of the ice on the 1st of August--a very early
date for that high latitude--and on the 8th had crossed over to
Possession bay; but being prevented by the land-ice, she bore up for
Pond bay and there landed the provisions. The same year (1850) several
vessels entered Lancaster sound. Sir John Ross also reached Melville
Island; from which it is evident that this season was far better than
any preceding. According to Captain Penny, this year a floe of ice at
least two years old, filled Wellington strait; but was diminished in
breadth at a subsequent visit. He also saw a boundless open sea from the
_western_ entrance of Wellington strait; but of course the ships could
not reach it, for the floe before mentioned. Following the indications
of the theory, we consider it almost certain that Franklin went to the
westward and not through Wellington channel; that he made but slow
progress until 1850, when finding the sea more open to the northward,
and attributing it more to local influences than to any change in the
season, he considered it a better course to extricate the expedition, by
pushing on towards Behring's straits than to attempt the frozen channels
he had already passed through. But the seasons again getting worse after
1850, he was again arrested in the polar basin by the ice and islands
off the northern coast of America.
Public-domain text, read in full here on John Shaqi.
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