es colder than the
water at the surface, which was then at 45 deg., whilst that of the air was
46 deg.. This experiment in shewing the water to be colder at a great depth
than at the surface, and in proportion to the increase of the descent,
coincides with the observations of Captain Ross and Lieutenant Parry, on
their late voyage to these seas, but is contrary to the results obtained
by Captain Buchan and myself, on our recent voyage to the north, between
Spitzbergen and Greenland, in which sea we invariably found the water
brought from any great depth to be warmer than that at the surface.
On the 28th we tacked, to avoid an extensive stream of sailing ice. The
temperature of the water fell to 39.5 deg.{5}, when we were near it, but was
at 41 deg., when at the distance of half a mile. The thermometer in the air
remained steadily at 40 deg.. Thus the proximity of this ice was not so
decidedly indicated by the decrease of the temperature of either the air
or water, as I have before witnessed, which was probably owing to the
recent arrival of the stream at this point, and its passing at too quick
a rate for the effectual diffusion of its chilling influence beyond a
short distance. Still the decrease in both cases was sufficient to have
given timely warning for a ship's performing any evolution that would
have prevented the coming in contact with it, had the thickness of the
weather precluded a distant view of the danger.
The approach to ice would be more evidently pointed out in the Atlantic,
or wherever the surface is not so continually chilled by the passing and
the melting of ice as in this sea; and I should strongly recommend a
strict hourly attention to the thermometrical state of the water at the
surface, in all parts where ships are exposed to the dangerous
concussion of sailing icebergs, as a principal means of security.
The following day our ship came near another stream of ice, and the
approach to it was indicated by a decrease of the temperature of the
water at the surface from 44 deg. to 42 deg.. A small pine-tree was picked up
much shattered by the ice. In the afternoon of the 30th, a very dense
fog came on; and, about six P.M., when sailing before a fresh breeze, we
were suddenly involved in a heavy stream of ice. Considerable difficulty
was experienced in steering through the narrow channels between the
different masses in this foggy weather, and the ship received several
severe blows.
The water, as
|