The Great Frozen Sea: A Personal Narrative of the Voyage of the "Alert"Markham, Albert Hastings, Sir
History
The Great Frozen Sea: A Personal Narrative of the Voyage of the "Alert"
Markham, Albert Hastings, Sir
Alert (Sloop : 1856-1895); Arctic regions; Nares, George S. (George Strong), 1831-1915
It was amusing to observe the eager excitement with which every one
received the latest intelligence regarding the state of the thermometer,
and when it was announced that the "lowest on record" had been
registered, there was a general shout of exultation. During the intense
cold several experiments were tried by exposing various substances to
its influence, and with the following results. Glycerine, on which a
temperature of -50° had little effect, became, at -70°, perfectly solid
and quite transparent. Rectified spirits of wine became of the
consistency of hair-oil. Concentrated rum, 40° over-proof, froze hard
when exposed in a shallow vessel like a saucer, but when in a large
quantity it resembled honey or molasses in consistency. Whiskey froze
hard, and we actually broke off bits and ate it! In consequence of this
latter proceeding we have since our return to England been, not without
reason, accused of "hard drinking," an accusation we are, of course,
unable to refute! Chloroform was the only substance on which the low
temperature had no apparent effect. Our temperatures were obtained by
taking the mean of ten thermometers that were exposed, to which result
was applied the corrections from Kew for each instrument. These had been
ascertained when the instruments were tested at the Kew observatory
before leaving England. The corrections and errors of the instruments
could, of course, only be approximately ascertained after the
freezing-point of mercury had been passed, as there was nothing beyond
that with which the spirit could be compared. The slightest impurity of
the spirit used, or the presence of even the most minute portions of
extraneous matter in it, would no doubt seriously affect the accuracy of
the observation. As an instance of the range exhibited by these
instruments, it may be interesting to know that one thermometer
indicated as low a temperature as -82°, while, _at the same time_,
another showed only -60°; but by applying the errors deduced at Kew, the
result was as nearly as possible the same. I think that the minimum
temperature recorded by us was, if not absolutely correct, as nearly so
as it was possible to arrive at.
Although we never again experienced such a severe burst of cold as we
did during the first few days of March, the temperature remained
extraordinarily low, and mercury was in a frozen state during nearly the
whole of that month. The presence of the sun appeared to have little
effect on the temperature, but thermometers exposed to its rays would
frequently rise as high as zero, and sometimes above that point.
The difference of temperature at the summit and at the base of Cairn
Hill, whose height, as has been stated, was four hundred and fifty feet,
was 5½°, the thermometer rising as the hill was ascended, and falling
again as it was brought down.
Public-domain text, read in full here on John Shaqi.
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