Himalayan Journals — Complete: Or, Notes of a Naturalist in Bengal, the Sikkim and Nepal Himalayas, the Khasia Mountains, etc.Hooker, Joseph Dalton
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Himalayan Journals — Complete: Or, Notes of a Naturalist in Bengal, the Sikkim and Nepal Himalayas, the Khasia Mountains, etc.
Hooker, Joseph Dalton
Himalaya Mountains -- Description and travel; Natural history -- Himalaya Mountains
that my passport was ample, and that I should expect a guide,
provisions, and snow-boots the next day; and that every impediment and
every facility should be reported to the rajah.
[74] A broad ring of this material, agate, or chalcedony, is a mark of
rank here, as amongst the Man-choos, and throughout Central Asia.
During my two days’ stay at Walloong, the weather was bitterly cold: as
heretofore, the nights and mornings were cloudless, but by noon the
whole sky became murky, the highest temperature (50°) occurring at 10
a.m. At this season the prospect from this elevation (10,385 feet), was
dreary in the extreme; and the quantity of snow on the mountains, which
was continually increasing, held out a dismal promise for my chance of
exploring lofty uninhabited regions. All annual and deciduous
vegetation had long past, and the lofty Himalayas are very poor in
mosses and lichens, as compared with the European Alps, and arctic
regions in general. The temperature fluctuated from 22° at sunrise, to
50° at 10 a.m.; the mean being 35°;[75] one night it fell to 64°.
Throughout the day, a south wind blew strong and cold up the valley,
and at sunset was replaced by a keen north blast, searching every
corner, and piercing through tent and blankets. Though the sun’s rays
were hot for an hour or two in the morning, its genial influence was
never felt in the wind. The air was never very dry, the wet-bulb
thermometer standing during the day 3·75° below the dry, thus giving a
mean dew-point of 30·25°. A thermometer sunk two feet stood at 44°,
fully 9° above the mean temperature of the air; one exposed to the
clear sky, stood, during the day, several degrees below the air in
shade, and, at night, from 9° to 14·75° lower. The black-bulb
thermometer, in the sun, rose to 65·75° above the air, indicating
upwards of 90° difference at nearly the warmest part of the day,
between contiguous shaded and sunny exposures. The sky, when cloudless,
was generally a cold blue or steel-grey colour, but at night the stars
were large, and twinkled gloriously. The black-glass photometer
indicated 10·521 inches[76] as the maximum intensity of sunlight; the
temperature of the river close by fell to 32° during the night, and
rose to 37° in the day. In my tent, the temperature fluctuated with the
state of the fire, from 26° at night to 58° when the sun beat on it;
but the only choice was between cold and suffocating smoke.
[75] This gives 1° Fahr. for every 309 feet of elevation, using
contemporaneous observations at Calcutta, and correcting for latitude,
etc.
[76] On three mornings the maxima occurred at between 9 and 10 a.m.
They were, Nov. 24th, 10·509, Nov. 25th, 10·521. On the 25th, at
Tuquoroma, I recorded 10·510. The maximum effect observed at Dorjiling
(7,340 feet) was 10·328, and on the plains of India 10·350. The
maximum I ever recorded was in Yangma valley (15,186 feet), 10·572 at
1 p.m.
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