Himalayan Journals, vol 2 by J. D. Hooker (great reads TXT) 📖

.367 .375 .375 .376

DECEMBER

No. of

Observations 28 29 28 24 23 23 23 23 23

Hour 8 a.m. 9 10 11 Noon 1 p.m. 2 3 4

Barom.

corrected 23.000 .013 +.018 .009 22.995 .980 .962 .947 -.944

Temp. Air 59.2 60.1 60.8 61.6 62.4 62.7 62.8 62.3 61.8

D.P. 58.1 58.5 59.5 60.0 60.5 60.5 60.4 60.0 59.9

Diff. 1.1 1.6 1.3 1.6 1.9 2.2 2.4 2.3 1.9

Tens. of

Vapour .492 .497 .514 .523 .533 .532 .531 .522 .521

Weight of

Vapour 5.50 5.57 5.77 5.83 5.93 5.92 5.90 5.83 5.82

Humidity .968 .945 .958 .950 .942 .942 .925 .924 .940

Press. of

Dry Air 22.508 .516 .504 .506 .462 .448 .431 .425 -.423

No. of

Observations 19 19 20 21 22 24 24 23

Hour 5 p.m. 6 7 8 9 10 11 M.n.

Barom.

corrected 22.944 .948 .958 .975 .986 +.991 .989 .994

Temp. Air 60.3 59.4 58.7 58.2 57.8 57.4 57.0 56.7

D.P. 58.6 58.4 57.4 57.0 56.6 56.4 55.9 55.4

Diff. 1.7 1.0 1.3 1.2 1.2 1.0 1.1 1.3

Tens. of

Vapour .498 .496 .479 .473 .467 .463 .456 .449

Weight of

Vapour 5.58 5.58 5.60 5.33 5.25 5.23 5.15 5.07

Humidity .940 .968 .960 .962 .960 .968 .962 .927

Press. of

Dry Air .446 .452 .479 .502 .519 .528 .533 +.545

OCTOBER (22 days)

No. of

Observations 11 19 20 20 19 13 15 13 13 14

Hour 6-6.30 a.m. 7 8 9 10 11 Noon 1 p.m. 2 3

Barom.

corrected 23.066 .072 .086 .099 +.100 .079 .072 .055 .033 .027

Temp. Air 54.4 54.3 55.2 56.3 57.1 57.6 57.9 58.0 57.7 57.9

D.P. 52.7 52.3 53.7 54.4 55.5 55.6 56.1 56.4 56.6 56.2

Diff. 1.7 2.0 1.5 1.9 1.6 2.0 1.8 1.6 1.1 1.7

Tens. of

Vapour .4.9 .403 .423 .434 .450 .451 .459 .463 .466 .460

Weight of

Vapour 4.65 4.58 4.78 4.90 5.07 5.08 5.15 5.17 5.25 5.16

Humidity .943 .925 .950 .935 .942 .935 .940 .950 .962 .940

Press. of

Dry Air +22.657 +.669 .663 .665 .650 .628 .613 .592 .567 .567

No. of

Observations 16 13 6 7 3 7 14 18 14

Hour 4 p.m. 5 6 7 8 9 10 11 M.n.

Barom.

corrected 23.024 -.022 .033 .045 .038 .061 +.072 .067 .068

Temp. Air 57.9 56.6 55.9 55.4 53.7 55.1 54.6 54.5 54.1

D.P. 56.1 54.8 54.4 53.8 53.3 54.1 53.0 53.0 52.8

Diff. 1.8 1.8 1.5 1.6 0.4 1.0 1.6 1.5 1.3

Tens. of

Vapour .458 .439 .433 .424 .417 .429 .413 .413 .411

Weight of

Vapour 5.15 4.98 4.90 4.80 4.75 4.83 4.82 4.82 4.65

Humidity .940 .948 .950 .950 .990 .965 .949 .950 .962

Press. of

Dry Air -.566 .583 .600 .621 .621 .632 .659 .654 .657

APPENDIX G.

ON THE RELATIVE HUMIDITY, AND ABSOLUTE AMOUNT OF VAPOUR

CONTAINED IN THE ATMOSPHERE AT DIFFERENT ELEVATIONS IN

THE SIKKIM HIMALAYA.

My observations for temperature and wet-bulb being for the most part desultory, taken at different dates, and under very different

conditions of exposure, etc., it is obvious that those at one station are hardly, if at all, comparative with those of another, and I have therefore selected only such as were taken at the same date and hour with others taken at the Calcutta Observatory, or as can easily be

reduced; which thus afford a standard (however defective in many

respects) for a comparison. I need hardly remind my reader that the vapour-charged wind of Sikkim is the southerly one, which blows over Calcutta; that in its passage northwards to Sikkim in the summer

months, it traverses the heated plains at the foot of the Himalaya, and ascending that range, it discharges the greater part of its

moisture (120 to 140 inches annually) over the outer Himalayan

ranges, at elevations of 4000 to 8000 feet. The cooling effect of the uniform covering of forest on the Sikkim ranges is particularly

favourable to this deposition, but the slope of the mountains being gradual, the ascending currents are not arrested and cooled so

suddenly as in the Khasia mountains, where the discharge is

consequently much greater. The heating of the atmosphere, too, over the dry plains at the foot of the outer range, increases farther its capacity for the retention of vapour, and also tends to render the

rain-fall less sudden and violent than on the Khasia, where the south wind blows over the cool expanse of the Jheels. It will be seen from the following observations, that in Sikkim the relative humidity of the atmosphere remains pretty constantly very high in the summer

months, and at all elevations, except in the rearward valleys; and

even there a humid atmosphere prevails up to 14,000 feet, everywhere within the influence of the snowy mountains. The uniformly high

temperature which prevails throughout the summer, even at elevations of 17,000 and 18,000 feet, is no doubt proximately due to the

evolution of heat during the condensation of these vapours. It will be seen by the pages of my journal, that continued sunshine, and the consequent heating of the soil, is almost unknown during the summer, at any elevation on the outer or southward ranges of Dorjiling: but the sunk thermometer proves that in advancing northward into the

heart of the mountains and ascending, the sun's effect is increased, the temperature of the earth becoming in summer considerably higher than that of the air. With regard to the observations themselves,

they may be depended upon as comparable with those of Calcutta, the instruments having been carefully compared, and the cases of

interpolation being few. The number of observations taken at each

station is recorded in a separate column; where only one is thus

recorded, it is not to be regarded as a single reading, but the mean, of several taken during an hour or longer period. I have rejected all solitary observations, even when accompanied by others at Calcutta; and sundry that were, for obvious reasons, likely to mislead. Where many observations were taken at one place, I have divided them into sets, corresponding to the hours at which alone the Calcutta

temperature and wet-bulb thermometer are recorded,* [Sunrise; 9.50

a.m.; noon; 2.40 p.m.; 4 p.m., and sunset.] in order that

meteorologists may apply them to the solution of other questions

relating to the distribution of heat and moisture. The Dorjiling

observations, and those in the immediate neighbourhood of that

station, appeared to me sufficiently numerous to render it worth

while classing them in months, and keeping them in a series by

themselves. The tensions of vapour are worked from the wet-bulb

readings by Apjohn's formula and tables, corrected for the height of the barometer at the time. The observations, except where otherwise noted, are taken by myself.

SERIES I. Observations made at or near Dorjiling.

JANUARY, 1849

DORJILING

No. of

Obs. Place Elev. Hour