The Philosophy of the Weather. And a Guide to Its ChangesButler, T. B. (Thomas Belden)
Science
The Philosophy of the Weather. And a Guide to Its Changes
Butler, T. B. (Thomas Belden)
Weather; Weather forecasting
+-------------------------------------------------------+
| Course. | July. | August. | Course. | July. | August. |
|-------------------------------------------------------|
| North. | 32 | 19 | S. S. W.| 9 | 6 |
| N. N. E.| 155 | 125 | S. W. | 3 | 9 |
| N. E. | 144 | 35 | W. S. W.| 13 | 14 |
| E. N. E.| 140 | 89 | West. | 12 | 3 |
| East. | 48 | 57 | W. N. W.| 7 | 7 |
| E. S. E.| 31 | 23 | N. W. | 11 | 1 |
| S. E. | 8 | 7 | N. N. W.| 36 | 6 |
| S. S. E.| 8 | 12 | Calm. | 18 | 12 |
| South. | 5 | 4 |---------|-------|---------|
| | | | Total, | 680 | 429 |
+-------------------------------------------------------+
It would seem to be impossible for any man to believe in the theory of
rarefaction, after an examination of these tables.
Professor Coffin discovers other anomalies, for which he finds it
difficult to account. Among these are the northerly tendency, in the
afternoon, of the winds in Ohio, south of Lake Erie; the winds of
south-western Asia, which, he says, "Are so irregular as to defy all
attempts to reduce them to system;" particularizing the N. W. at
Jerusalem, the westerly at Bagdad, the N. E. at Constantinople, the
northerly at Trebizond, etc., etc. Jerusalem has the Mediterranean at the
N. W., Bagdad has it at the west, Constantinople has the Black Sea at the
N. E., Trebizond N. N. W. and N. E., and the counter-trade, as it passes
over them, draws its storm-surface wind or sea-breeze, from the quarter
where evaporation is greatest, and the atmosphere is most susceptible of
electrical inductive influence. Precisely as it draws from the ocean and
the eastward, east of the Alleghanies, from the lake region, west of the
lakes, and from the northward, south of the lakes, and from the westward,
east of them.
This law of attraction will explain, too, the mean prevalence of easterly
winds north of the parallel of 60 deg., at the stations named in his work.
Great Bear Lake, Great Slave Lake, and Fort Enterprise, lie east of the
Rocky Mountain range which interposes between them and the Pacific, and
have Hudson's Bay and other large bodies of water on the east and north.
Hence, easterly winds prevail at these places. At Norway House, on
Nelson's River, near the north end of Lake Winnipeg, a large body of
water, which stretches off to the south, we find the south wind the
prevalent one, especially in December, when the northern and north-eastern
waters are frozen up, and the N. E. largely present at all seasons of the
year.
Public-domain text, read in full here on John Shaqi.
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