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
+----------------------------------------------------+
| | Anjarakandy. | Calcutta. |
| Months. |--------------------|-------------------|
| | Rain. | Temp. | Rain. | Temp. |
|-----------|----------|---------|---------|---------|
| | M. M. | | M. M.| |
| January, | 2,26 | 26 deg.,5 | 0,0 | 18 deg.,4 |
| February, | 2,26 | 27 deg.,7 | 67,68 | 21 deg.,5 |
| March, | 6,77 | 28 deg.,4 | 24,82 | 25 deg.,6 |
| April, | 29,33 | 29 deg.,8 | 130,84 | 28 deg.,5 |
| May, | 175,96 | 28 deg.,6 | 16,24 | 29 deg.,7 |
| June, | 794,05 | 26 deg.,6 | 575,24 | 29 deg.,3 |
| July, | 807,59 | 25 deg.,8 | 338,38 | 28, deg.1 |
| August, | 572,98 | 26 deg.,0 | 311,31 | 28 deg.,3 |
| September,| 311,31 | 26 deg.,4 | 254,91 | 28 deg.,0 |
| October, | 157,91 | 26 deg.,8 | 42,86 | 27 deg.,2 |
| November, | 65,42 | 26 deg.,9 | 20,30 | 23 deg.,0 |
| December, | 29,33 | 26 deg.,5 | 0,0 | 19 deg.,2 |
|-----------|----------|---------|---------|---------|
| Year, | 2955,14 | 27 deg.,2 | 1928,74 | 26 deg.,4 |
+----------------------------------------------------+
Anjarakandy is on the Malabar coast, between 12 deg. and 13 deg. north latitude.
Calcutta in an angle of the Bay of Bengal, at 22 deg. 30' north latitude. The
former is in and near the focus of the monsoons, and has a temperature in
July (when 18 inches of rain fall), about as low as in December.
In the foregoing table from Kaemptz, the rain is in millimetres, about
twenty-five of which make an inch, and the temperature is centigrade,
which may be raised to Fahrenheit by adding four fifths of the quantity
and also 32 deg.--thus, if the height of the centigrade thermometer be 25 deg.,
add to this four fifths of 25 deg., which is 20 deg., and also 32 deg., the result is
77 deg.. Twenty-five centigrade is therefore equal to seventy-seven
Fahrenheit.
Lieutenant Maury is not, and should not be a theorist. He occupies the
position, in some sort, of a national _investigator_, and, of course, of
national _instructor_. Opinions which emanate from him, or which are
endorsed by him, should be accurate. Sooner or later that which he has
adopted in relation to the monsoons, and some others, must be abandoned.
In addition to what has already been said, I wish to call his, and the
reader's attention, to several other facts and considerations in relation
to the monsoons, and particularly those of India.
Public-domain text, read in full here on John Shaqi.
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