The evolution of climateBrooks, C. E. P. (Charles Ernest Pelham)
Science
The evolution of climate
Brooks, C. E. P. (Charles Ernest Pelham)
Climatology; Paleoclimatology
Draw a circle round the point of angular radius ten degrees (i.e. set
the compass to cover ten degrees of latitude) and divide this into
two halves by a line passing from north to south through the centre.
By means of squared tracing paper, or otherwise, measure: (_a_) the
amount of ice in the whole circle; (_b_) the amount of land in the
western half; (_c_) the amount of land in the eastern half. (_a_) is
expressed as a percentage of the area of the whole circle; (_b_) and
(_c_) as percentages of the area of a semicircle.
The term “ice” includes ice-sheets such as that of Greenland or
Antarctica, and also frozen sea or sea closely covered by pack-ice;
the latter figure may vary in different months.
The temperature in January or July is then calculated from the
following formula:
Temperature = basal temperature + ice coeff. x per cent. of ice +
land west coeff. x per cent. of land to west + land east coeff. x per
cent. of land to east.
The basal temperatures and the appropriate coefficients are given in
the following table.
In calculating the effect of a given slight change of land and sea
distribution, it is not necessary to employ the basal temperature.
Instead the equation can be treated as a differential, and the change
of temperature due to the change of land and ice calculated from the
figures in columns 3 to 5. The figures are given in degrees absolute,
273°0 = 32° F. To convert differences to Fahrenheit, multiply by 1°8.
---------+-------------+----------+-----------+-----------
Latitude.| Basal Temp. |Ice Coeff.| Land, | Land,
|(Water Zone).| |West Coeff.|East Coeff.
---------+-------------+----------+-----------+-----------
Jan. | a. | | |
70 N. | 298.8 | -0.49 | -0.43 | -0.20
60 | 277.4 | -0.07 | -0.31 | -0.01
50 | 276.8 | -0.09 | -0.29 | 0.09
40 | 282.5 | -- | -0.17 | 0.04
30 | 289.6 | -- | -0.08 | 0.03
20 | 294.2 | -- | -0.01 | -0.01
10 | 298.6 | -- | -0.01 | 0.03
0 | 299.3 | -- | 0.01 | 0.00
10 S. | 298.2 | -- | 0.04 | -0.01
20 | 296.2 | -- | 0.07 | 0.00
30 | 293.5 | -- | 0.06 | 0.03
40 | 289.3 | -- | 0.09 | -0.03
| | | |
July. | | | |
70 N. | 279.3 | -0.16 | 0.02 | 0.02
60 | 280.7 | -- | -0.01 | 0.11
50 | 285.8 | -- | 0.04 | 0.06
40 | 291.1 | -- | 0.05 | 0.07
30 | 296.8 | -- | 0.08 | -0.01
20 | 297.6 | -- | 0.07 | 0.02
10 | 298.8 | -- | 0.03 | -0.01
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