Introductory Meteorology

Cover Introductory Meteorology
Introductory Meteorology
United States. Weather Bureau. [from Old Catalog]
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For example, in the winter season, there is on the average an inver- sion layer, i. e., one in which the temperature increases with altitude, at Drexel extending to the 1500 meter level. This is due to the fact that this station has a typical continental climate and is, more- over, in the path of the greater number of strong anticyclones, which as before stated are characterized by extreme cold at the surface and in general by an inversion above it. At Mount Weather, Blue Hill and in Europe the
... winter gradient is positive, but very small. In Digitized by Google ATMOSPHERIC TEMPERATURE. 39 the other seasons the gradients are much steeper at all places. For the year the mean value from the surface to the 5 kilometer level is approximately 0.5° C. per 100 meters, or about half the adiabatic TEMPERATURE. *€.
-20 -18 -16 -14 -12 -10 -8-6-4-2 2 4 6 8 10 12 14 16 18 20 22 24 26 8.0 50 4 8 4 8 4 6 4 6 4 4 4 4 42 42 40 40 38 38 36 36 3 4 3 4 32 32 /30 30 S, g26 26Q ^ £4 2 4 t ^22 iii 20 2 ^18 16 16 1.4 14 12 12 10 1.0 A 8 6 6 .4 * .2 2 TEMPERATURE.


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