Practical Exercises in Elementary MeteorologyWard, Robert DeCourcy
Science
Practical Exercises in Elementary Meteorology
Ward, Robert DeCourcy
Meteorology
From Ft. Smith the line cannot go north or northwest or west, because the
temperatures there are all below 30°. To the south the temperatures are
all above 30°. Evidently there is only one direction in which you can
prolong the line, and that is to the southwest. Temperatures of 30° cannot
be found north of El Paso (28°), because there the temperature distinctly
falls, Santa Fé having 4°, Denver, -14°, and Cheyenne, -23°. Therefore
temperatures _above_ 28° must be found south of El Paso. From Ft. Smith
you may, therefore, continue the 30° line southwest and west, passing
close to El Paso, but to the south of it. In determining the further
course of the 30° line, note that Yuma and all the California stations
have temperatures above 30°, while Winnemucca, Nev., has 13°, and
Portland, Ore., has exactly 30°. From El Paso you may, therefore, continue
the line to the northwest, passing up through Central California parallel
with the coast line, and to the east of all the California stations and of
Roseburg, Ore., and thence running through Portland, Ore., ending just
west of Seattle, Wash. Notice that the 30° line should be nearer to
Sacramento, Cal., with 36°, than to Red Bluff with 44°.
Thus you have drawn the line which passes through all places that have a
temperature of 30° on the map under discussion. This may be called _a line
of equal temperature_. _Isotherm_, a compound of two Greek words meaning
_equal temperature_, is the name given in meteorology to such lines as
this. You have drawn the isotherm of 30°. All parts of the United States
north and east of this line are below 30°, while all districts south and
west of it are above 30°. You see, therefore, how much easier the drawing
of this one line has made the description of the temperature distribution
over the United States.
Carry this process a step further by drawing the line which shall pass
through all places with a temperature of 40°. This line begins at
Jacksonville, Fla. (40°), and runs west, passing between Montgomery, Ala.
(33°), and Pensacola, Fla. (46°). Thence it turns to the northwest,
passing between Vicksburg, Miss. (35°), and New Orleans, La. (48°), and
through Shreveport, La. (40°). From Shreveport it turns to the southwest,
passing to the north and west of Palestine, Tex. (46°), and down through
San Antonio, Tex. (40°). Its further exact location cannot be determined
in Mexico, because there are no observations from Mexican stations, but
the readings at Yuma, Ariz. (41°), and at San Diego (42°), Los Angeles
(44°), San Francisco (45°), Red Bluff (44°), and Cape Mendocino (43°), all
in California, show that the 40° isotherm may be started again just north
of Yuma, and may be carried up through California, nearly parallel with
the Pacific Coast, ending between Cape Mendocino, Cal. (43°), and
Roseburg, Ore. (37°). You have now drawn the isotherms of 30° and of 40°,
and in order to avoid confusion, mark the ends of the first line 30° and
the ends of the second line 40°.
Public-domain text, read in full here on John Shaqi.
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