Practical Exercises in Elementary MeteorologyWard, Robert DeCourcy
Science
Practical Exercises in Elementary Meteorology
Ward, Robert DeCourcy
Meteorology
_C._ =The Relation of Local Pressure Changes to Cyclones and Anticyclones,
and thus to Weather Changes.=——Make a detailed study of the relation of
the local pressure changes at your station, as shown by the barograph
curves, or by frequent readings of the mercurial or aneroid barometers, to
the passage of cyclones and anticyclones, and to their accompanying
weather changes. Classify the simple types of pressure change, so far as
possible, together with the general weather conditions that usually
accompany these types. Apply the knowledge of local weather changes thus
gained when you make your forecast on the basis of the daily weather
maps.
CHAPTER XXVI.
METEOROLOGICAL TABLES.
The tables which follow are those which are now in use by the United
States Weather Bureau. They were first published in the _Instructions for
Voluntary Observers_ issued in 1892, and were reprinted in 1897. The
following instructions will be found of service in the use of the
tables:——
TABLE I.——DEW-POINT.
The figures in heavy type, arranged in vertical columns at each side of
the page, are the _air temperatures_ in degrees Fahrenheit, as recorded by
the dry-bulb thermometer. The figures in heavy type, running across the
page, denote the _differences_, in degrees and tenths of degrees, _between
the dry-bulb and wet-bulb readings_, or, technically, the _depression of
the wet-bulb thermometer_. The figures in the vertical columns denote the
_dew-points_. Make your observation of the wet and dry-bulb thermometers
and note the difference between the two readings. Find, in the vertical
columns of heavy type, the temperature corresponding to your dry-bulb
reading, or the nearest temperature to that. Then look along the
horizontal lines of figures in heavy type for the figure which corresponds
exactly, or most nearly, with the difference between your wet and dry-bulb
readings. Look down the vertical column under this latter figure until you
reach the horizontal line corresponding to your dry-bulb reading. At this
point the figures in the vertical column give the dew-point of the air at
the time of your observation.
_Example_: Air Temperature (dry bulb), 47°; Wet Bulb, 44°; Difference, 3°.
On page 148 will be found the table containing both 47° (dry bulb) and 3°
(depression of the dew-point). In the twenty-eighth line of this table and
in the seventh column will be found the dew-point, viz., 41°.
_Example_: Air Temperature, 61.5°; Wet Bulb, 55.5°; Difference, 6°.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account