Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
There are many other interesting optical phenomena connected with
sunrise and sunset, including, first of all, the morning and evening
twilight. When the sun, or any other heavenly body, is only a little
below a clear horizon, it is still visible, on account of the
bending of its rays by the atmosphere. This lifting effect, known
as _astronomical refraction_, amounts to about half a degree (at
the horizon), which is about equivalent to the apparent diameter of
the sun or moon. As the sun sinks farther below the horizon, in the
evening, the only daylight that comes to us is that reflected from
the upper levels of the atmosphere, which are still illuminated. This
is called twilight, and it lasts until the sun is about 18 degrees
below the horizon, when total darkness sets in. The period as a whole
is sometimes called _astronomical twilight_, in distinction from the
briefer period known as _civil twilight_, during which there is light
enough for outdoor occupations; the latter lasts from sunset until the
sun is about 6 degrees below the horizon. Morning twilight is more
commonly called “dawn.”
An interesting succession of light and color effects is observed before
and after sunset and, in inverse position and order, about sunrise.
Considering sunset only: After the sun has sunk out of sight, a broad
band of golden light, called the _bright segment_, is seen along the
western horizon. Above this, in the western sky, appears a more or less
circular expanse of rosy glow, known as the _purple light_. In the
eastern heavens, after sunset, there rises steadily from the horizon
the so-called _dark segment_, which is the blue or ashy shadow of
the earth on the sky. This is bordered above by the pink or purplish
_antitwilight arch_. As time goes on, the purple light in the west,
after increasing in brightness for a while, finally sinks behind the
bright segment; while in the east the rising dark segment encroaches
upon and finally obliterates the antitwilight arch. Sometimes, in clear
weather, there is a fainter repetition of these lights and colors
(_second purple light_, etc.).
Public-domain text, read in full here on John Shaqi.
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