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(Chris Devlin) #1
18 ASTRONOMY • FEBRUARY 2018

W


ith the focus
on the Moon’s
shadow on the
wane after the
August 2017
total solar eclipse, I’d like to
bring us back to Earth and its
shadow. Some subtle effects of
light and color accompany its
projection onto our planet’s
atmosphere during twilight,
which can be overlooked from
the ground but appear obvious
from the air.

A physiological
wonder
Earth’s shadow is a relatively
brief twilight phenomenon.
Seen against a f lat horizon,
it gradually rises in the east
shortly after sunset. Before
sunrise, you’ll find it setting
in the west. At a glance, the
dark sapphire blue band is
capped by a rose-petal pink
arch known as the Belt of
Venus — a roughly 10°-wide
wedge of reddened sunlight
backscattered to our eyes like
alpine glow. I find it impossible
to discuss the shadow without
the Belt because they meld
together to form a single visual
physiological wonder whose
colors and intensities play off
one another like two thespians
improvising on stage.

SECRETSKY


Earth’s


‘shadow bands’


The near 180° breadth of Earth’s
shadow tends to draw the eye’s
focus along the horizontal
with a peripheral sweep. But
the slight differences you’ll be
searching for — in both inten-
sity and color — are best noticed
with direct vision and scanning
vertically with your eyes.
From the ground under
excellent conditions, Earth’s
shadow generally has a colorful
blue middle with a dull, washed-
out bottom as if someone tried
to scrub the color away. This is
where our eyes look through the
densest and dustiest layer of our
atmosphere. The shadow’s upper
boundary (where it mixes with
the Belt) presents a grape tone,
which brightens into lavender,
followed by cotton candy pink
in the middle, crowned by a
lavender pink hue that diffuses
into the pale sky above.

Up high
As seen from a jet some 35,
feet (10,670 meters) up, Earth’s
shadow stands out much more
boldly, appearing as a deep
purple wedge at its lowest to a
royal blue arch when highest.
Its upper boundary has a crisp
edge. And, because we can
detect our planet’s curvature

BY STEPHEN JAMES O’MEARA

Our planet’s shadow stretches
90° to each side of the antisolar
point (the point in the sky
directly opposite the Sun’s posi-
tion) and tapers northward and
southward. When highest, it
lifts only 6° above the horizon
before it dissolves into the gath-
ering darkness about 35 minutes
after sunset. If only a segment of
sky is visible, the bands appear
deceptively parallel.
Its ill-defined upper bound-
ary transitions into the Belt of
Venus, which is most distinct
when closest to the horizon.
This blending zone becomes
less defined as the shadow
rises. A strong color contrast
occurs when the air is largely
free of contaminants. Dusty
conditions or poor air quality
can erase the shadow from
view. Instead, a muddy gray
band with a dull amber cap
will ring the horizon like a
dusky fog, confusing the view.

Subtleties
Under excellent conditions, the
striking color contrast between
the bluish shadow and the
pinkish Belt of Venus is satis-
faction enough. But if you’d
like to increase your perception,
take time to search for subtle
gradations within the bound-
ary between the two regions.

from that altitude, the shadow’s
slope is dramatically enhanced.
From altitude, the shadow’s
color gradations are deeper and
clearly defined. Moisture in the
upper atmosphere makes the
shadow appear washed out. But
unlike at ground level, it
doesn’t turn dull but bright,
making that part of the shadow
appear whitewashed. The sharp
edge is a deep purple. Above it
is a “raw meat” reddish tone,
followed by orange, yellow, and
a pale salmon that washes into
the blue-white sky above.
Equally fascinating is the
changing color of the terres-
trial landscape below. At times,
the shadow is so intense that
detecting the horizon line takes
effort. The landscape’s color,
which we see through the
densest layers of the atmo-
sphere, mirrors the color of the
sky immediately above it. (See
the three-part sequence below.)
As always, keep your eye on
the sky (day and night) and
let me know your thoughts at
[email protected].

They’re a lot easier to see than
those from a solar eclipse.

BROWSE THE “SECRET SKY” ARCHIVE AT http://www.Astronomy.com/OMeara.

If the sky is clear just after sunset, you’ll see Earth’s shadow rising low in the east.
The pinkish region above it is known as the Belt of Venus. ALL IMAGES: STEPHEN JAMES O’MEARA

Left to right: When Earth’s blue shadow is visible, the landscape is also in shadow and appears blue. About 10 minutes before sunrise, the yellow sky of the east is mirrored in the
west, and the terrestrial landscape is awash with yellow light. At sunrise, the western horizon appears more peach — a color reflected in the air above Earth.

Stephen James O’Meara
is a globe-trotting observer
who is always looking for the
next great celestial event.
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