Donald
F. Collins
Warren Wilson College
This
image was photographed soon after sunset on Dec. 31, 2003 looking
away from the sun at 5:39 pm from the author's home near Asheville,
NC. The sky was extremely clear all day. The dark rays are shadows
caused by mountain peaks or clouds in the distance behind the camera.
The shadows
are parallel, but they appear to converge just above the “Four
Brothers” mountain in the foreground. The convergence of the
parallel rays is analogous to the convergence of parallel railroad
tracks in the distance. Extensive image processing was performed to
enhance the contrast of the shadows.
The
image at right is the sun rising on the summer solstice (June 21,
2002) photographed from the same location. Notice that the sun rises
from the second knob from the left of the “Four Brothers”
mountain. This is the same location at which the sunset shadows in
the top picture converge. The sunset shadows was photographed very
close to the winter solstice. The winter solstice sunset is
diametrically opposite the summer solstice sunrise.
Below
is another
photograph of "anti-crepuscular" rays. This was photographed soon
after sunrise on Jan. 12, 2004 looking west with the sun having
just risen in the southeast behind the camera. The shadows in the
sky are produced by clouds to the left of the photo.
Keep posted for more atmospheric and
astronomical phenomena.