Northern spring is the best time to spot one of the
loveliest sights in the heavens: Earthlight reflected from the
April 12, 2002: It was just before dawn one morning not long ago when I was driving down a twisty mountain road. The yellow middle line was swishing back and forth like a cat's tail: it took plenty of concentration to follow the curves.
That's when it happened.
I spotted something over the ridge that took away my breath -- and my attention. The next thing I knew, I was screeching to a stop at the margin, no longer sleepy.
I had seen Earthshine.
Above: At dusk, a thin crescent moon with Earthshine shines romantically over the Cabrillo Lighthouse on San Diego's Pt. Loma. Credit: Dennis Mammana.
Rising before the Sun that day was an exquisite crescent Moon with the bright planet Venus nearby. The Moon was a whopper, swollen by the well-known illusion that makes moons near the horizon seem big. But that wasn't what grabbed my attention. The wonderful thing was the way the "dark" part of the Moon was faintly glowing.
The view from the Moon itself must be stunning. When the Moon is new, or nearly so, Earth is a dazzling, fully-lit orb in lunar skies. Blue and green and swirling white, our planet would appear four times wider than the Sun and 50 times brighter than a Full Moon.
I envy future astronauts who visit the Moon and stay long enough for sunset.
Right: Leonardo Da Vinci made this sketch of the crescent Moon with Earthshine. It's part of the Codex Leicester, written by Da Vinci between 1506 and 1510. [more]
Phil Goode of Big Bear Solar Observatory is principal investigator of Project Earthshine, a NASA-supported effort to monitor Earth's albedo (the astronomer's term for reflectivity). He says, "it's not surprising that Earth's albedo changes with the seasons." After all, most of the sunlight reflected from our planet is reflected from clouds -- and cloud cover changes from one season to the next.
Clouds dominate the "shininess" of our planet, adds Goode. "They reflect about 50% of the sunlight that hits them -- more than oceans (10%) or land (10% to 25%). Only snow and ice reflect more (40% to 90%) than clouds do, but snowy areas tend to be cloud covered anyway."
Left: A Project Earthshine study of Earth's albedo revealed peaks during northern spring. From "Earthshine Observations of the Earth's Reflectance," by Goode et al, Geophysical Research Letters, Vol. 28, no. 9 (May 1, 2001), pages 1,671-1,674.
There are faster changes, too: As our planet rotates, different parts of it turn to face the Moon. To a lunar astronaut, the Pacific Ocean would appear relatively dark -- like a maria on the Moon itself. On the other hand, a big cloud-covered continent like Asia could reflect two or three times more sunlight than Pacific waters. For this reason the Moon's ashen glow can wax and wane from hour to hour -- "at the 5% level," says Goode.
Look for the changes. Enjoy the glow. Just don't gawk and drive.
Project Earthshine -- To make a systematic determination of Earth's albedo, a ground based earthshine observing project, supported by NASA, was begun at Big Bear Solar Observatory in the summer of 1998
Earthshine: Moon illuminates climate study (PhysicsWeb); Scientists Watch Dark Side of the Moon to Monitor Earth's Climate (AGU)
Leonardo Da Vinci's explanation of Earthshine -- (American Museum of Natural History) The Codex Leicester, written between 1506 and 1510, opens a window onto the mind of the awe-inspiring Renaissance artist.
Our planet's average albedo in recent years is 0.297 plus or minus 0.005 according to Project Earthshine researchers. For more information see "Earthshine Observations of the Earth's Reflectance," by Goode et al, Geophysical Research Letters, Vol. 28, no. 9 (May 1, 2001), pages 1,671-1,674.
Right: Clouds are among the brightest things on planet Earth. [more]
The Inconstant Moon -- an invaluable guide to Earth's moon.
Patterns in the Sky -- (Salisbury State University) This astronomy lecture by Dr. Joseph W. Howard includes diagrams of Moon phases and explains the basics of Earthshine.
Albedo and Earth's Energy Budget: Solar Radiation Primer (NISDC); What Factors Impact a Greenhouse (UCAR); Natural impacts on the climate system (University of New Mexico); Seasonal Variations of Cloud and Surface Properties (NASA's ISCCP); Clouds and Radiation (NASA); Cirrus Clouds and Climate (NASA); Clouds and the Energy Cycle (NASA)
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