Space Pictures This Week: Airglow, Frozen Trees

PanSTARRS’s Northern Debut
Photograph by Babak A. Tafreshi, TWAN
As the distorted crescent moon sets near the horizon, the newly discovered comet PanSTARRS (upper left) makes its first appearance in the Northern Hemisphere on March 12, setting behind the William Herschel Telescope during a cloudy evening in La Palma, California.
The comet, which had grazed through the sky in the Southern Hemisphere for several months, is visible to the naked eye and is said to be brighter than any other comet seen in recent years.
Published March 17, 2013
Running Dry
Image courtesy Robert Simmon, Landsat/USGS/NASA
An image taken in 2006 by the Landsat 5 satellite of Iraq's Qadisiya Reservoir shows the abundance of water in the man-made lake nestled along the Euphrates River.
An image taken three years later reveals the massive depletion of the freshwater reserve—a result of pumping groundwater faster than natural processes can replenish it. Both images were released this week by NASA. (Read: 8 Mighty Rivers Run Dry From Overuse)
Researchers found that between 2003 and 2009, the Tigris and Euprhates river basins lost 117 million acre feet of freshwater, roughly the equivalent to the volume of the Dead Sea. Only one-fifth of the loss was due to natural causes like the shrinking of snowpack and the drying up of soil during the 2007 drought in the Middle East.
"That's enough water to meet the needs of tens of millions to more than a hundred million people in the region each year, depending on regional water-use standards and availability," lead researcher Jay Famiglietti at the University of California, Irvine told NASA.
Published March 17, 2013
Colorful Airglow
Photograph courtesy Yuri Beletsky, ESO
An unusually bright airglow is captured at Las Campanas observatory in La Serena, Chile, by astronomer Yuri Beletsky of the European Southern Observatory.
Airglow is the glowing of the atmosphere, caused by the release of energy from the various atoms, molecules, and ions excited by the sun's ultraviolet rays. Unlike the aurora, which is only visible in high latitudes, airglow can be seen from all over the globe and is brightest at 10 to 15 degrees above the horizon.
While the light emitted is very colorful, as pictured above, airglow appears mostly green and yellow to the unaided eye because the other colors are outside human visible spectrum.
Published March 17, 2013
Asymmetrical Impact Crater
Image courtesy Arizona State University/NASA
Pictured is an asymmetric impact crater found in the moon's Lassell Massiff region, a red spot that astronomers believe harbors pyroclastic, or volcanic, material, speaking to the moon's volcanic history.
Published March 17, 2013
Comets’ Tails
Photograph courtesy G. Brammer, ESO
Two comets, the PanSTARR and the Lemmon, move across the southern sky on March 5, during sunset at the Paranal Observatory in Chile's Atacama desert.
Trailing behind the PanSTARR comet near the horizon is a tail caused by comet dust reflecting sunlight. Above the right slope of the mountain are the glowing green ions of fainter Lemmon comet's tail. Both tails point toward the recently set sun.
And at just the right time in the right place, a shooting star whizzes between the two comets, burning up in the atmosphere.
Published March 17, 2013
Street of Clouds
Image courtesy Jeff Schmaltz, MODIS/NASA
Known as cloud streets, clouds formed over the Davis Strait--between Greenland and Canada in the northern Labrador Sea--during late winter align with the direction of the wind in a parallel pattern.
When the arctic air moves over the warm, open water of the strait, the mix of rising moist air and the temperature difference results in streaks of clouds.
Published March 17, 2013
Riisitunturi Park
Photograph by Bernd Pröschold, TWAN
A vibrant green aurora flashes in the clear night sky behind the "Tykky" sculptures, or "frozen" trees, in Finland's Riisitunturi National Park. The park's forests are especially well known for their snow-covered trees, which appear almost surreal when the moonlight is blue.
During the winter in the Lapland, the most northern region of Finland, snow accumulation ranges from 23 inches (60 centimeters) to more than 35 inches (90 centimeters).
Published March 17, 2013

More »

3 comments

Newest | Oldest

Liam Hosmer

The bright dancing lights of the aurora are actually collisions between electrically charged particles from the sun that enter the earth's atmosphere. The lights are seen above the magnetic poles of the northern and southern hemispheres. They are known as 'Aurora borealis' in the north and 'Aurora australis' in the south..

Auroral displays appear in many colours although pale green and pink are the most common. Shades of red, yellow, green, blue, and violet have been reported. The lights appear in many forms from patches or scattered clouds of light to streamers, arcs, rippling curtains or shooting rays that light up the sky with an eerie glow.