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Science Acrylic Print featuring the photograph Arctic Summer Storm 2012 by Science Source

The watermark in the lower right corner of the image will not appear on the final print.

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Arctic Summer Storm 2012 Acrylic Print

Science Source

by Science Source

$109.00

Product Details

Arctic Summer Storm 2012 acrylic print by Science Source.   Bring your artwork to life with the stylish lines and added depth of an acrylic print. Your image gets printed directly onto the back of a 1/4" thick sheet of clear acrylic. The high gloss of the acrylic sheet complements the rich colors of any image to produce stunning results. Two different mounting options are available, see below.

Design Details

Summer Storm Spins Over Arctic. An unusually strong storm formed off the coast of Alaska on August 5 and tracked into the center of the Arctic Ocean,... more

Ships Within

3 - 4 business days

Additional Products

Arctic Summer Storm 2012 Photograph by Science Source

Photograph

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Acrylic Print Tags

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Photograph Tags

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Artist's Description

Summer Storm Spins Over Arctic. An unusually strong storm formed off the coast of Alaska on August 5 and tracked into the center of the Arctic Ocean, where it slowly dissipated over the next several days. The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA's Aqua satellite captured this natural-color mosaic image on August 6, 2012. The center of the storm at that date was located in the middle of the Arctic Ocean. The storm had an unusually low central pressure area. Paul A. Newman, Chief Scientist for Atmospheric Sciences at NASA Goddard estimates that there have only been about eight storms of similar strength during the month of August in the last 34 years of satellite records. Arctic storms such as this one can have a large impact on the sea ice, causing it to melt rapidly through many mechanisms, such as tearing off large swaths of ice and pushing them to warmer sites, churning the ice and making it slushier, or lifting warmer waters from the depths of the Arctic Oc...

 

$109.00

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