Showing posts with label ICE FLOWS. Show all posts
Showing posts with label ICE FLOWS. Show all posts

Wednesday, May 14, 2014

NASA SCIENTISTS RETURN FROM ANTARTICA

FROM:  NASA 

NASA aircraft and scientists have returned to the United States after a short ice-surveying mission to Antarctica. Despite having only a week of flying time, the team returned with crucial scientific data and a trove of spectacular aerial photographs.

The flights over Antarctica were part of Operation IceBridge, a multi-year mission to monitor conditions in Antarctica and the Arctic until a new ice-monitoring satellite, ICESat-2, launches in 2016. ICESat-1 was decommissioned in 2009, and IceBridge aircraft have been flying ever since.

Previous Antarctic IceBridge flights took off from Punta Arenas, Chile, but this time NASA’s P-3 took off from the sea ice runway at McMurdo Station, a first for the team. Operated by the National Science Foundation, the station is located on Antarctica’s Ross Island. Flying from McMurdo meant the IceBridge team was able to survey some areas that were unreachable from Chile.

In 43 hours across five science flights in late November, the P-3 collected more than 20,000 kilometers (12,000 miles) worth of science data. Instruments gathered information about the thickness of the ice over subglacial lakes, mountains, coasts, and frozen seas.

Laser altimeter and radar data are the primary products of the mission, but IceBridge project scientist Michael Studinger almost always has his digital camera ready as well. On November 24, 2013, he took the top photograph of a multi-layered lenticular cloud hovering near Mount Discovery, a volcano about 70 kilometers (44 miles) southwest of McMurdo. The Operational Land Imager (OLI) on Landsat 8 captured a wider satellite view (second image) of McMurdo and New Zealand’s nearby Scott Base on November 30, 2013.

Lenticular clouds are a type of wave cloud. They usually form when a layer of air near the surface encounters a topographic barrier, gets pushed upward, and flows over it as a series of atmospheric gravity waves. Lenticular clouds form at the crest of the waves, where the air is coolest and water vapor is most likely to condense into cloud droplets. The bulging sea ice in the foreground is a pressure ridge, which formed when separate ice flows collided and piled up on each other.  Image Credit: Michael Studinger Caption: Adam Voiland.


Tuesday, April 10, 2012

CURRENTS ALONG THE KANCHATKA PENINSULA AS SEEN FROM THE INTERNATIONAL SPACE STATION



FROM:  NASA 
The vantage point from orbit on the International Space Station (ISS) frequently affords astronauts with the opportunity to observe processes that are impossible to see on the ground. The winter season blankets the Kamchatka Peninsula of Russia in snow, but significant amounts of sea ice can also form and collect along the Pacific coastline. As ice floes grind against each other, they produce smaller floes that can be moved by wind and currents.
The irregular southeastern coastline of Kamchatka provokes large, circular eddy currents to spin off from the main southwestward-flowing Kamchatka current. Three such eddies are highlighted by surface ice floe patterns at image center. The patterns are very difficult (and dangerous) to navigate in an ocean vessel. While the floes may look thin and delicate from the ISS vantage point, even the smaller ice chunks are several meters across. White clouds (image top right) are distinguished from the sea ice and snow cover by their high brightness and discontinuous nature.
The Kamchatka Peninsula also hosts many currently and historically active stratovolcanoes. Kliuchevskoi Volcano, the highest in Kamchatka (summit elevation 4,835 meters) and one of the most active, had its most recent confirmed eruption in June 2011. Meanwhile, Karymsky Volcano (to the south) likely produced ash plumes just days before this image was taken; the snow cover on the south and east sides of the summit is darkened by a cover of fresh ash or melted away altogether (image bottom center). By contrast, Kronotsky Volcano—a “textbook” symmetrical cone-shaped stratovolcano—last erupted in 1923.
Astronaut photograph ISS030-E-162344 was acquired on March 15, 2012, with a Nikon D2Xs digital camera using a 28 mm lens, and is provided by the ISS Crew Earth Observations experiment and Image Science & Analysis Laboratory, Johnson Space Center. The image was taken by the Expedition 30 crew. The image has been cropped and enhanced to improve contrast, and lens artifacts have been removed. The International Space Station Program supports the laboratory as part of the ISS National Lab to help astronauts take pictures of Earth that will be of the greatest value to scientists and the public, and to make those images freely available on the Internet. Additional images taken by astronauts and cosmonauts can be viewed at the NASA/JSC Gateway to Astronaut Photography of Earth. Caption by William L. Stefanov, Jacobs/ESCG at NASA-JSC.
Instrument: 
ISS - Digital Camera

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