Mostrando entradas con la etiqueta Ice Sheet. Mostrar todas las entradas
Mostrando entradas con la etiqueta Ice Sheet. Mostrar todas las entradas

jueves, 8 de diciembre de 2016

NASA : Rift in Antarctica's Larsen C Ice Shelf .- Grieta en la plataforma Larsen de hielo en la Antártida...

https://www.nasa.gov/image-feature/rift-in-antarcticas-larsen-c-ice-shelf

Rift in ice shelf photographed from flight overhead
On Nov. 10, 2016, scientists on NASA's IceBridge mission photographed an oblique view of a massive rift in the Antarctic Peninsula's Larsen C ice shelf. Icebridge, an airborne survey of polar ice, completed an eighth consecutive Antarctic deployment on Nov. 18.
Ice shelves are the floating parts of ice streams and glaciers, and they buttress the grounded ice behind them; when ice shelves collapse, the ice behind accelerates toward the ocean, where it then adds to sea level rise. Larsen C neighbors a smaller ice shelf that disintegrated in 2002 after developing a rift similar to the one now growing in Larsen C.
The IceBridge scientists measured the Larsen C fracture to be about 70 miles long, more than 300 feet wide and about a third of a mile deep. The crack completely cuts through the ice shelf but it does not go all the way across it – once it does, it will produce an iceberg roughly the size of the state of Delaware.
The mission of Operation IceBridge is to collect data on changing polar land and sea ice and maintain continuity of measurements between NASA's Ice, Cloud and Land Elevation Satellite (ICESat) missions. The original ICESat mission ended in 2009, and its successor, ICESat-2, is scheduled for launch in 2018. Operation IceBridge, which began in 2009, is currently funded until 2019. The planned overlap with ICESat-2 will help scientists validate the satellite’s measurements.
Image Credit: NASA/John Sonntag
Last Updated: Dec. 2, 2016
Editor: Sarah Loff
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Guillermo Gonzalo Sánchez Achutegui
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viernes, 18 de noviembre de 2016

ESA : Probing Greenland’s ice sheet for future satellites .- Sondar la capa de hielo de Groenlandia para futuros satélites

http://www.esa.int/Our_Activities/Observing_the_Earth/The_Living_Planet_Programme/Campaigns/Probing_Greenland_s_ice_sheet_for_future_satellites

A desolate place to work
 
16 November 2016
With a helicopter the sole feature on the vast expanse of ice and her only way back to warmth and safety, polar scientist Anna Hogg must have thought, “What on Earth am I doing out here?” as she set to taking ice samples.
Anna and fellow scientist Andrew Shepherd, from the University of Leeds in the UK, spent two days extracting long cylindrical ice cores and using instruments to probe the ice sheet as part of an international effort to develop new space technology to monitor our changing polar environment.
Since it was launched in 2010, ESA’s CryoSat has been delivering vital information about how the thickness of Earth’s ice is changing. To do this, the satellite carries a radar altimeter, and now scientists want to find out if an altimeter working at two wavelengths would provide even better information in the future.
 
Monitoring the radar

So, as well as work on the ice, the experiment included taking measurements from an aircraft carrying two radar altimeters: one working at ‘Ka-band’ radio wavelengths less than 1 cm (8 mm) long and the other at ‘Ku-band’ around 2.2 cm.
While Anna and Andrew braved the cold down on the ice sheet, scientists from the Technical University of Denmark and Metasensing operated the complex radar instruments on the plane, focusing their attention on the precious data being collected as they flew back and forth across the ice sheet.
Henriette Skourup, in charge of the airborne measurements, said, “CryoSat relies on a Ku-band radar altimeter to map how the height of the ice caps change over time. Because it has a shorter wavelength, Ka-band penetrates the snow less and therefore provides useful complementary information on ice-sheet topography.
“By comparing airborne and ground data, the campaign will provide valuable feedback on the benefits we expect from Ka-band measurements.”
 
: First Ka-band data

Malcolm Davidson, ESA campaign coordinator, added, “Before any new space technology can be built, a huge effort goes into prototyping the measurements.
“In this case, we need to understand how a two-wavelength radar altimeter could offer continuity and improve the current single-wavelength measurements provided by CryoSat.
“The results from the campaign should help us, together with European space industry, to design future space missions to monitor polar regions.
“Earth’s ice is extremely vulnerable, so it is important that we investigate different ways it could be measured in the future.”
After some well-deserved rest, the campaign team are now busy processing and analysing the data they collected in Greenland and will have the first results before the end of the year.
 
Karen field campaign
ESA
Guillermo Gonzalo Sánchez Achutegui
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martes, 24 de julio de 2012

The Earth: Satellites See Unprecedented Greenland Ice Sheet Surface Melt

Hi My Friends: A VUELO DE UN QUINDE EL BLOG., For several days this month, Greenland's surface ice cover melted over a larger area than at any time in more than 30 years of satellite observations. Nearly the entire ice cover of Greenland, from its thin, low-lying coastal edges to its 2-mile-thick center, experienced some degree of melting at its surface, according to measurements from three independent satellites analyzed by NASA and university scientists
 Extent of surface melt over Greenland’s ice sheet on July 8 (left) and July 12 (right). Measurements from three satellites showed that on July 8, about 40 percent of the ice sheet had undergone thawing at or near the surface. In just a few days, the melting had dramatically accelerated and an estimated 97 percent of the ice sheet surface had thawed by July 12. In the image, the areas classified as “probable melt” (light pink) correspond to those sites where at least one satellite detected surface melting. The areas classified as “melt” (dark pink) correspond to sites where two or three satellites detected surface melting. The satellites are measuring different physical properties at different scales and are passing over Greenland at different times. As a whole, they provide a picture of an extreme melt event about which scientists are very confident. Credit: Nicolo E. DiGirolamo, SSAI/NASA GSFC, and Jesse Allen, NASA Earth Observatory
› Hi-res of left image
› Hi-res of right image

For several days this month, Greenland's surface ice cover melted over a larger area than at any time in more than 30 years of satellite observations. Nearly the entire ice cover of Greenland, from its thin, low-lying coastal edges to its two-mile-thick center, experienced some degree of melting at its surface, according to measurements from three independent satellites analyzed by NASA and university scientists.

On average in the summer, about half of the surface of Greenland's ice sheet naturally melts. At high elevations, most of that melt water quickly refreezes in place. Near the coast, some of the melt water is retained by the ice sheet and the rest is lost to the ocean. But this year the extent of ice melting at or near the surface jumped dramatically. According to satellite data, an estimated 97 percent of the ice sheet surface thawed at some point in mid-July.

Researchers have not yet determined whether this extensive melt event will affect the overall volume of ice loss this summer and contribute to sea level rise.

"The Greenland ice sheet is a vast area with a varied history of change. This event, combined with other natural but uncommon phenomena, such as the large calving event last week on Petermann Glacier, are part of a complex story," said Tom Wagner, NASA's cryosphere program manager in Washington. "Satellite observations are helping us understand how events like these may relate to one another as well as to the broader climate system."

Son Nghiem of NASA's Jet Propulsion Laboratory in Pasadena, Calif., was analyzing radar data from the Indian Space Research Organisation's (ISRO) Oceansat-2 satellite last week when he noticed that most of Greenland appeared to have undergone surface melting on July 12. Nghiem said, "This was so extraordinary that at first I questioned the result: was this real or was it due to a data error?"

Nghiem consulted with Dorothy Hall at NASA's Goddard Space Flight Center in Greenbelt, Md. Hall studies the surface temperature of Greenland using the Moderate-resolution Imaging Spectroradiometer (MODIS) on NASA's Terra and Aqua satellites. She confirmed that MODIS showed unusually high temperatures and that melt was extensive over the ice sheet surface.

Thomas Mote, a climatologist at the University of Georgia, Athens, Ga; and Marco Tedesco of City University of New York also confirmed the melt seen by Oceansat-2 and MODIS with passive-microwave satellite data from the Special Sensor Microwave Imager/Sounder on a U.S. Air Force meteorological satellite.

The melting spread quickly. Melt maps derived from the three satellites showed that on July 8, about 40 percent of the ice sheet's surface had melted. By July 12, 97 percent had melted.

This extreme melt event coincided with an unusually strong ridge of warm air, or a heat dome, over Greenland. The ridge was one of a series that has dominated Greenland's weather since the end of May. "Each successive ridge has been stronger than the previous one," said Mote. This latest heat dome started to move over Greenland on July 8, and then parked itself over the ice sheet about three days later. By July 16, it had begun to dissipate.

Even the area around Summit Station in central Greenland, which at 2 miles above sea level is near the highest point of the ice sheet, showed signs of melting. Such pronounced melting at Summit and across the ice sheet has not occurred since 1889, according to ice cores analyzed by Kaitlin Keegan at Dartmouth College in Hanover, N.H. A National Oceanic and Atmospheric Administration weather station at Summit confirmed air temperatures hovered above or within a degree of freezing for several hours July 11-12.

"Ice cores from Summit show that melting events of this type occur about once every 150 years on average. With the last one happening in 1889, this event is right on time," says Lora Koenig, a Goddard glaciologist and a member of the research team analyzing the satellite data. "But if we continue to observe melting events like this in upcoming years, it will be worrisome."

Nghiem's finding while analyzing Oceansat-2 data was the kind of benefit that NASA and ISRO had hoped to stimulate when they signed an agreement in March 2012 to cooperate on Oceansat-2 by sharing data.
Maria-José Viñas
NASA's Earth Science News Team
Goddard Space Flight Center, Greenbelt, Md.
 Guillermo Gonzalo Sánchez Achutegui
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