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Ultrafast dynamics of melting and ablation at l...
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Ultrafast dynamics of melting and ablation at large laser intensities ab 21.99 € als Taschenbuch: . Aus dem Bereich: Bücher, Wissenschaft, Physik,

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Ultrafast dynamics of melting and ablation at l...
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Ultrafast dynamics of melting and ablation at large laser intensities ab 16.1 € als pdf eBook: . Aus dem Bereich: eBooks, Belletristik, Erzählungen,

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Ultrafast dynamics of melting and ablation at l...
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Ultrafast dynamics of melting and ablation at large laser intensities ab 21.99 EURO

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Ultrafast dynamics of melting and ablation at l...
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Ultrafast dynamics of melting and ablation at large laser intensities ab 16.1 EURO

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Glacier mass balance
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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Crucial to the survival of a glacier is its mass balance, the difference between accumulation and ablation (melting and sublimation). Climate change may cause variations in both temperature and snowfall, causing changes in mass balance. Changes in mass balance control a glacier''s long term behavior and is the most sensitive climate indicator on a glacier. From 1980-2008 the mean cumulative mass loss of glaciers reporting mass balance to the World Glacier Monitoring Service is -12 m. This includes 19 consecutive years of negative mass balances. A glacier with a sustained negative balance is out of equilibrium and will retreat, while one with a sustained positive balance is out of equilibrium and will advance. Glacier retreat results in the loss of the low elevation region of the glacier. Since higher elevations are cooler than lower ones, the disappearance of the lowest portion of the glacier reduces overall ablation, thereby increasing mass balance and potentially reestablishing equilibrium.

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Ferpècle Glacier
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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. The Ferpècle Glacier is a 6.5 km (4.0 mi) long glacier (2005) situated in the Pennine Alps in the canton of Valais in Switzerland. In 1973 it had an area of 9.8 km2 (3.8 sq mi). A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight.

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Greenwell Glacier
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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. The Greenwell Glacier is a major tributary glacier of Antarctica, 72 km long, draining northwest between Mirabito Range and Everett Range to enter Lillie Glacier below Mount Works, in northwest Victoria Land. Mapped by USGS from surveys and U.S. Navy aerial photography, 1960-63. Named by US-ACAN for Cdr. Martin D. Greenwell, USN, Commander of Antarctic Squadron Six (VX-6), 1961-62. A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries.

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Liv Glacier
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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Liv Glacier is a steep valley glacier, 64 km (40 mi) long, emerging from the Antarctic Plateau just southeast of Barnum Peak and draining north through the Queen Maud Mountains to enter Ross Ice Shelf between Mayer Crags and Duncan Mountains. Discovered in 1911 by Roald Amundsen, who named it for the daughter of Fridtjof Nansen.A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries.

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Algie Glacier
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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Algie Glacier (82°8 S 162°5 ECoordinates: 82°8 S 162°5 E) is a 25-mile (40 km) long glacier which flows southeast into Nimrod Glacier just west of the Nash Range of Antarctica. It was named by the New Zealand Ross Sea Committee for R.M. Algie who, as Minister in Charge of Scientific and Industrial Research, gave his strong support to the New Zealand party of the Commonwealth Trans-Antarctic Expedition, 1956 58.A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight.

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