Results 41 to 50 of about 113,623 (164)
Pitted terrains on (1) Ceres and implications for shallow subsurface volatile distribution
Prior to the arrival of the Dawn spacecraft at Ceres, the dwarf planet was anticipated to be ice‐rich. Searches for morphological features related to ice have been ongoing during Dawn's mission at Ceres.
H. G. Sizemore +20 more
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Ground-Ice Wedges: The Dominant Form of Ground-Ice on the North Coast of Alaska [PDF]
It is a widely known fact that the ground in Arctic and subArctic regions is permanently frozen to a great depth, only the upper few feet thawing in summer. Nearly all observers have reported the presence of bodies of more or less clear ice underlying the surface of the ground, usually immediately below the limit of annual thawing.
openaire +1 more source
Isotopic composition on ground ice in Western Yamal (Marre-Sale)
The profile of Quaternary sediments near Marre-Salle polar station, Western Yamal Peninsula, has large bodies of tabular ground ice. This profile is considered strata-typical and critical in understanding of paleogeographic conditions of the Arctic in ...
I. D. Streletskaya +3 more
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Study region: The Zonag Lake-Yanhu Lake basin on the Qinghai-Tibet Plateau (QTP). Study focus: The melting of ground ice near the permafrost table is an important factor leading to the lake expansion on the QTP.
Shibo Liu +9 more
doaj +1 more source
Dissolved organic carbon (DOC) in Arctic ground ice [PDF]
Thermal permafrost degradation and coastal erosion in the Arctic remobilize substantial amounts of organic carbon (OC) and nutrients which have accumulated in late Pleistocene and Holocene unconsolidated deposits.
M. Fritz +6 more
doaj +1 more source
This Open File presents new national-scale mapping of ground ice conditions in Canada. The mapping depicts a first-order estimate of the combined volumetric percentage of excess ice in the top 5 m of permafrost from segregated, wedge, and relict ice. The estimates for the three ice types are based on modelling by O'Neill et al.
H B O'Neill, S A Wolfe, C Duchesne
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Ice–shelf Grounding: Ice and Bedrock Temperature Changes [PDF]
Abstract Ice rises form where an ice shelf runs aground on the sea bed. After grounding occurs, basal ice temperatures cool from the sea-water temperature towards an equilibrium temperature appropriate to grounded ice. This cooling can take many thousands of years, and much of the delay is due to the thermal inertia of the bedrock ...
Douglas R. MacAyeal, Robert H. Thomas
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Fine-scale maps of ground ice and related surface features are critical for permafrost-related modelling and management. However, such maps are lacking across almost the entire Arctic.
Qianyu Chang +2 more
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Twenty-four buried ice masses remotely mapped in Transantarctic Mountains, Antarctica
Glacial ice contains information on paleoclimate, but typically is less than 1 Myrs old because glaciers continuously flow and melt. A recently discovered buried ice mass in Antarctica is dated to 3-5 Myrs and highlights the potential for long ...
Jaakko Putkonen, Taufique H. Mahmood
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The Ice Factor in Frozen Ground
The nature of ice formations in frozen ground has been a major subject of investigation for Ross Mackay. In this paper, characteristics of the freezing of water in porous materials are reviewed and examples given of the effects of frost action. The thermodynamic basis for the explanation of ice segregation is given and the possible role of spreading ...
openaire +2 more sources

