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Breaching of an ice dam at Qorlortossup tasia, south Greenland
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Sensitivity of subglacial drainage to water supply distribution at the Kongsfjor...
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Sensitivity of subglacial drainage to water supply distribution at the Kongsfjor...
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Sensitivity of subglacial drainage to water supply distribution at the Kongsfjor...
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Recent Evolution of Supraglacial Lakes on ice shelves in Dronning Maud Land, Eas...
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Svalbard impact assessment forcing dataset, version 1 ...
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Severe cloud contamination of MODIS Land Surface Temperatures over an Arctic ice...
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Simulating climatic mass balance, seasonal snow development and associated fresh...
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Meltwater runoff and glacier mass balance in the high Arctic: 1991–2022 simulati...
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The relative age of mountain permafrost — estimation of Holocene permafrost limi...
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A Consistent Framework for Coupling Basal Friction With Subglacial Hydrology on...
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A Consistent Framework for Coupling Basal Friction With Subglacial Hydrology on...
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A Consistent Framework for Coupling Basal Friction With Subglacial Hydrology on...
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A Consistent Framework for Coupling Basal Friction With Subglacial Hydrology on...
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Meteorological conditions on an Arctic ice cap—8 years of automatic weather stat...
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Subglacial permafrost dynamics and erosion inside subglacial channels driven by...
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Subglacial permafrost dynamics and erosion inside subglacial channels driven by...
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Subglacial permafrost dynamics and erosion inside subglacial channels driven by...
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Raw data: Subglacial permafrost dynamics and erosion inside subglacial channels...
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Raw data: Subglacial permafrost dynamics and erosion inside subglacial channels...
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Related Subjects
Svalbard
Arctic
glaciers
snow
[SDE]Environmental Sciences
black carbon
article
ALTITUDE
DATE/TIME
Event label
Snow/ice sample
Verlagsveröffentlichung
Location
Arctic glaciers
Physical Geography
Snow
inorganic ions
mass balance
water isotopes 31
Carbon
Carbon, elemental
Carbon, organic
DEPTH
DEPTH, ice/snow
Earth-Surface Processes
Positioning type/details
Spitzbergen
elemental
glacier mass balance
ice/snow
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