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Quantitative Mineralogy for 34 sediment samples from various circum-Arctic re...
Quantitative mineralogy was determined using the RockJock program (USGS, 2003). United States Geological Survey (USGS) 2003. User's Guide to RockJock -- A Program for... -
X-ray diffraction (XRD) raw patterns for 34 sediment samples from various cir...
Samples processed with the following steps: 1 gram of the <45 µm sample is mixed with 0.25 grams of powdered, 99.9% pure corundum which serves as an internal standard. This... -
Stable water isotope record from block profiles Chli-Titlis_Profile3
This dataset has no description
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Stable water isotope record from block profiles Chli-Titlis_Profile2
This dataset has no description
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Stable water isotope record from block profiles Chli-Titlis_Profile1
This dataset has no description
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Crystal c-axes (fabric analyser G50) of basal ice samples from Chli Titlis, S...
This dataset has no description
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Large Area Scan Macroscope images of basal ice samples from Chli Titlis, Swit...
This dataset has no description
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Ice and snow thicknesses and water column depth at ten locations in Polar Fox...
This dataset has no description
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Thickness and properties of sea ice and snow of land-fast sea ice in Atka Bay...
Manual measurements of sea ice thickness, sub-ice platelet layer thickness, freeboard, and snow thickness are distributed evenly and repeated along a 25km-long transect across... -
(Table 2) Surface exposure ages of samples near the head of Reedy Glacier
Be-10 concentrations are based on Be isotopic measurements normalized to pre-2007 values of the KNSTD standard series. Multiply by 1.106 for values compatible with post-2007... -
(Table 1) Surface exposure ages of samples from the Quartz Hills, Reedy Glacier
Be-10 concentrations are based on Be isotopic measurements normalized to pre-2007 values of the KNSTD standard series. Multiply by 1.106 for values compatible with post-2007... -
(Table 1) Attenuation coefficient of lateral propagating light in sea ice, so...
The attenuation property of a lateral propagating light (LPL) in sea ice was measured using an artificial lamp in the Canadian Arctic during the 2007/2008 winter. A measurement... -
(Table 1) Clay and non-clay mineral composition of dirty ice samples from acr...
Extensive dirty ice patches with up to 7 kg/m**2 sediment concentrations in layers of up to 10 cm thickness were encountered in 2005 and 2007 in numerous areas across the... -
(Table 1) White ice and melt pond characteristics in Darnley and Franklin Bay...
Melt pond covered sea ice is a ubiquitous feature of the summertime Arctic Ocean when meltwater collects in lower-lying areas of ice surfaces. Horizontal transects were... -
(Table 1) Ice thickness at lake Nam Co, Tibet, during 2008-2009
Lake ice change is one of the sensitive indicators of regional and global climate change. Different sources of data are used in monitoring lake ice phenology nowadays. Visible... -
Age determination and glacier model for a small ice cap on Baffin Island
Records of Neoglacial glacier activity in the Arctic constructed from moraines are often incomplete due to a preservation bias toward the most extensive advance, usually the... -
Snow cover data across Nordenskiöldland, Svalbard, from point measurements du...
Snow depths and bulk densities of the annual snow layer were measured at 69 different locations on glaciers across Nordenskiöldland, Svalbard, during the spring seasons of the... -
(Table S1) Molar gas ratios and stable oxygen and nitrogen gas isotopes of ai...
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(Table S2) Molar gas ratios and stable oxygen and nitrogen gas isotopes of ai...
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(Electronic annex 2) Mercury species concentration in ice and brine samples n...
This dataset has no description
