Dataset - B2FIND

Landfast sea-ice and platelet-layer thickness and conductivity along Transect 1a

This dataset has no description

(Table 2) Seasonal ice speed at four GPS sites on Kangiata Nunata Sermia glac...

The summer period begins on day 155 for KNS1 and KNS2 and on day 180 for KNS3 and KNS4 and finishes at the end of our survey at each site. Ice speed for all nonsummer days is...

(Table 1) Site characteristics and ice thickness at four GPS sites on Kangiat...

This dataset has no description

(Table 3) Stable carbon and nitrogen isotope ratios of ice algae sampled in R...

Ice algae were obtained in the lowermost 5 to 7 cm of sea ice.

Annual glacier elevation change rate raster dataset, Southern Patagonia Ice F...

The contribution to sea level rise from Patagonian icefields is one of the largest mass losses outside the large ice sheets of Antarctica and Greenland. However, only a few...

Sea ice conditions within the Antarctic Marginal Ice Zone in summer 2016, onb...

Our knowledge of sea ice variability, which contributes to the detection of the Antarctic climate change trends, stems primarily from remotely sensed information. However, sea...

(Table 1) Seasonal sea ice concentration and the observed changes from 1972 t...

A reliable data set of Arctic sea ice concentration based on satellite observations exists since 1972. Over this time period of 36 years western arctic temperatures have...

(Appendix) Recent surface areas and historical lengths of glaciers from Patag...

Fluctuations in the length of 72 glaciers in the Northern and Southern Patagonia Icefield (NPI and SPI, respectively) and the Cordillera Darwin Icefield (CDI) were estimated...

Abb. 3 Change of altitude in the EGIG-West-East-profile

The members of the two International Glaciological Greenland Expeditions (EGIG) in 1959 and 1968 determined the altitudes in the West-East-profile by levelling. The comparison...