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Foraminifer counts in core JM01-1199, and review of radiocarbon ages in the N...
We compare six high-resolution Holocene, sediment cores along a S-N transect on the Norwegian-Svalbard continental margin from ca 60°N to 77.4°N, northern North Atlantic.... -
Methane and nitrous oxide dissolved gas concentrations from rivers in the Nor...
This dataset contains methane and nitrous oxide dissolved gas concentration and dissolved methane carbon isotope data from rivers in the Canadian Arctic Archipelago region... -
(Table 3) Basal melting rates under the Amery Ice Shelf, East Antarctica
The basal melting and freezing rates under the Amery Ice Shelf, East Antarctica, are evaluated, and their spatial distributions mapped. Ice velocity, surface elevation and... -
(Table 1) Characteristics of snow pits on De Geerfonna and Vestfonna during t...
Extensive glaciological field measurements were carried out on the ice cap Vestfonna as well as on the minor ice body De Geerfonna (Nordaustlandet, Svalbard) within the... -
(Table 1) Stable oxygen isotopic ratios and yearly snow accumulation of firn ...
We analyse ice cores from Vestfonna ice cap (Nordaustlandet, Svalbard). Oxygen isotopic measurements were made on three firn cores (6.0, 11.0 and 15.5 m deep) from the two... -
Upper air soundings during POLARSTERN cruise ANT-XXV/2
The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled... -
Upper air soundings during POLARSTERN cruise ARK-XXIV/3
The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled... -
Upper air soundings during POLARSTERN cruise ANT-XXIV/2
The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled... -
Upper air soundings during POLARSTERN cruise ANT-XXIII/9
The upper air soundings are normally performed once a day to measure vertical profiles of air pressure, temperature, relative humidity and the wind vector. Helium filled... -
Accumulation, velocities, fluxes and mass balance of glacial tributaries to t...
By incorporating recently available remote sensing data, we investigated the mass balance for all individual tributary glacial basins of the Lambert Glacier-Amery Ice Shelf... -
Mean chemical characteristics and volcano signatures of ice cores from Belukh...
Ice cores from outside the Greenland and Antarctic ice sheets are difficult to date because of seasonal melting and multiple sources (terrestrial, marine, biogenic and... -
Isotopic composition of diet and tissues, and isotope discrimination factors ...
Breeding in the high Arctic is time constrained and animals should therefore start with their annual reproduction as early as possible. To allow for such early reproduction in... -
Geochemistry of frost flowers and snow obtained near Ahlmann summit, Vestfonn...
The chemistry of snow and ice cores from Svalbard is influenced by variations in local sea ice margin and distance to open water. Snow pits sampled at two summits of Vestfonna... -
Database of Antarctic snow isotopic composition
Data included in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 -
Initial biomass and biomass change of tundra and forest plants in three herbi...
Recent Pan-Arctic shrub expansion has been interpreted as a response to a warmer climate. However, herbivores can also influence the abundance of shrubs in arctic ecosystems. We... -
(Table 1) GRACE-derived mass balance of the Greenland ice sheet 2002-2010
We re-evaluate the Greenland mass balance for the recent period using low-pass Independent Component Analysis (ICA) post-processing of the Level-2 GRACE data (2002-2010) from... -
(Appendix A) Abundance of selected coccolithophores in sediment core DS97-2P,...
The calcareous nannofossil assemblages from sediment core DS97-2P from the Reykjanes Ridge have been investigated to document oceanographic changes in surface water during the... -
(Appendix A) Relative abundance of Emiliania huxleyi in sediment cores of the...
The coccolithophore species Emiliania huxleyi is characterized by a wide range of sizes, which can be easily distinguished in the light microscope. In this study we have... -
(Table 2) Radiocarbon dates of sediment cores obtained during Bio Hespérides ...
A high-resolution paleomagnetic and rock magnetic study has been carried out on sediment cores collected in glaciomarine silty-clay sequences from the continental shelf and... -
(Table 1) Physical oceanography during Lance cruise LA99/2 in the marginal ic...
Zooplankton was studied on eight stations in the marginal ice zone (MIZ) of the Barents Sea, in May 1999, along two transects across the ice edge. On each station, physical...
