-
Stable-isotope records from Dronning Maud Land, Antarctica
The European Project for Ice Coring in Antarctica (EPICA) includes a comprehensive pre-site survey on the inland ice plateau of Dronning Maud Land. This paper focuses on the... -
Chemical measurements from the EPICA Dome C core
Sea ice and dust flux increased greatly in the Southern Ocean during the last glacial period. Palaeorecords provide contradictory evidence about marine productivity in this... -
Physical properties and accumulation rates in Dronning Maud Land, Antarctica
The European Programme for Ice Coring in Antarctica includes a comprehensive pre-site survey on the inland ice plateau of Dronning Maud Land, Antarctica. The German... -
Physical properties of firn cores from the 1995/96 and 1996/97 field seasons
The paper focuses on studies of snow-pit samples and shallow firn cores taken during the 1995-96 and 1996-97 field seasons at Amundsenisen, Dronning Maud Land, Antarctica. The... -
Data from the EPICA Dome C ice core EDC
The Antarctic Vostok ice core provided compelling evidence of the nature of climate, and of climate feedbacks, over the past 420,000 years. Marine records suggest that the... -
First results from stable-istope measurements on ice cores from Dronning Maud...
The European Project for Ice Coring in Antarctica (EPICA) focuses on the drilling of two deep ice cores, the first at Dome C and the second at Kohnen station (75°00' S, 0°04' E)... -
EPICA Dome C carbon dioxide concentrations from 650 to 391 kyr BP
A record of atmospheric carbon dioxide (CO2) concentrations measured on the EPICA (European Project for Ice Coring in Antarctica) Dome Concordia ice core extends the Vostok CO2... -
Carbon dioxide concentrations for the Last Millennium, Antarctica
The most direct method of investigating past variations of the atmospheric CO2 concentration before 1958, when continuous direct atmospheric CO2 measurements started, is the... -
High-resolution carbon dioxide concentration records from the EPICA Dome C ic...
Changes in past atmospheric carbon dioxide concentrations can be determined by measuring the composition of air trapped in ice cores from Antarctica. So far, the Antarctic... -
Static GPS measurements in the vicinity of EDML and an elevation model for Dr...
The knowledge of ice sheet surface topography and the location of the ice divides are essential for ice dynamic modeling. An improved digital elevation model (DEM) of Dronning... -
Rare earth elements determined in Antarctic ice by inductively coupled plasma
Inductively coupled plasma mass spectrometry (ICP-MS) is a suitable tool for multi-element analysis at low concentration levels. Rare earth element (REE) determinations in... -
Dust record from the EPICA Dome C ice core, Antarctica, covering 0 to 800 kyr BP
Dust can affect the radiative balance of the atmosphere by absorbing or reflecting incoming solar radiation and it can be a source of micronutrients, such as iron, to the ocean.... -
Aeolian dust and chemistry records from the EDML and EDC ice cores
To improve quantitative interpretation of ice core aeolian dust records a systematic methodical comparison has been made involving methods of water-insoluble particle counting... -
Thick-section images of the EPICA-Dronning-Maud-Land (EDML) ice core
This data set consists of 3.5 Million images with a total size of 313 GByte. -
Static GPS measurements and elevation model in the vicinity of the EDML deep-...
Interpretation of ice-core records requires accurate knowledge of the past and present surface topography and stress-strain fields. The European Project for Ice Coring in... -
Chronology for the EDML ice core from Dronning Maud Land, Antarctica, over th...
A chronology called EDML1 has been developed for the EPICA ice core from Dronning Maud Land (EDML). EDML1 is closely interlinked with EDC3, the new chronology for the EPICA ice... -
Methane and stable isotope record of ice core EDML from Dronning Maud Land, A...
Precise knowledge of the phase relationship between climate changes in the two hemispheres is a key for understanding the Earth's climate dynamics. For the last glacial period,...
