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Visual stratigraphy of the North Greenland Ice Core Project (NorthGRIP) ice core during the last glacial period

  • Weiterlesen über Visual stratigraphy of the North Greenland Ice Core Project (NorthGRIP) ice core during the last glacial period

Deconvolution‐based resolution enhancement of chemical ice core records obtained by continuous flow analysis

  • Weiterlesen über Deconvolution‐based resolution enhancement of chemical ice core records obtained by continuous flow analysis

Volcanic ash layers from the Last Glacial Termination in the NGRIP ice core

  • Weiterlesen über Volcanic ash layers from the Last Glacial Termination in the NGRIP ice core

European Project for Ice Coring in Antarctica (EPICA)

  • Weiterlesen über European Project for Ice Coring in Antarctica (EPICA)

Effect of impurities on grain growth in cold ice sheets

  • Weiterlesen über Effect of impurities on grain growth in cold ice sheets

"EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years

  • Weiterlesen über "EDML1": a chronology for the EPICA deep ice core from Dronning Maud Land, Antarctica, over the last 150 000 years

Ice core evidence for a very tight link between North Atlantic and east Asian glacial climate

  • Weiterlesen über Ice core evidence for a very tight link between North Atlantic and east Asian glacial climate

The Southern Hemisphere at glacial terminations: insights from the Dome C ice core

  • Weiterlesen über The Southern Hemisphere at glacial terminations: insights from the Dome C ice core

Sulfate Spikes in the Deep Layers of EPICA-Dome C Ice Core: Evidence of Glaciological Artifacts

  • Weiterlesen über Sulfate Spikes in the Deep Layers of EPICA-Dome C Ice Core: Evidence of Glaciological Artifacts

New MIS 19 EPICA Dome C high resolution deuterium data: Hints for a problematic preservation of climate variability at sub-millennial scale in the “oldest ice”

  • Weiterlesen über New MIS 19 EPICA Dome C high resolution deuterium data: Hints for a problematic preservation of climate variability at sub-millennial scale in the “oldest ice”

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