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Annual layering in the NGRIP ice core during the Eemian

  • Weiterlesen über Annual layering in the NGRIP ice core during the Eemian

A refined TALDICE-1a age scale from 55 to 112 ka before present for the Talos Dome ice core based on high-resolution methane measurements

  • Weiterlesen über A refined TALDICE-1a age scale from 55 to 112 ka before present for the Talos Dome ice core based on high-resolution methane measurements

Continuous Flow Analysis of Labile Iron in Ice-Cores

  • Weiterlesen über Continuous Flow Analysis of Labile Iron in Ice-Cores

Eemian interglacial reconstructed from a Greenland folded ice core

  • Weiterlesen über Eemian interglacial reconstructed from a Greenland folded ice core

Representativeness and seasonality of major ion records derived from NEEM firn cores

  • Weiterlesen über Representativeness and seasonality of major ion records derived from NEEM firn cores

Millennial changes in North American wildfire and soil activity over the last glacial cycle

  • Weiterlesen über Millennial changes in North American wildfire and soil activity over the last glacial cycle

High-resolution aerosol concentration data from the Greenland NorthGRIP and NEEM deep ice cores

  • Weiterlesen über High-resolution aerosol concentration data from the Greenland NorthGRIP and NEEM deep ice cores

Magnitude, frequency and climate forcing of global volcanism during the last glacial period as seen in Greenland and Antarctic ice cores (60–9 ka)

  • Weiterlesen über Magnitude, frequency and climate forcing of global volcanism during the last glacial period as seen in Greenland and Antarctic ice cores (60–9 ka)

Bipolar volcanic synchronization of abrupt climate change in Greenland and Antarctic ice cores during the last glacial period

  • Weiterlesen über Bipolar volcanic synchronization of abrupt climate change in Greenland and Antarctic ice cores during the last glacial period

Decadal-scale progression of the onset of Dansgaard–Oeschger warming events

  • Weiterlesen über Decadal-scale progression of the onset of Dansgaard–Oeschger warming events

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