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ICE CORE METHODS | Studies of Firn Air
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Assessment of diffusive isotopic fractionation in polar firn, and application to...
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An automated GC-C-GC-IRMS setup to measure paleoatmospheric δ 13 C-CH 4 , δ 15 N...
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An automated GC-C-GC-IRMS setup to measure palaeoatmospheric δ13C-CH4, δ15N-N2O...
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An automated GC-C-GC-IRMS setup to measure palaeoatmospheric δ13C-CH4, δ15N-N2O...
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An automated GC-C-GC-IRMS setup to measure palaeoatmospheric delta C-13-CH4, del...
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An automated GC-C-GC-IRMS setup to measure palaeoatmospheric d13C-CH4, d15N-N2O...
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The potential of 14CO in glacial ice as a tracer for past cosmic ray flux and at...
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An automated setup to measure paleoatmospheric δ13C-CH4, δ15N-N2O and δ18O-N2O i...
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How well do different tracers constrain the firn diffusivity profile?
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Consistent evidence of increasing Antarctic accumulation with warming
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A setup to analyze isotopes of paleoatmospheric CH4 and N2O in a single ice core...
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NOAA/WDS Paleoclimatology - Greenland 22,000 Year Seasonal Temperature Reconstru...
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Diachronous retreat of the Greenland ice sheet during the last deglaciation
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Greenland-Wide Seasonal Temperatures During the Last Deglaciation
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Consistent evidence of increasing Antarctic accumulation with warming
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Continuous measurements of methane mixing ratios from ice cores
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Continuous measurements of methane mixing ratios from ice cores
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Continuous measurements of methane mixing ratios from ice cores
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Continuous measurements of methane mixing ratios from ice cores
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