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Variation of Atmospheric Pressure01:18

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Related Experiment Video

Updated: Jul 22, 2026

Measurement of Greenhouse Gas Flux from Agricultural Soils Using Static Chambers
11:50

Measurement of Greenhouse Gas Flux from Agricultural Soils Using Static Chambers

Published on: August 3, 2014

Variations in atmospheric N2O concentration during abrupt climatic changes

Fluckiger1, Dallenbach, Blunier

  • 1Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland. CNRS Laboratoire de Glaciologie et Geophysique de l'Environnement (LGGE), Boite Postale 96, 38402 St Martin d'Heres Cedex, Gr.

Science (New York, N.Y.)
|July 10, 1999
PubMed
Summary

Atmospheric nitrous oxide (N2O) levels are rising. Ice core data reveals N2O concentrations paralleled temperature shifts during past climate changes, offering insights into environmental responses.

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Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O

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Last Updated: Jul 22, 2026

Measurement of Greenhouse Gas Flux from Agricultural Soils Using Static Chambers
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Published on: August 3, 2014

Automated, High-resolution Mobile Collection System for the Nitrogen Isotopic Analysis of NOx
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Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O
08:05

Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O

Published on: October 7, 2020

Area of Science:

  • Paleoclimatology
  • Atmospheric Chemistry
  • Greenhouse Gas Research

Background:

  • Nitrous oxide (N2O) is a significant greenhouse gas with a current annual increase of 0.25%.
  • Understanding past N2O variations is crucial for assessing its role in climate dynamics.

Purpose of the Study:

  • To reconstruct past atmospheric N2O concentrations using ice core records.
  • To investigate the relationship between N2O levels and temperature variations during climatic shifts.

Main Methods:

  • Analysis of two ice cores from Summit, Central Greenland.
  • Dating and measurement of N2O concentrations within ice core samples.

Main Results:

  • A millennium-long N2O record has reduced uncertainty in preindustrial concentration estimates.
  • N2O concentrations closely tracked rapid temperature changes during the last glacial-interglacial transition and a rapid climate change event in the last ice age.

Conclusions:

  • Past N2O concentrations fluctuated in sync with Northern Hemisphere temperature variations.
  • This demonstrates a clear environmental response to global climatic changes, with N2O playing a key role.