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High‐resolution Holocene N2O ice core record and its relationship with CH4 and CO2
Open accessAbstract
Nitrous oxide (N 2 O) concentration records exist for the last 1000 years and for time periods of rapid climatic changes like the transition from the last glacial to today's interglacial and for one of the fast climate variations during the last ice age. Little is known, however, about possible N 2 O variations during the more stable climate of the present interglacial (Holocene) spanning the last 11 thousand years. Here we fill this gap with a high‐resolution N 2 O record measured along the European Project for Ice Coring in Antarctica (EPICA) Dome C Antarctic ice core. On the same ice we obtained high‐resolution methane and carbon dioxide records. This provides the unique opportunity to compare variations of the three most important greenhouse gases (after water vapor) without any uncertainty in their relative timing. The CO 2 and CH 4 records are in good agreement with previous measurements on other ice cores. The N 2 O concentration started to decrease in the early Holocene and reached minimum values around 8 ka (<260 ppbv) before a slow increase to its preindustrial concentration of ∼265 ppbv.
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Law Dome CO 2 , CH 4 and N 2 O ice core records extended to 2000 years BP
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Atmospheric Methane and Nitrous Oxide of the Late Pleistocene from Antarctic Ice Cores
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Self-citation
Metadata
- Authors
- Flückiger, J., Monnin, E., Stauffer, B., Schwander, J., Stocker, T. F., Chappellaz, J., Raynaud, D., & Barnola, J.
- Venue
- Global Biogeochemical Cycles
- Publisher
- American Geophysical Union (AGU)
- Published
- 2002-02-16
- Volume
- 16
- Issue
- 1
- ISSN
- 0886-6236 (ISSN-L)
- 1944-9224
- OpenAlex
- W1660980549
- Cited by
- 245
- References
- 2
- FWCI
- 11.59
- Type
- journal article
- Language
- en
- Open access
- bronze
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