Methane and nitrous oxide in the ice core record

Polar ice cores contain, in trapped air bubbles, an archive of the concentrations of stable atmospheric gases. Of the major non-CO2 greenhouse gases, methane is measured quite routinely, while nitrous oxide is more challenging, with some artefacts occurring in the ice and so far limited interpretati...

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Published in:Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
Main Authors: Wolff, Eric, Spahni, Renato
Format: Article in Journal/Newspaper
Language:English
Published: Royal Society of London 2007
Subjects:
Online Access:https://boris.unibe.ch/25270/1/wolff07ptrs.pdf
https://boris.unibe.ch/25270/
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spelling ftunivbern:oai:boris.unibe.ch:25270 2023-08-20T04:00:23+02:00 Methane and nitrous oxide in the ice core record Wolff, Eric Spahni, Renato 2007 application/pdf https://boris.unibe.ch/25270/1/wolff07ptrs.pdf https://boris.unibe.ch/25270/ eng eng Royal Society of London https://boris.unibe.ch/25270/ info:eu-repo/semantics/restrictedAccess Wolff, Eric; Spahni, Renato (2007). Methane and nitrous oxide in the ice core record. Philosophical transactions of the Royal Society. Series A - mathematical, physical and engineering sciences, 365(1856), pp. 1775-1792. London: Royal Society of London 10.1098/rsta.2007.2044 <http://dx.doi.org/10.1098/rsta.2007.2044> info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2007 ftunivbern https://doi.org/10.1098/rsta.2007.2044 2023-07-31T20:48:45Z Polar ice cores contain, in trapped air bubbles, an archive of the concentrations of stable atmospheric gases. Of the major non-CO2 greenhouse gases, methane is measured quite routinely, while nitrous oxide is more challenging, with some artefacts occurring in the ice and so far limited interpretation. In the recent past, the ice cores provide the only direct measure of the changes that have occurred during the industrial period; they show that the current concentration of methane in the atmosphere is far outside the range experienced in the last 650 000 years; nitrous oxide is also elevated above its natural levels. There is controversy about whether changes in the pre-industrial Holocene are natural or anthropogenic in origin. Changes in wetland emissions are generally cited as the main cause of the large glacial–interglacial change in methane. However, changing sinks must also be considered, and the impact of possible newly described sources evaluated. Recent isotopic data appear to finally rule out any major impact of clathrate releases on methane at these time-scales. Any explanation must take into account that, at the rapid Dansgaard–Oeschger warmings of the last glacial period, methane rose by around half its glacial–interglacial range in only a few decades. The recent EPICA Dome C (Antarctica) record shows that methane tracked climate over the last 650 000 years, with lower methane concentrations in glacials than interglacials, and lower concentrations in cooler interglacials than in warmer ones. Nitrous oxide also shows Dansgaard–Oeschger and glacial–interglacial periodicity, but the pattern is less clear. Article in Journal/Newspaper Antarc* Antarctica EPICA ice core BORIS (Bern Open Repository and Information System, University of Bern) Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 365 1856 1775 1792
institution Open Polar
collection BORIS (Bern Open Repository and Information System, University of Bern)
op_collection_id ftunivbern
language English
description Polar ice cores contain, in trapped air bubbles, an archive of the concentrations of stable atmospheric gases. Of the major non-CO2 greenhouse gases, methane is measured quite routinely, while nitrous oxide is more challenging, with some artefacts occurring in the ice and so far limited interpretation. In the recent past, the ice cores provide the only direct measure of the changes that have occurred during the industrial period; they show that the current concentration of methane in the atmosphere is far outside the range experienced in the last 650 000 years; nitrous oxide is also elevated above its natural levels. There is controversy about whether changes in the pre-industrial Holocene are natural or anthropogenic in origin. Changes in wetland emissions are generally cited as the main cause of the large glacial–interglacial change in methane. However, changing sinks must also be considered, and the impact of possible newly described sources evaluated. Recent isotopic data appear to finally rule out any major impact of clathrate releases on methane at these time-scales. Any explanation must take into account that, at the rapid Dansgaard–Oeschger warmings of the last glacial period, methane rose by around half its glacial–interglacial range in only a few decades. The recent EPICA Dome C (Antarctica) record shows that methane tracked climate over the last 650 000 years, with lower methane concentrations in glacials than interglacials, and lower concentrations in cooler interglacials than in warmer ones. Nitrous oxide also shows Dansgaard–Oeschger and glacial–interglacial periodicity, but the pattern is less clear.
format Article in Journal/Newspaper
author Wolff, Eric
Spahni, Renato
spellingShingle Wolff, Eric
Spahni, Renato
Methane and nitrous oxide in the ice core record
author_facet Wolff, Eric
Spahni, Renato
author_sort Wolff, Eric
title Methane and nitrous oxide in the ice core record
title_short Methane and nitrous oxide in the ice core record
title_full Methane and nitrous oxide in the ice core record
title_fullStr Methane and nitrous oxide in the ice core record
title_full_unstemmed Methane and nitrous oxide in the ice core record
title_sort methane and nitrous oxide in the ice core record
publisher Royal Society of London
publishDate 2007
url https://boris.unibe.ch/25270/1/wolff07ptrs.pdf
https://boris.unibe.ch/25270/
genre Antarc*
Antarctica
EPICA
ice core
genre_facet Antarc*
Antarctica
EPICA
ice core
op_source Wolff, Eric; Spahni, Renato (2007). Methane and nitrous oxide in the ice core record. Philosophical transactions of the Royal Society. Series A - mathematical, physical and engineering sciences, 365(1856), pp. 1775-1792. London: Royal Society of London 10.1098/rsta.2007.2044 <http://dx.doi.org/10.1098/rsta.2007.2044>
op_relation https://boris.unibe.ch/25270/
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1098/rsta.2007.2044
container_title Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
container_volume 365
container_issue 1856
container_start_page 1775
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