Hostname: page-component-76fb5796d-x4r87 Total loading time: 0 Render date: 2024-04-25T20:54:16.850Z Has data issue: false hasContentIssue false
  • English
  • Français

Changes Of Atmospheric Methane Concentration Parallel To Climatic Changes

Published online by Cambridge University Press:  20 January 2017

B. Stauffer ,
H. Oeschger  and
J. Schwander
B. Stauffer
Affiliation:
Physikalisches Institut, Universität Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland
H. Oeschger
Affiliation:
Physikalisches Institut, Universität Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland
J. Schwander
Affiliation:
Physikalisches Institut, Universität Bern, Sidlerstrasse 5, CH-3012 Bern, Switzerland
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Measurements on ice-core samples showed that atmospheric methane concentration changed with the large climatic cycles during the last two glaciations (Stauffer and others, 1988; Raynaud and others, 1988). The methane concentration is lower in cold periods and higher in warm periods. In this paper we discuss the results of CH4 measurements of samples from periods of minor climatic change, like the climatic optimum 8000 years B.P. and the Younger Dryas period about 10 000 to 11 000 years B.P.. The data are interpreted in terms of the present understanding of methane sources and sinks.

Type
Research Article
Information
Annals of Glaciology , Volume 14 , 1990 , pp. 359
Copyright
Copyright © International Glaciological Society 1990

References

Raynaud, D, Chappelaz, J, Barnola, J.M, Korotkevich, Y.S and Lorius, C. 1988. Climatic and CH4 cycle implications of glacial-interglacial CH4 change in the Vostok ice core. Nature, 333(6174), 655–657.Google Scholar
Stauffer, B, Lochbronner, E, Oeschger, H, and Schwander, J. 1988. Methane concentration in the glacial atmosphere was only half that of the preindustrial Holocene. Nature, 332(6167), 812–814.Google Scholar