Changes in the atmospheric CH4gradient between Greenland and Antarctica during the Last Glacial and the transition to the Holocene-Reference-Cited by-同舟云学术

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Changes in the atmospheric CH4gradient between Greenland and Antarctica during the Last Glacial and the transition to the Holocene

Published:2000-04-01 Issue:7 Volume:27 Page:1005-1008
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Dällenbach A.,Blunier T.,Flückiger J.,Stauffer B.,Chappellaz J.,Raynaud D.

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://www.agu.org/journals/gl/v027/i007/1999GL010873/1999GL010873.pdf

Reference13 articles.

1. Asynchrony of Antarctic and Greenland climate change during the last glacial period;Blunier;Nature,1998

2. Atmospheric methane and millennial scale climate change;Brook;AGU Monograph on Mechanisms of Millennial Scale Climate Change,1999

3. Changes in the atmospheric CH4 gradient between Greenland and Antarctica during the Holocene;Chappellaz;J. Geophys. Res.,1997

4. Synchronous changes in atmospheric CH4 and Greenland climate between 40 and 8 kyr BP;Chappellaz;Nature,1993

5. The atmospheric CH4 increase since the Last Glacial Maximum;Chappellaz;Tellus,1993

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