Author
Listed:
- Vasilii V. Petrenko
(University of Rochester)
- Andrew M. Smith
(Australian Nuclear Science and Technology Organisation (ANSTO))
- Hinrich Schaefer
(National Institute of Water and Atmospheric Research (NIWA))
- Katja Riedel
(National Institute of Water and Atmospheric Research (NIWA))
- Edward Brook
(College of Earth, Ocean and Atmospheric Sciences, Oregon State University)
- Daniel Baggenstos
(Scripps Institution of Oceanography, University of California, San Diego
University of Berne, Physics Institute)
- Christina Harth
(Scripps Institution of Oceanography, University of California, San Diego)
- Quan Hua
(Australian Nuclear Science and Technology Organisation (ANSTO))
- Christo Buizert
(College of Earth, Ocean and Atmospheric Sciences, Oregon State University)
- Adrian Schilt
(College of Earth, Ocean and Atmospheric Sciences, Oregon State University)
- Xavier Fain
(Université Grenoble Alpes/CNRS, Laboratoire de Glaciologie et Géophysique de l’Environnement (LGGE), UMR 5183)
- Logan Mitchell
(College of Earth, Ocean and Atmospheric Sciences, Oregon State University
University of Utah)
- Thomas Bauska
(College of Earth, Ocean and Atmospheric Sciences, Oregon State University
University of Cambridge)
- Anais Orsi
(Scripps Institution of Oceanography, University of California, San Diego
Laboratoire des Sciences du Climat et de l’Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay)
- Ray F. Weiss
(Scripps Institution of Oceanography, University of California, San Diego)
- Jeffrey P. Severinghaus
(Scripps Institution of Oceanography, University of California, San Diego)
Abstract
Measurements from Antarctic ice suggest that geological methane emissions are much lower than previously thought, and that methane emissions from hydrates and permafrost in response to climate warming are minimal.
Suggested Citation
Vasilii V. Petrenko & Andrew M. Smith & Hinrich Schaefer & Katja Riedel & Edward Brook & Daniel Baggenstos & Christina Harth & Quan Hua & Christo Buizert & Adrian Schilt & Xavier Fain & Logan Mitchell, 2017.
"Minimal geological methane emissions during the Younger Dryas–Preboreal abrupt warming event,"
Nature, Nature, vol. 548(7668), pages 443-446, August.
Handle:
RePEc:nat:nature:v:548:y:2017:i:7668:d:10.1038_nature23316
DOI: 10.1038/nature23316
Download full text from publisher
As the access to this document is restricted, you may want to search for a different version of it.
Corrections
All material on this site has been provided by the respective publishers and authors. You can help correct errors and omissions. When requesting a correction, please mention this item's handle: RePEc:nat:nature:v:548:y:2017:i:7668:d:10.1038_nature23316. See general information about how to correct material in RePEc.
If you have authored this item and are not yet registered with RePEc, we encourage you to do it here. This allows to link your profile to this item. It also allows you to accept potential citations to this item that we are uncertain about.
We have no bibliographic references for this item. You can help adding them by using this form .
If you know of missing items citing this one, you can help us creating those links by adding the relevant references in the same way as above, for each refering item. If you are a registered author of this item, you may also want to check the "citations" tab in your RePEc Author Service profile, as there may be some citations waiting for confirmation.
For technical questions regarding this item, or to correct its authors, title, abstract, bibliographic or download information, contact: Sonal Shukla or Springer Nature Abstracting and Indexing (email available below). General contact details of provider: http://www.nature.com .
Please note that corrections may take a couple of weeks to filter through
the various RePEc services.