Late Quaternary temperature variability described as abrupt transitions on a 1/<i>f</i> noise background
In order to have a scaling description of the climate system that is not inherently non-stationary, the rapid shifts between stadials and interstadials during the last glaciation (the Dansgaard-Oeschger events) cannot be included in the scaling law. The same is true for the shifts between the glacia...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-03-01
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Series: | Earth System Dynamics |
Online Access: | http://www.earth-syst-dynam.net/7/281/2016/esd-7-281-2016.pdf |