Frost for the trees: Did climate increase erosion in unglaciated landscapes during the late Pleistocene?-Reference-Cited by-同舟云学术

Frost for the trees: Did climate increase erosion in unglaciated landscapes during the late Pleistocene?

Published:2015-11-06 Issue:10 Volume:1 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Marshall Jill A.¹²^ORCID,Roering Joshua J.¹,Bartlein Patrick J.³^ORCID,Gavin Daniel G.³^ORCID,Granger Darryl E.⁴,Rempel Alan W.¹^ORCID,Praskievicz Sarah J.⁵,Hales Tristram C.⁶

Affiliation:

1. Department of Geological Sciences, University of Oregon, Eugene, OR 97403, USA.

2. Department of Earth and Planetary Science, University of California, Berkeley, Berkeley, CA 94720, USA.

3. Department of Geography, University of Oregon, Eugene, OR 97403, USA.

4. Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, IN 47907, USA.

5. Department of Geography, University of Alabama, Tuscaloosa, AL 35487, USA.

6. School of Earth and Ocean Sciences, Cardiff University, Cardiff CF10 3AT, UK.

Abstract

Frost processes more than doubled erosion rates in unglaciated terrain during the Last Glacial Maximum.

Funder

National Science Foundation

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference80 articles.

1. Rock damage and regolith transport by frost: An example of climate modulation of the geomorphology of the critical zone;Anderson R. S.;Earth Surf. Process. Landforms,2013

2. National Research Council (US) Committee on Challenges and Opportunities in Earth Surface Processes Landscapes on the Edge: New Horizons for Research on Earth’s Surface (The National Academies Press Washington DC 2010).

3. W. E. Dietrich D. G. Bellugi L. S. Sklar J. D. Stock A. M. Heimsath J. J. Roering in Predictions in Geomorphology P. R. Wilcock R. M. Iverson Eds. (American Geophysical Union Washington DC 2003) pp. 103–132.

4. Tectonic forcing of late Cenozoic climate

5. Worldwide acceleration of mountain erosion under a cooling climate

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