How will biotic interactions influence climate change–induced range shifts?
Version of Record online: 22 JUL 2013
© 2013 New York Academy of Sciences.
Annals of the New York Academy of Sciences
Volume 1297, Climate Change and Species Interactions: Ways Forward pages 112–125, September 2013
How to Cite
HilleRisLambers, J., Harsch, M. A., Ettinger, A. K., Ford, K. R. and Theobald, E. J. (2013), How will biotic interactions influence climate change–induced range shifts?. Annals of the New York Academy of Sciences, 1297: 112–125. doi: 10.1111/nyas.12182
- Issue online: 18 SEP 2013
- Version of Record online: 22 JUL 2013
- UW Royalty Research Foundation (J.H.)
- U.S. Department of Energy (DOE#DE-FC02-06ER64159 to J.H.)
- National Science Foundation
Disclaimer: Supplementary materials have been peer-reviewed but not copyedited.
|nyas12182-sup-0001-FigureS1.docx||247K||Figure S1. The 4.3-km elevational gradient created by Mt. Rainier (A) generates large gradients in temperature (B), winter precipitation (C, falling primarily as snow), and summer precipitation (D). Picture© Michael Arthur Hill/Wikimedia Commons/CC-BY-SA-3.0. Data in B–D are smoothed from 800×800-m grid cell estimates of 30-year monthly temperature and precipitation averages (1971–2000) through the PRISM climate model. Mean annual temperature is the average temperature across all months; winter precipitation, the sum of November–March values; and summer precipitation, the sum of May–September values.|
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