Variable temperature effects of Open Top Chambers at polar and alpine sites explained by irradiance and snow depth
Version of Record online: 18 OCT 2012
© 2012 Blackwell Publishing Ltd
Global Change Biology
Volume 19, Issue 1, pages 64–74, January 2013
How to Cite
Bokhorst, S., Huiskes, A., Aerts, R., Convey, P., Cooper, E. J., Dalen, L., Erschbamer, B., Gudmundsson, J., Hofgaard, A., Hollister, R. D., Johnstone, J., Jónsdóttir, I. S., Lebouvier, M., Van de Vijver, B., Wahren, C.-H. and Dorrepaal, E. (2013), Variable temperature effects of Open Top Chambers at polar and alpine sites explained by irradiance and snow depth. Global Change Biology, 19: 64–74. doi: 10.1111/gcb.12028
- Issue online: 6 DEC 2012
- Version of Record online: 18 OCT 2012
- Accepted manuscript online: 17 SEP 2012 09:43PM EST
- Manuscript Accepted: 4 SEP 2012
- Manuscript Revised: 29 AUG 2012
- Manuscript Received: 11 MAY 2012
- Netherlands Organisation for Scientific Research
- Natural Sciences and Engineering Research Council of Canada
- French Polar Institute
- Australian Research Council
- British Antarctic Survey
- European Commission
- Norwegian Svalbard Society
- Norwegian Polar Institute
- University of Innsbruck
- Club Allegra Munich
- Icelandic Research Fund
- U.S. National Science Foundation
Figure S1. Map with study sites indicated by black circles. From Convey 2010, with permission.
Figure S2. OTC effect on air temperatures.
Figure S3. OTC effect on soil surface temperatures.
Figure S4. OTC effect on soil temperatures.
Figure S5. Air temperature extremes in control plots and Open Top Chambers.
Figure S6. Temperature extremes at the soil surface in control plots and Open Top Chambers.
Figure S7. Temperature extremes in the soil in control plots and Open Top Chambers.
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