Predictability of biomass burning in response to climate changes
Version of Record online: 23 OCT 2012
©2012. American Geophysical Union. All Rights Reserved.
Global Biogeochemical Cycles
Volume 26, Issue 4, December 2012
How to Cite
2012), Predictability of biomass burning in response to climate changes, Global Biogeochem. Cycles, 26, GB4007, doi:10.1029/2011GB004249., et al. (
- Issue online: 23 OCT 2012
- Version of Record online: 23 OCT 2012
- Manuscript Accepted: 4 SEP 2012
- Manuscript Revised: 17 AUG 2012
- Manuscript Received: 9 NOV 2011
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|gbc1936-sup-0001-readme.txt||plain text document||8K||readme.txt|
|gbc1936-sup-0002-fs01.pdf||PDF document||527K||Figure S1. Simulated changes in semi-hemispheric mean annual temperature (MAT) and runoff (precipitation minus evaporation, P-E) from the ECBILT-CLIO Sim2b1 simulation.|
|gbc1936-sup-0003-fs02.pdf||PDF document||468K||Figure S2. Simulated changes of summer (JJA in the Northern Hemisphere; DJF in the Southern Hemisphere), winter (DJF in the Northern Hemisphere; JJA in the Southern Hemisphere), and annual temperature for latitudinal belts from the northern polar to the southern polar zone.|
|gbc1936-sup-0004-fs03.pdf||PDF document||115K||Figure S3. Generalized additive model (GAM) showing the relationship between ca 65,000 individual charcoal influx z-scores and climate.|
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