Articles | Volume 10, issue 9
https://doi.org/10.5194/gmd-10-3329-2017
https://doi.org/10.5194/gmd-10-3329-2017
Model experiment description paper
 | 
11 Sep 2017
Model experiment description paper |  | 11 Sep 2017

Historic global biomass burning emissions for CMIP6 (BB4CMIP) based on merging satellite observations with proxies and fire models (1750–2015)

Margreet J. E. van Marle, Silvia Kloster, Brian I. Magi, Jennifer R. Marlon, Anne-Laure Daniau, Robert D. Field, Almut Arneth, Matthew Forrest, Stijn Hantson, Natalie M. Kehrwald, Wolfgang Knorr, Gitta Lasslop, Fang Li, Stéphane Mangeon, Chao Yue, Johannes W. Kaiser, and Guido R. van der Werf

Data sets

Charcoal records Global Paleofire Working Group (GPWG) https://www.paleofire.org/

GFED4s data Global Fire Emissions Database http://www.globalfiredata.org/data.html

Biomass Burning emissions for CMIP6 (v1.2). Version 20161213. Earth System Grid Federation M. J. E. van Marle, S. Kloster, B. I. Magi, J. R. Marlon, A.-L. Daniau, R. D. Field, A. Arneth, M. Forrest, S. Hantson, N. M. Kehrwald, W. Knorr, G. Lasslop, F. Li, S. Mangeon, C. Yue, J. W. Kaiser, and G. R. van der Werf https://doi.org/10.22033/ESGF/input4MIPs.1117

Global fire emissions estimates during 1997–2015 G. R. van der Werf, J. T. Randerson, L. Giglio, T. T. van Leeuwen, Y. Chen, B. M. Rogers, M. Mu, M. J. E. van Marle, D. C. Morton, G. J. Collatz, R. J. Yokelson, and P. S. Kasibhatla https://doi.org/10.5194/essd-2016-62

Reconstructions of biomass burning from sediment-charcoal records to improve data–model comparisons J. R. Marlon, R. Kelly, A.-L. Daniau, B. Vannière, M. J. Power, P. Bartlein, P. Higuera, O. Blarquez, S. Brewer, T. Brücher, A. Feurdean, G. G. Romera, V. Iglesias, S. Y. Maezumi, B. Magi, C. J. Courtney Mustaphi, and T. Zhihai https://doi.org/10.5194/bg-13-3225-2016

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Short summary
Fire emission estimates are a key input dataset for climate models. We have merged satellite information with proxy datasets and fire models to reconstruct fire emissions since 1750 AD. Our dataset indicates that, on a global scale, fire emissions were relatively constant over time. Since roughly 1950, declining emissions from savannas were approximately balanced by increased emissions from tropical deforestation zones.