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Historic Global Biomass Burning Emissions for CMIP6 (BB4CMIP) Based on Merging Satellite Observations with Proxies and Fire Models (1750-2015)

Authors :
van Marle, Margreet J. E
Kloster, Silvia
Magi, Brian I
Marlon, Jennifer R
Daniau, Anne-Laure
Field, Robert D
Arneth, Almut
Forrest, Matthew
Hantson, Stijn
Kehrwald, Natalie M
Knorr, Wolfgang
Lasslop, Gitta
Li, Fang
Mangeon, Stephane
Yue, Chao
Kaiser, Johannes W
van der Werf, Guido R
Source :
Geoscientific Model Development. 10(9)
Publication Year :
2017
Publisher :
United States: NASA Center for Aerospace Information (CASI), 2017.

Abstract

Fires have influenced atmospheric composition and climate since the rise of vascular plants, and satellite data has shown the overall global extent of fires. Our knowledge of historic fire emissions has progressively improved over the past decades due mostly to the development of new proxies and the improvement of fire models. Currently there is a suite of proxies including sedimentary charcoal records, measurements of fire-emitted trace gases and black carbon stored in ice and firn, and visibility observations. These proxies provide opportunities to extrapolate emissions estimates based on satellite data starting in 1997, but each proxy has strengths and weaknesses regarding, for example, the spatial and temporal extents over which they are representative. We developed a new historic biomass burning emissions dataset starting in 1750 that merges the satellite record with several existing proxies, and uses the average of six models from the Fire Model Intercomparison Project (FireMIP) protocol to estimate emissions when the available proxies had limited coverage. According to our approach, global biomass burning emissions were relatively constant with 10-year averages varying between 1.8 and 2.3 petagrams of carbon per year. Carbon emissions increased only slightly over the full time period and peaked during the 1990's after which they decreased gradually. There is substantial uncertainty in these estimates and patterns varied depending on choices regarding data representation, especially on regional scales. The observed pattern in fire carbon emissions is for a large part driven by African fires, which accounted for 58 percent of global fire carbon emissions. African fire emissions declined since about 1950 due to conversion of savanna to cropland, and this decrease is partially compensated for by increasing emissions in deforestation zones of South America and Asia. These global fire emissions estimates are mostly suited for global analyses and will be used in the Coupled Model Intercomparison Project Phase 6 (CMIP6) simulations.

Details

Language :
English
ISSN :
19919603 and 1991959X
Volume :
10
Issue :
9
Database :
NASA Technical Reports
Journal :
Geoscientific Model Development
Notes :
EU H2020 MACC-III 633080, , NNX14AB99A, , EU PEGASOS 265148, , NSF BCS-1437074, , EU FP7 BACCHUS 603445, , NSF BCS-1436496, , PICS CNRS 06484, , ERC 280061, , EU FP7 LUC4C 603542
Publication Type :
Report
Accession number :
edsnas.20170009159
Document Type :
Report
Full Text :
https://doi.org/10.5194/gmd-10-3329-2017