What could have caused pre-industrial biomass burning emissions to exceed current rates?

Recent studies based on trace gas mixing ratios in ice cores and charcoal data indicate that biomass burning emissions over the past millennium exceeded contemporary emissions by up to a factor of 4 for certain time periods. This is surprising because various sources of biomass burning are linked wi...

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Published in:Climate of the Past
Main Authors: van der Werf, G. R., Peters, W., Giglio, L., van Leeuwen, T. T.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:https://hdl.handle.net/11370/58ffccba-10d0-43dc-8f30-d16bbb326b85
https://research.rug.nl/en/publications/58ffccba-10d0-43dc-8f30-d16bbb326b85
https://doi.org/10.5194/cp-9-289-2013
https://pure.rug.nl/ws/files/55011749/cp_9_289_2013_1_.pdf
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spelling ftunigroningenpu:oai:pure.rug.nl:publications/58ffccba-10d0-43dc-8f30-d16bbb326b85 2024-06-02T08:08:08+00:00 What could have caused pre-industrial biomass burning emissions to exceed current rates? van der Werf, G. R. Peters, W. Giglio, L. van Leeuwen, T. T. 2013-01-31 application/pdf https://hdl.handle.net/11370/58ffccba-10d0-43dc-8f30-d16bbb326b85 https://research.rug.nl/en/publications/58ffccba-10d0-43dc-8f30-d16bbb326b85 https://doi.org/10.5194/cp-9-289-2013 https://pure.rug.nl/ws/files/55011749/cp_9_289_2013_1_.pdf eng eng https://research.rug.nl/en/publications/58ffccba-10d0-43dc-8f30-d16bbb326b85 info:eu-repo/semantics/openAccess van der Werf , G R , Peters , W , Giglio , L & van Leeuwen , T T 2013 , ' What could have caused pre-industrial biomass burning emissions to exceed current rates? ' , Climate of the Past , vol. 9 , no. 1 , pp. 289-306 . https://doi.org/10.5194/cp-9-289-2013 article 2013 ftunigroningenpu https://doi.org/10.5194/cp-9-289-2013 2024-05-07T19:39:02Z Recent studies based on trace gas mixing ratios in ice cores and charcoal data indicate that biomass burning emissions over the past millennium exceeded contemporary emissions by up to a factor of 4 for certain time periods. This is surprising because various sources of biomass burning are linked with population density, which has increased over the past centuries. We have analysed how emissions from several landscape biomass burning sources could have fluctuated to yield emissions that are in correspondence with recent results based on ice core mixing ratios of carbon monoxide (CO) and its isotopic signature measured at South Pole station (SPO). Based on estimates of contemporary landscape fire emissions and the TM5 chemical transport model driven by present-day atmospheric transport and OH concentrations, we found that CO mixing ratios at SPO are more sensitive to emissions from South America and Australia than from Africa, and are relatively insensitive to emissions from the Northern Hemisphere. We then explored how various landscape biomass burning sources may have varied over the past centuries and what the resulting emissions and corresponding CO mixing ratio at SPO would be, using population density variations to reconstruct sources driven by humans (e.g., fuelwood burning) and a new model to relate savanna emissions to changes in fire return times. We found that to match the observed ice core CO data, all savannas in the Southern Hemisphere had to burn annually, or bi-annually in combination with deforestation and slash and burn agriculture exceeding current levels, despite much lower population densities and lack of machinery to aid the deforestation process. While possible, these scenarios are unlikely and in conflict with current literature. However, we do show the large potential for increased emissions from savannas in a pre-industrial world. This is mainly because in the past, fuel beds were probably less fragmented compared to the current situation; satellite data indicates that the majority of ... Article in Journal/Newspaper ice core South pole University of Groningen research database South Pole Climate of the Past 9 1 289 306
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description Recent studies based on trace gas mixing ratios in ice cores and charcoal data indicate that biomass burning emissions over the past millennium exceeded contemporary emissions by up to a factor of 4 for certain time periods. This is surprising because various sources of biomass burning are linked with population density, which has increased over the past centuries. We have analysed how emissions from several landscape biomass burning sources could have fluctuated to yield emissions that are in correspondence with recent results based on ice core mixing ratios of carbon monoxide (CO) and its isotopic signature measured at South Pole station (SPO). Based on estimates of contemporary landscape fire emissions and the TM5 chemical transport model driven by present-day atmospheric transport and OH concentrations, we found that CO mixing ratios at SPO are more sensitive to emissions from South America and Australia than from Africa, and are relatively insensitive to emissions from the Northern Hemisphere. We then explored how various landscape biomass burning sources may have varied over the past centuries and what the resulting emissions and corresponding CO mixing ratio at SPO would be, using population density variations to reconstruct sources driven by humans (e.g., fuelwood burning) and a new model to relate savanna emissions to changes in fire return times. We found that to match the observed ice core CO data, all savannas in the Southern Hemisphere had to burn annually, or bi-annually in combination with deforestation and slash and burn agriculture exceeding current levels, despite much lower population densities and lack of machinery to aid the deforestation process. While possible, these scenarios are unlikely and in conflict with current literature. However, we do show the large potential for increased emissions from savannas in a pre-industrial world. This is mainly because in the past, fuel beds were probably less fragmented compared to the current situation; satellite data indicates that the majority of ...
format Article in Journal/Newspaper
author van der Werf, G. R.
Peters, W.
Giglio, L.
van Leeuwen, T. T.
spellingShingle van der Werf, G. R.
Peters, W.
Giglio, L.
van Leeuwen, T. T.
What could have caused pre-industrial biomass burning emissions to exceed current rates?
author_facet van der Werf, G. R.
Peters, W.
Giglio, L.
van Leeuwen, T. T.
author_sort van der Werf, G. R.
title What could have caused pre-industrial biomass burning emissions to exceed current rates?
title_short What could have caused pre-industrial biomass burning emissions to exceed current rates?
title_full What could have caused pre-industrial biomass burning emissions to exceed current rates?
title_fullStr What could have caused pre-industrial biomass burning emissions to exceed current rates?
title_full_unstemmed What could have caused pre-industrial biomass burning emissions to exceed current rates?
title_sort what could have caused pre-industrial biomass burning emissions to exceed current rates?
publishDate 2013
url https://hdl.handle.net/11370/58ffccba-10d0-43dc-8f30-d16bbb326b85
https://research.rug.nl/en/publications/58ffccba-10d0-43dc-8f30-d16bbb326b85
https://doi.org/10.5194/cp-9-289-2013
https://pure.rug.nl/ws/files/55011749/cp_9_289_2013_1_.pdf
geographic South Pole
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South pole
genre_facet ice core
South pole
op_source van der Werf , G R , Peters , W , Giglio , L & van Leeuwen , T T 2013 , ' What could have caused pre-industrial biomass burning emissions to exceed current rates? ' , Climate of the Past , vol. 9 , no. 1 , pp. 289-306 . https://doi.org/10.5194/cp-9-289-2013
op_relation https://research.rug.nl/en/publications/58ffccba-10d0-43dc-8f30-d16bbb326b85
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