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 inClimate of the past Vol. 9; no. 1; pp. 289 - 306
Main Authors van der Werf, G. R., Peters, W., van Leeuwen, T. T., Giglio, L.
Format Journal Article
LanguageEnglish
Published Katlenburg-Lindau Copernicus GmbH 31.01.2013
Copernicus Publications
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Online AccessGet full text
ISSN1814-9332
1814-9324
1814-9332
DOI10.5194/cp-9-289-2013

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Abstract 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 savannas have not burned in the past 10 yr, even in Africa, which is considered "the burning continent". Although we have not considered increased charcoal burning or changes in OH concentrations as potential causes for the elevated CO concentrations found at SPO, it is unlikely they can explain the large increase found in the CO concentrations in ice core data. Confirmation of the CO ice core data would therefore call for radical new thinking about causes of variable global fire rates over recent centuries.
AbstractList 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 savannas have not burned in the past 10 yr, even in Africa, which is considered "the burning continent". Although we have not considered increased charcoal burning or changes in OH concentrations as potential causes for the elevated CO concentrations found at SPO, it is unlikely they can explain the large increase found in the CO concentrations in ice core data. Confirmation of the CO ice core data would therefore call for radical new thinking about causes of variable global fire rates over recent centuries.
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 savannas have not burned in the past 10 yr, even in Africa, which is considered "the burning continent". Although we have not considered increased charcoal burning or changes in OH concentrations as potential causes for the elevated CO concentrations found at SPO, it is unlikely they can explain the large increase found in the CO concentrations in ice core data. Confirmation of the CO ice core data would therefore call for radical new thinking about causes of variable global fire rates over recent centuries
Audience Academic
Author Peters, W.
van Leeuwen, T. T.
van der Werf, G. R.
Giglio, L.
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  fullname: Giglio, L.
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Cites_doi 10.1073/pnas.0804042105
10.5194/acp-7-295-2007
10.1029/1999JD901006
10.1111/j.1466-8238.2010.00568.x
10.1126/science.1197257
10.1016/j.quascirev.2009.09.028
10.1177/0959683609356587
10.1126/science.1144856
10.1111/j.1365-2486.2008.01754.x
10.1038/nature11461
10.1007/BF00137988
10.1126/science.1163886
10.1029/2012JG002128
10.5194/acp-11-4039-2011
10.1007/0-387-21515-8_4
10.1126/science.1159769
10.1071/WF02042
10.5194/bg-7-1171-2010
10.3402/tellusb.v51i2.16276
10.1029/1999JD900835
10.1029/2002JD002272
10.1177/0959683612450196
10.3402/tellusb.v55i1.16354
10.1038/ngeo313
10.1029/2009GB003460
10.1016/j.atmosenv.2009.08.021
10.5194/acp-10-11707-2010
10.1038/nature01779
10.1111/j.1365-2486.2008.01786.x
10.3402/tellusb.v64i0.18196
10.1080/0143116031000070283
10.5194/bg-7-1877-2010
10.1126/science.1186925
10.1071/WF08016
10.1038/ngeo443
10.5194/acp-12-4365-2012
10.1073/pnas.1003669107
10.1046/j.1365-2699.2002.00677.x
10.1016/S0079-1946(97)81142-1
10.1111/j.1365-2699.2011.02595.x
10.5194/acp-10-7017-2010
10.5194/acp-11-3611-2011
10.1016/j.quascirev.2012.11.029
10.2307/1932179
10.1029/2005JD006338
10.1016/j.rse.2011.05.025
10.1038/440436a
10.1016/j.rse.2009.08.016
10.1016/j.gloplacha.2007.08.005
10.1029/1999GB900046
10.5194/gmd-3-445-2010
10.1073/pnas.0901970106
10.1073/pnas.0604090103
10.1016/j.quascirev.2010.10.010
10.1038/19066
10.1029/2007GB002961
10.1126/science.1115193
10.1029/2002GB001952
10.1111/j.1365-2486.2008.01655.x
10.1034/j.1600-0889.1999.00013.x
10.5194/acp-5-417-2005
10.1890/1051-0761(1999)009[0526:AYRAOC]2.0.CO;2
10.1126/science.227.4682.53
10.1029/2000GB001382
10.1111/j.1365-2486.2005.00920.x
10.1029/2007GB003122
10.1016/j.rse.2008.10.006
10.1890/100052
10.1071/9780643096493
10.1071/WF07011
10.1126/science.1086112
10.5194/acp-11-4705-2011
10.1126/science.1199809
10.1029/2009GL040000
10.1016/j.atmosenv.2010.01.011
10.1098/rstb.2006.1980
10.1007/s00382-007-0334-x
10.1034/j.1600-0889.1990.00009.x
10.1016/j.rse.2005.04.007
10.1029/2004GB002278
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References ref13
ref57
ref12
ref56
ref15
ref59
ref14
ref58
ref53
ref52
ref11
ref55
ref10
ref54
ref17
ref16
ref19
ref18
ref51
ref50
ref46
ref45
ref48
ref47
ref42
ref41
ref44
ref43
ref49
ref8
ref7
ref9
ref4
ref3
ref6
ref5
ref82
ref81
ref40
ref83
ref80
ref35
ref79
ref34
ref78
ref37
ref36
ref31
ref75
ref30
ref74
ref33
ref77
ref32
ref76
ref2
ref1
ref39
ref38
ref71
ref70
ref73
ref72
ref24
ref68
ref23
ref67
ref26
ref25
ref69
ref20
ref64
ref63
ref22
ref66
ref21
ref65
ref28
ref27
ref29
ref60
ref62
ref61
References_xml – ident: ref26
  doi: 10.1073/pnas.0804042105
– ident: ref7
  doi: 10.5194/acp-7-295-2007
– ident: ref71
  doi: 10.1029/1999JD901006
– ident: ref5
  doi: 10.1111/j.1466-8238.2010.00568.x
– ident: ref81
  doi: 10.1126/science.1197257
– ident: ref35
  doi: 10.1016/j.quascirev.2009.09.028
– ident: ref38
  doi: 10.1177/0959683609356587
– ident: ref48
  doi: 10.1126/science.1144856
– ident: ref4
  doi: 10.1111/j.1365-2486.2008.01754.x
– ident: ref67
  doi: 10.1038/nature11461
– ident: ref70
  doi: 10.1007/BF00137988
– ident: ref9
  doi: 10.1126/science.1163886
– ident: ref64
  doi: 10.1029/2012JG002128
– ident: ref1
  doi: 10.5194/acp-11-4039-2011
– ident: ref15
  doi: 10.1007/0-387-21515-8_4
– ident: ref28
  doi: 10.1126/science.1159769
– ident: ref18
  doi: 10.1071/WF02042
– ident: ref24
  doi: 10.5194/bg-7-1171-2010
– ident: ref76
– ident: ref75
  doi: 10.3402/tellusb.v51i2.16276
– ident: ref25
  doi: 10.1029/1999JD900835
– ident: ref45
  doi: 10.1029/2002JD002272
– ident: ref60
  doi: 10.1177/0959683612450196
– ident: ref40
  doi: 10.3402/tellusb.v55i1.16354
– ident: ref46
  doi: 10.1038/ngeo313
– ident: ref50
  doi: 10.1029/2009GB003460
– ident: ref52
  doi: 10.1016/j.atmosenv.2009.08.021
– ident: ref78
  doi: 10.5194/acp-10-11707-2010
– ident: ref13
  doi: 10.1038/nature01779
– ident: ref14
  doi: 10.1111/j.1365-2486.2008.01786.x
– ident: ref36
  doi: 10.3402/tellusb.v64i0.18196
– ident: ref22
  doi: 10.1080/0143116031000070283
– ident: ref39
  doi: 10.5194/bg-7-1877-2010
– ident: ref3
  doi: 10.1126/science.1186925
– ident: ref73
  doi: 10.1071/WF08016
– ident: ref20
  doi: 10.1038/ngeo443
– ident: ref82
  doi: 10.5194/acp-12-4365-2012
– ident: ref58
  doi: 10.1073/pnas.1003669107
– ident: ref61
  doi: 10.1046/j.1365-2699.2002.00677.x
– ident: ref34
  doi: 10.1016/S0079-1946(97)81142-1
– ident: ref10
  doi: 10.1111/j.1365-2699.2011.02595.x
– ident: ref43
  doi: 10.5194/acp-10-7017-2010
– ident: ref79
  doi: 10.5194/acp-11-3611-2011
– ident: ref47
  doi: 10.1016/j.quascirev.2012.11.029
– ident: ref57
  doi: 10.2307/1932179
– ident: ref72
  doi: 10.1029/2005JD006338
– ident: ref6
  doi: 10.1016/j.rse.2011.05.025
– ident: ref51
  doi: 10.1038/440436a
– ident: ref21
  doi: 10.1016/j.rse.2009.08.016
– ident: ref16
  doi: 10.1016/j.gloplacha.2007.08.005
– ident: ref63
  doi: 10.1029/1999GB900046
– ident: ref33
  doi: 10.5194/gmd-3-445-2010
– ident: ref37
  doi: 10.1073/pnas.0901970106
– ident: ref69
  doi: 10.1073/pnas.0604090103
– ident: ref53
  doi: 10.1016/j.quascirev.2010.10.010
– ident: ref55
  doi: 10.1038/19066
– ident: ref31
  doi: 10.1029/2007GB002961
– ident: ref19
  doi: 10.1126/science.1115193
– ident: ref80
– ident: ref83
  doi: 10.1029/2002GB001952
– ident: ref8
  doi: 10.1111/j.1365-2486.2008.01655.x
– ident: ref30
  doi: 10.1034/j.1600-0889.1999.00013.x
– ident: ref41
  doi: 10.5194/acp-5-417-2005
– ident: ref42
  doi: 10.1890/1051-0761(1999)009[0526:AYRAOC]2.0.CO;2
– ident: ref66
  doi: 10.1126/science.227.4682.53
– ident: ref2
  doi: 10.1029/2000GB001382
– ident: ref54
  doi: 10.1111/j.1365-2486.2005.00920.x
– ident: ref77
  doi: 10.1029/2007GB003122
– ident: ref23
  doi: 10.1016/j.rse.2008.10.006
– ident: ref17
  doi: 10.1890/100052
– ident: ref56
– ident: ref12
  doi: 10.1071/9780643096493
– ident: ref68
  doi: 10.1071/WF07011
– ident: ref27
  doi: 10.1126/science.1086112
– ident: ref29
  doi: 10.5194/acp-11-4705-2011
– ident: ref62
  doi: 10.1126/science.1199809
– ident: ref32
  doi: 10.1029/2009GL040000
– ident: ref49
  doi: 10.1016/j.atmosenv.2010.01.011
– ident: ref11
  doi: 10.1098/rstb.2006.1980
– ident: ref59
  doi: 10.1007/s00382-007-0334-x
– ident: ref44
  doi: 10.1034/j.1600-0889.1990.00009.x
– ident: ref65
  doi: 10.1016/j.rse.2005.04.007
– ident: ref74
  doi: 10.1029/2004GB002278
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Snippet Recent studies based on trace gas mixing ratios in ice cores and charcoal data indicate that biomass burning emissions over the past millennium exceeded...
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StartPage 289
SubjectTerms 20th-century
amazonian forests
carbon
climate
land-use
model tm5
past 2 millennia
rain-forest fires
southern africa
trace gases
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Title What could have caused pre-industrial biomass burning emissions to exceed current rates?
URI https://www.proquest.com/docview/1315213391
https://www.proquest.com/docview/1323815143
http://www.narcis.nl/publication/RecordID/oai:library.wur.nl:wurpubs%2F444542
https://doaj.org/article/2ee678ab17d5471b9794f96ca1e4e9ed
Volume 9
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