Historical Southern Hemisphere biomass burning variability inferred from ice core carbon monoxide records

Strawson, Ivo; Faïn, Xavier; Bauska, Thomas K. ORCID: https://orcid.org/0000-0003-1901-0367; Muschitiello, Francesco; Vladimirova, Diana O. ORCID: https://orcid.org/0000-0002-1678-0174; Tetzner, Dieter R. ORCID: https://orcid.org/0000-0001-7659-8799; Humby, Jack ORCID: https://orcid.org/0000-0003-0526-2766; Thomas, Elizabeth R. ORCID: https://orcid.org/0000-0002-3010-6493; Liu, Pengfei; Zhang, Bingqing; Grilli, Roberto; Rhodes, Rachael H.. 2024 Historical Southern Hemisphere biomass burning variability inferred from ice core carbon monoxide records. Proceedings of the National Academy of Sciences, 121 (33), e2402868121. 10.1073/pnas.2402868121

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Official URL: http://dx.doi.org/10.1073/pnas.2402868121

Abstract/Summary

Biomass burning plays an important role in climate-forcing and atmospheric chemistry. The drivers of fire activity over the past two centuries, however, are hotly debated and fueled by poor constraints on the magnitude and trends of preindustrial fire regimes. As a powerful tracer of biomass burning, reconstructions of paleoatmospheric carbon monoxide (CO) can provide valuable information on the evolution of fire activity across the preindustrial to industrial transition. Here too, however, significant disagreements between existing CO records currently allow for opposing fire histories. In this study, we reconstruct a continuous record of Antarctic ice core CO between 1821 and 1995 CE to overlap with direct atmospheric observations. Our record indicates that the Southern Hemisphere CO burden ([CO]) increased by 50% from a preindustrial mixing ratio of ca. 35 ppb to ca. 53 ppb by 1995 CE with more variability than allowed for by state-of-the-art chemistry-climate models, suggesting that historic CO dynamics have been not fully accounted for. Using a 6-troposphere box model, a 40 to 50% decrease in Southern Hemisphere biomass-burning emissions, coincident with unprecedented rates of early 20th century anthropogenic land-use change, is identified as a strong candidate for this mismatch.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1073/pnas.2402868121
ISSN:	0027-8424
Date made live:	06 Aug 2024 09:24 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/537803

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1073/pnas.2402868121

ISSN:

0027-8424

Date made live:

06 Aug 2024 09:24 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/537803