Low atmospheric CO2 levels during the Little Ice Age due to cooling-induced terrestrial uptake

Rubino, M.; Etheridge, D. M.; Trudinger, C. M.; Allison, C. E.; Rayner, P. J.; Enting, I.; Mulvaney, R. ORCID: https://orcid.org/0000-0002-5372-8148; Steele, L. P.; Langenfelds, R. L.; Sturges, W. T.; Curran, M. A. J.; Smith, A. M.. 2016 Low atmospheric CO2 levels during the Little Ice Age due to cooling-induced terrestrial uptake. Nature Geoscience, 9 (9). 691-694. https://doi.org/10.1038/ngeo2769

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Official URL: http://dx.doi.org/10.1038/ngeo2769

Abstract/Summary

Low atmospheric carbon dioxide (CO2) concentration1 during the Little Ice Age has been used to derive the global carbon cycle sensitivity to temperature2. Recent evidence3 confirms earlier indications4 that the low CO2 was caused by increased terrestrial carbon storage. It remains unknown whether the terrestrial biosphere responded to temperature variations, or there was vegetation re-growth on abandoned farmland5. Here we present a global numerical simulation of atmospheric carbonyl sulfide concentrations in the pre-industrial period. Carbonyl sulfide concentration is linked to changes in gross primary production6 and shows a positive anomaly7 during the Little Ice Age. We show that a decrease in gross primary production and a larger decrease in ecosystem respiration is the most likely explanation for the decrease in atmospheric CO2 and increase in atmospheric carbonyl sulfide concentrations. Therefore, temperature change, not vegetation re-growth, was the main cause of the increased terrestrial carbon storage. We address the inconsistency between ice-core CO2 records from different sites8 measuring CO2 and δ13CO2 in ice from Dronning Maud Land (Antarctica). Our interpretation allows us to derive the temperature sensitivity of pre-industrial CO2 fluxes for the terrestrial biosphere (γL = −10 to −90 Pg C K−1), implying a positive climate feedback and providing a benchmark to reduce model uncertainties9.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1038/ngeo2769
Programmes:	BAS Programmes > BAS Programmes 2015 > Ice Dynamics and Palaeoclimate
ISSN:	1752-0894
Additional Keywords:	carbon cycle, palaeoclimate
Date made live:	24 Oct 2016 09:59 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/514895

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1038/ngeo2769

Programmes:

BAS Programmes > BAS Programmes 2015 > Ice Dynamics and Palaeoclimate

ISSN:

1752-0894

Additional Keywords:

carbon cycle, palaeoclimate

Date made live:

24 Oct 2016 09:59 +0 (UTC)