Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/8642
Title: Low atmospheric CO2 levels during the Little Ice Age due to cooling-induced terrestrial uptake
Authors: Rubino, M
Etheridge, DM
Trudinger, CM
Allison, CE
Rayner, PJ
Enting, I
Mulvaney, R
Steele, LP
Langenfelds, RL
Sturges, WT
Curran, MAJ
Smith, AM
Keywords: Ice
Terrestrial ecosystems
Atmospheres
Carbon dioxie
Carbon oxysulfide
Climates
Issue Date: 25-Jul-2016
Publisher: Springer Nature
Citation: Rubino, M., Etheridge, D. M., Trudinger, C. M., Allison, C. E., Rayner, P. J., Enting, I., Mulvaney, 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. doi:10.1038/ngeo2769
Abstract: 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 uncertainties. © 2016, Nature Publishing Group.
Gov't Doc #: 7460
URI: https://doi.org/10.1038/ngeo2769
http://apo.ansto.gov.au/dspace/handle/10238/8642
ISSN: 1752-0908
Appears in Collections:Journal Articles

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