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www.clim-past-discuss.net/6/2177/2010/
doi:10.5194/cpd-6-2177-2010
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under the Creative Commons Attribution 3.0 License.
Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation?
1Department of Geosciences, University of Bremen, 28334 Bremen, Germany
2MARUM–Center for Marine Environmental Sciences, University Bremen, 28334 Bremen, Germany
Abstract. Instrumental records of North Atlantic sea surface temperature reveal a large-scale low frequency mode of variability that has become known as the Atlantic Multidecadal Oscillation (AMO). Proxy and modelling studies have demonstrated the important consequences of the AMO on other components of the climate system both within and outside the Atlantic region. Over longer time scales the past behavior of the AMO is predominantly constrained by terrestrial proxies and only a limited number of records are available from the marine realm itself. Here we use an Earth System-Climate Model of intermediate complexity to simulate AMO-type behavior in the Atlantic with a specific focus placed on the ability of ocean paleothermometers to capture the associated surface and subsurface temperature variability. Given their lower prediction errors and annual resolution, coral-based proxies of sea surface temperature appear to be capable of reconstructing the temperature variations associated with the past AMO with an adequate signal-to-noise ratio. Contrastingly, the relatively high prediction error and low temporal resolution of sediment-based proxies, such as the composition of foraminiferal calcite, limits their ability to produce interpretable records of past temperature anomalies corresponding to AMO activity.
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Notice on Discussion StatusCitation: Heslop, D. and Paul, A.: Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation?, Clim. Past Discuss., 6, 2177-2197, doi:10.5194/cpd-6-2177-2010, 2010. Bibtex EndNote Reference Manager XML
