Can oceanic paleothermometers reconstruct the Atlantic Multidecadal Oscillation?
Instrumental records of the 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...[Show more]
|Collections||ANU Research Publications|
|Source:||Climate of the Past|
|01_Heslop_Can_oceanic_paleothermometers_2011.pdf||376.77 kB||Adobe PDF|
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