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Ailie J. E. Gallant, Steven J. Phipps, David J. Karoly, A. Brett Mullan, and Andrew M. Lorrey

patterns associated with the localized variability in paleoclimate proxies. For example, circulation-based approaches using multiproxy networks and regional climate regime classification can be used to investigate teleconnection patterns ( Lorrey et al. 2007 , 2008 , 2012 ). Subsequently, the role of the remote climate driver as a regulator of unique circulation patterns can be established and linked to remote paleoclimate proxy variability, ideally with guidance from dynamical climate models so that

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Michelle Ho, Danielle C. Verdon-Kidd, Anthony S. Kiem, and Russell N. Drysdale

winter rainfall. The climate in both catchments ranges from temperate in the east to arid in the west ( Peel et al. 2007 ). Both are seasonally influenced to varying degrees by large-scale climate drivers such as ENSO, IOD, and SAM ( Verdon and Franks 2005 ; Meneghini et al. 2007 ; Risbey et al. 2009 ). The Wimmera catchment was chosen to represent the southern MDB (winter-dominated rainfall regime), where the climate is primarily influenced by SAM processes originating from the Southern Ocean

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