A modelling and observational study of the relationship between sea surface temperature in the North‐West atlantic and the atmospheric general circulation

By Tim N. Palmer, Zhaobo Sun. 2007

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Structure and dynamics of decadal anomalies in the wintertime midlatitude North Pacific ocean–atmosphere system (2016, background): “Some of those responses are barotropic, with atmospheric high pressure over warm oceanic surface, as in observation (Palmer and Sun 1985; Latif and Barnett 1994, 1996; Peng et al. 1995, 1997), or with atmospheric low pressure over warm oceanic surface (Picther et al.”
A mechanism for lagged North Atlantic climate response to solar variability (2013, background): “…studies of observed climate [Ratcliffe and Murray, 1970; Rodwell and Folland, 2003] and modelling studies with prescribed ocean conditions [Palmer and Sun, 1985; Rodwell et al., 1999; Peng et al., 2002; Sutton et al., 2001; Cassou et al., 2007; Keeley et al., 2012] demonstrate atmospheric…”
An Observed Connection between the North Atlantic Oscillation and the Madden-Julian Oscillation (2009, background): “Candidates include the forcing from the underlying sea surface temperature (SST) anomaly in the extratropical North Atlantic (e.g., Palmer and Sun 1985; Peng and Whitaker 1999), coupling with the stratosphere (e.g., Baldwin et al. 2003), and interaction with the snow cover in Eurasia (e.g., Cohen…”