A Study of the Interaction of the North Atlantic Oscillation with Ocean Circulation

By John Marshall, H. Johnson, J. Goodman. 2001

400 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/02b1cba4453cfd7deb9e083d5590c446a0183309

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Citations in the corpus

Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “Interannual to decadal UOHC anomalies in the Gulf Stream region are forced by changes in ocean geostrophic advection and are damped by air-sea heat fluxes [Marshall et al., 2001a; Dong and Kelly, 2004; Dong et al., 2007; Zhai and Sheldon, 2012; Buckley et al., 2014a, 2015] (see Figure 7a).”
A delayed oscillator model for the quasi-periodic multidecadal variability of the NAO (2015, neutral): “Previous theoretical studies have also suggested that the feedback of ocean onto the NAO is critical for the NAO spectrum peak at the decadal frequency band (Marshall et al. 2001; Czaja and Marshall 2000).”
Kuroshio Extension variability and forcing of the Pacific Decadal Oscillations (2003, background): “Thus far, the proposed ocean processes include 1) limited resonance of the midlatitude baroclinic Rossby waves with basinwide stochastic wind forcing (e.g., Jin 1997), 2) delayed oscillation with the timescale of delay set by the adjustment of the wind-driven gyre or the thermohaline circulation (e.”
A Review of the Role of the Atlantic Meridional Overturning Circulation in Atlantic Multidecadal Variability and Associated Climate Impacts (2019, background): “319 sign in the subtropical region from that in the subpolar and tropical areas) induced by the NAO at interannual timescales (Cayan, 1992; Delworth et al., 2017; Deser et al., 2010; Kushnir, 1994; Marshall et al., 2001; Visbeck et al., 2003).”
Atmospheric GCM Response to Extratropical SST Anomalies: Synthesis and Evaluation* (2002, background): “Moreover, the search for the causes of decadal climate variability and for perplexing shifts and trends in key circulation indices, including that of ENSO, have fueled the debate over the role of the extratropical oceans in long-term climate variability (Latif and Barnett 1994, 1996; Gu and Philande”
Bi-decadal variability excited in the coupled ocean–atmosphere system by strong tropical volcanic eruptions (2012, background): “In particular, we focus on its two leading modes of variability: The first is the intergyre gyre component (IGG), i.e., the anomalous wind-driven circulation straddling the boundary between the subpolar and subtropical gyres which is thought to play an important role in the link between the NAO, the”
Response of the North Atlantic subpolar gyre to persistent North Atlantic oscillation like forcing (2009, methodology): “This spatial non-linearity is consistent with the findings from Marshall et al. (2001) using a simplified mathematical model.”
A decadal prediction case study: Late twentieth-century North Atlantic Ocean heat content (2012, background): “2c) and is generally understood to be the ocean signature of persistent positive NAO (NAO1) forcing in the years leading up to the shift (Marshall et al. 2001; Eden and Willebrand 2001; Lozier et al. 2008; Lohmann et al. 2009b; Lohmann et al. 2009a; Robson et al. 2012).”
The ocean's response to North Atlantic Oscillation variability (2013, methodology): “More recent studies [e.g. Cayan 1992a; Visbeck et al. 1998; Seager et al. 2000; Marshall et al. 2001a] correlated SST anomalies from the NCEP-NCAR reanalysis with the NAO index and reproduced a similar response pattern.”
Sea surface temperature variability: patterns and mechanisms. (2010, background): “…circulation anomalies and attendant changes in the turbulent and radiative energy fluxes at the air-sea interface and the local wind-driven Ekman currents (Cayan, 1992; Alexander and Scott, 1997; Deser and Timlin, 1997; Marshall et al., 2001; Visbeck et al., 2003; Alexander and Scott, 2008).”