Sea surface temperature variability: patterns and mechanisms.

By C. Deser, M. Alexander, Shang-Ping Xie, A. Phillips. Annual Review of Marine Science, 2010

1,069 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/e618531c0153ee829e612e7790463c937bceb4c6

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Citations in the corpus

A delayed oscillator model for the quasi-periodic multidecadal variability of the NAO (2015, neutral): “Moreover, the imaginary part is reminiscent of the well-known North Atlantic SST tripole (Visbeck et al. 2003, and references therein; Deser et al. 2010).”
Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, methodology): “…estimates of the separation into externally and internally forced components, indicating uncertainties in the assumptions used to estimate the externally forced signal [Delworth et al., 2007; Ting et al., 2009; Deser et al., 2010; Mann et al., 2014] and potentially nonlinearities in the system.”
Towards multi-resolution global climate modeling with ECHAM6–FESOM. Part I: model formulation and mean climate (2015, background): “The AMO is usually diagnosed as a simple SST index of areaaveraged anomalies in the North Atlantic region between 0◦ –70◦ N (Deser et al. 2010).”
Low-Cloud Feedbacks from Cloud-Controlling Factors: A Review (2017, background): “In tropical subsidence regions, both inter-annual variability in SST (1–2 K * two standard deviations, Deser et al. 2010) and the amplitude of its seasonal cycle (2–4 K, Shea et al. 1992) are generally comparable in magnitude to the 2–3 K increases typical of a response to CO2 doubling.”
NAO implicated as a predictor of Northern Hemisphere mean temperature multidecadal variability (2013, positive): “The NHT response to the interannual NAO variability is modeled by the Hasselmann climate model [ Hasselmann , 1976; Thompson et al. , 2009; Deser et al. , 2010] as follows where T NAO denotes the simulated response of NHT to interannual NAO variability, C is the estimated effective heat capacity of…”
Atmospheric circulation patterns which promote winter Arctic sea ice decline (2017, background): “As noted by Czaja and Frankignoul (2002), Deser et al (2010) and Gastineau and Frankignoul (2015) the NAO has an imprint on the SST in the North Atlantic midlatitudes on interannual and decadal timescales and the NAOþ can correspond to high SST near the GSE region due to the wind stress forcing…”
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).”
SEAS5: the new ECMWF seasonal forecast system (2018, background): “ECMWF already had high skill in forecasting ENSO compared to other stateof-the-art seasonal forecast models, especially in the boreal spring and summer months that are more difficult to forecast (Barnston et al., 2012; Molteni et al., 2011).”
Drivers of exceptionally cold North Atlantic Ocean temperatures and their link to the 2015 European heat wave (2016, neutral): “The heat budget for the upper-ocean mixed layermay bewritten as (Deser et al 2010) ( ) ( )( ) ( ) r = + + ⋅ + + -”