Influence of the Gulf Stream on the troposphere

By S. Minobe, A. Kuwano‐Yoshida, N. Komori, Shang-Ping Xie, R. Small. Nature, 2008

735 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/8e263c204b9754ce6a055bffceadbefb8bf9f96f

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Citations in the corpus

Structure and dynamics of decadal anomalies in the wintertime midlatitude North Pacific ocean–atmosphere system (2016, methodology): “In recent years, observational studies with high-resolution satellite data (Nakamura et al. 2004; Small et al. 2008) and numerical studies with high-resolution GCM (Minobe et al. 2008; Taguchi et al. 2009; Sampe et al. 2010; Czaja and Blunt 2011; Feliks et al. 2004, 2007, 2011) have shown that the S”
A Coupled Decadal Prediction of the Dynamic State of the Kuroshio Extension System (2014, neutral): “1c) (Hoskins and Valdes 1990; Nakamura et al. 2004; Minobe et al. 2008; Joyce et al. 2009; Tokinaga et al. 2009; Taguchi et al. 2009; Kwon et al. 2010).”
Improved Atlantic winter blocking in a climate model (2011, background): “[15] Several mechanisms exist by which Atlantic SST affects the atmosphere: stronger ocean–atmosphere coupling occurs at higher model resolution [Minobe et al., 2008] and surface baroclinicity, thermal winds and baroclinic eddy growth are all affected by Atlantic SST [Brayshaw et al., 2009].”
Importance of Resolving Kuroshio Front and Eddy Influence in Simulating the North Pacific Storm Track (2017, background): “2a) and is associated with a strong surface convergence along the front (Minobe et al. 2008).”
Resolving and Parameterising the Ocean Mesoscale in Earth System Models (2020, background): “sea surface temperatures (SSTs) affect atmospheric circulation and precipitation [3], ocean circulation [4] and biogeochemistry [5] determine the flux of carbon between the oceanic and atmospheric reservoirs, and upper ocean temperatures and circulation influence sea ice properties and dynamics, whi”
What is the current state of scientific knowledge with regard to seasonal and decadal forecasting? (2012, background): “This is a key area of research for decadal predictions, although there is some evidence that the atmosphere is more strongly coupled to the ocean in higher resolution models (e.g. Minobe et al 2008).”
Modulation of Wind-Work by Oceanic Current Interaction with the Atmosphere (2016, methodology): “The ocean feedback to the atmosphere has been recently studied, mainly focusing on the thermal feedback (e.g., Chelton et al. 2004, 2007; Spall 2007; Perlin et al. 2007, 2011; Minobe et al. 2008; Jin et al. 2009; Park et al. 2006; Cornillon and Park 2001).”
Air–sea interaction over ocean fronts and eddies (2008, background): “The surface flux changes that occur across the ocean fronts appear to help the growth of storms and/or steer developing storms (Kuo et al., 1991; Xie et al., 2002; Businger et al., 2005; Sampe, 2005; Minobe et al., 2008).”
Influence of the Gulf Stream on the Barents Sea ice retreat and Eurasian coldness during early winter (2014, background): “It has been investigated whether the sharp SST gradient over the Gulf Stream has great impact on tropospheric circulation through diabatic heating over the surface wind convergence zone (Minobe et al 2008).”
Coupled ocean-atmosphere interaction at oceanic mesoscales (2010, background): “Numerical simulations of crossfrontal winds over the Gulf Stream suggest the importance of secondary circulations and atmospheric pressure adjustment (Wai and Stage, 1989; Warner et al., 1990; Song et al., 2006; Minobe et al., 2008, 2010).”