Wind-Driven Shifts in the Latitude of the Kuroshio–Oyashio Extension and Generation of SST Anomalies on Decadal Timescales*

By R. Seager, Y. Kushnir, N. Naik, M. Cane, Jennifer Miller. 2001

248 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/e45f49fed5c436f3d9351e5c8d08ef9fd78832df

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Bunmei Taguchi
2. N. Schneider
3. Shang-Ping Xie
4. Gerrit Lohmann
5. Mihai O. Dima
6. Hisashi Nakamura
7. Y. Kushnir
8. R. Seager

In Global and Planetary Change

1. N. Schneider
2. Bunmei Taguchi
3. Shang-Ping Xie
4. Gerrit Lohmann
5. Mihai O. Dima
6. B. Qiu
7. Hisashi Nakamura
8. Y. Kushnir

In Oceanography

1. N. Schneider
2. Bunmei Taguchi
3. Shang-Ping Xie
4. Gerrit Lohmann
5. Mihai O. Dima
6. B. Qiu
7. Y. Kushnir
8. R. Seager

Citations in the corpus

• Decadal Variability of the Kuroshio Extension: Observations and an Eddy-Resolving Model Hindcast* (2006, methodology): “SST in the KE and Oyashio Extension (Latif and Barnett 1994; Xie et al. 2000; Qiu 2000; Seager et al. 2001; Schneider et al. 2002; Nonaka et al. 2006).”
• Kuroshio Extension variability and forcing of the Pacific Decadal Oscillations (2003, background): “The importance of meridional displacement of the subtropical‐subpolar gyre boundary in creating SST anomalies in the KOE region is also emphasized by Seager et al. (2001) in their hindcast modeling study of the decadal North Pacific SST variations.”
• Decadal Variability in the Kuroshio–Oyashio Extension Simulated in an Eddy-Resolving OGCM (2006, methodology): “the gyre boundary migration (Seager et al. 2001) and vertical thermocline displacement (e.”
• A Coupled Decadal Prediction of the Dynamic State of the Kuroshio Extension System (2014, background): “…the transitions between the stable and unstable states of the KE system has been explored extensively both observationally and based on ocean circulationmodels of various complexities (Miller et al. 1998; Seager et al. 2001; Schneider et al. 2002; Qiu 2003; Taguchi et al. 2007; Sasaki et al. 2013).”
• A hemispheric mechanism for the atlantic multidecadal oscillation (2007, background): “Further, through atmospheric teleconnections it is transmitted from the tropical Pacific to the North Pacific (Seager et al. 2001).”
• Atmospheric GCM Response to Extratropical SST Anomalies: Synthesis and Evaluation* (2002, background): “…changes in oceanic heat advection, reminiscent of phenomena associated with El Niño, was suggested by numerical simulations with ocean models (see Seager et al. 2001; and references therein) and spurred speculations regarding a new, predictable form of extratropical atmosphere–ocean interaction…”
• Mechanisms of Hemispherically Symmetric Climate Variability (2003, background): “The latter feature has been explained by the adjustment of the wind-driven ocean gyre circulation, which is quite different between the North Pacific and South Pacific (Schneider et al. 2002; Seager et al. 2001).”
• The Forcing of the Pacific Decadal Oscillation (2005, background): “The North Pacific atmosphere affects the surface heat budget via anomalies of surface fluxes and Ekman advection (Alexander 1992), and the excitation and propagation of Rossby waves that affect the upper ocean in the Kuroshio–Oyashio Extension (KOE) region (Miller et al. 1998; Deser et al. 1999; Xie”