Interdecadal Thermocline Variability in the North Pacific for 1958–97: A GCM Simulation*

By Shang-Ping Xie, T. Kunitani, Atsushi Kubokawa, M. Nonaka, S. Hosoda. 2000

169 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/2df0238a1f257591d29b503143591ebec287a3ae

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Citations in the corpus

Satellite Observations of Cool Ocean–Atmosphere Interaction (2004, background): “The deep winter mixed layer there allows the ocean memory of past wind changes to have a marked effect on SST (Xie et al. 2000) by the Rossby wave (Schneider and Miller 2001) or gyre-boundary adjustment mechanism (Seager et al. 2001).”
Kuroshio Extension variability and forcing of the Pacific Decadal Oscillations (2003, background): “Evidence supporting this notion can be found in recent upper-ocean heat budget studies for the Kuroshio Extension region by Qiu (2000), Xie et al. (2001) , and Vivier et al. (2002).”
Decadal Variability of the Kuroshio Extension: Observations and an Eddy-Resolving Model Hindcast* (2006, background): “The Kuroshio–Oyashio Extension (KOE) region, including the KE and the Oyashio subarctic front, has recently been identified as the window in which subsurface ocean variability strongly affects sea surface temperature (SST; Xie et al. 2000).”
Wind-Driven Shifts in the Latitude of the Kuroshio–Oyashio Extension and Generation of SST Anomalies on Decadal Timescales* (2001, background): “The dominance of the locally forced anomalous Ekman drift in the central Pacific is also a result common to our model and those of SMP and Xie et al. (2000).”
The Forcing of the Pacific Decadal Oscillation (2005, background): “…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 et al. 2000; Miller and Schneider 2000; Seager et al. 2001; Schneider et al. 2002; Qiu 2003).”
Anatomy of North Pacific Decadal Variability (2002, background): “…caused temperature anomalies in the Kuroshio– Oyashio extension (KOE) region (Miller and Schneider 2000) that could not be explained by contemporaneous local atmospheric forcing (Xie et al. 2000) and were independent of contemporaneous SST variation in the central Pacific (Nakamura et al. 1997).”