Decadal Variability of the Kuroshio Extension: Observations and an Eddy-Resolving Model Hindcast*
By Bunmei Taguchi, Shang-Ping Xie, N. Schneider, M. Nonaka, Hideharu Sasaki, Y. Sasai. 2006
273 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/34239e415e0d654d662f0c4817bac2261e88df83
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
- Bunmei Taguchi
- N. Schneider
- L. Ceballos
- C. Hoyos
- Emanuele Di Lorenzo
- Larry W. O'Neill
- R. Small
- William Dewar
In Global and Planetary Change
- Bunmei Taguchi
- N. Schneider
- L. Ceballos
- C. Hoyos
- Emanuele Di Lorenzo
- Larry W. O'Neill
- R. Small
- B. Qiu
In Oceanography
- Bunmei Taguchi
- N. Schneider
- L. Ceballos
- C. Hoyos
- Emanuele Di Lorenzo
- Larry W. O'Neill
- R. Small
- B. Qiu
Citations in the corpus
- A Coupled Decadal Prediction of the Dynamic State of the Kuroshio Extension System (2014, background): “This favorable comparison indicates that the OFES hindcast captured well the decadally modulating KE system, a result consistent with the findings of other recent studies analyzing theOFES hindcast output (Nonaka et al. 2006; Taguchi et al. 2007; Ceballos et al. 2009; Sasaki et al. 2013).”
- Sea Level Expression of Intrinsic and Forced Ocean Variabilities at Interannual Time Scales (2011, background): “10b, Taguchi et al. (2007) show in the Kuroshio Extension a ratio R*5sILF/s T LF that relates to our ratio R in a simple way: R; 100”
- North Pacific Gyre Oscillation Synchronizes Climate Fluctuations in the Eastern and Western Boundary Systems (2009, methodology): “Taguchi et al. (2007) isolate the KOE mode 2 and showed that it is associated with changes in the Kuroshio Extension’s strength, but did not provide any forcing mechanism.”
- Air–sea interaction over ocean fronts and eddies (2008, background): “From measurements at TAO moorings, Thum et al. (2002) showed that individual TIWs were associated with sensible and latent heat fluxes per ◦C of SST anomaly of around 4 W m−2 and 33 W m−2”