Kuroshio Extension variability and forcing of the Pacific Decadal Oscillations
By B. Qiu. 2003
187 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/5314a072a3e16497e2c4cbbaefce386a1aba2a91
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
- William Dewar
- A. Treguier
- Shang-Ping Xie
In Global and Planetary Change
- N. Schneider
- Bunmei Taguchi
- B. Qiu
- L. Ceballos
- C. Hoyos
- Emanuele Di Lorenzo
- Shang-Ping Xie
- Shuiming Chen
In Oceanography
- N. Schneider
- Bunmei Taguchi
- B. Qiu
- L. Ceballos
- C. Hoyos
- Emanuele Di Lorenzo
- Shang-Ping Xie
- Shuiming Chen
Citations in the corpus
- Decadal Variability of the Kuroshio Extension: Observations and an Eddy-Resolving Model Hindcast* (2006, background): “From 11-yr-long satellite SSH data, Qiu (2003) found decadal modulations in the KE jet’s intensity.”
- 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.”
- Sea Level Expression of Intrinsic and Forced Ocean Variabilities at Interannual Time Scales (2011, background): “For instance, the Kuroshio undergoes realistic interannual variability patterns both in wind-driven laminar models (Qiu 2003) and in constantly forced eddying models (Pierini 2006); Taguchi et al. (2007) suggests from more realistic simulations that the observed variability arises from the…”
- A Coupled Decadal Prediction of the Dynamic State of the Kuroshio Extension System (2014, background): “The first approach takes advantage of the facts that the SSH adjustment in themidlatitude ocean is via baroclinic Rossby waves and that the low-frequency wind forcing in the North Pacific has its center of action in the eastern part of the basin (Qiu 2003).”