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List of works by Bunmei Taguchi

Atmospheric sounding over the winter Kuroshio Extension: Effect of surface stability on atmospheric boundary layer structure

article

Baiu Rainband Termination in Atmospheric and Coupled Atmosphere–Ocean Models

Decadal Variability of the Kuroshio Extension: Observations and an Eddy-Resolving Model Hindcast*

article

Decadal variability of the Kuroshio Extension: mesoscale eddies and recirculations

article by Bunmei Taguchi et al published 16 May 2010 in Ocean Dynamics

East Pacific ocean eddies and their relationship to subseasonal variability in Central American wind jets

scholarly article

How potentially predictable are midlatitude ocean currents?

scientific article published on February 2016

Influences of the Kuroshio/Oyashio Extensions on Air–Sea Heat Exchanges and Storm-Track Activity as Revealed in Regional Atmospheric Model Simulations for the 2003/04 Cold Season*

article

Interannual variations of the Hawaiian Lee Countercurrent induced by potential vorticity variability in the subsurface

Intraseasonal variability in sea surface height over the South China Sea

scholarly article

Large-scale climate control of zooplankton transport and biogeography in the Kuroshio-Oyashio Extension region

scholarly article by Sanae Chiba et al published 8 October 2013 in Geophysical Research Letters

North Pacific Gyre Oscillation Synchronizes Climate Fluctuations in the Eastern and Western Boundary Systems*

Oceanic moisture sources contributing to wintertime Euro-Atlantic blocking

scientific article published on 31 August 2021

On the triggering of Benguela Niños: Remote equatorial versus local influences

scholarly article

Publisher Correction: Reply to: Eurasian cooling in response to Arctic sea-ice loss is not proved by maximum covariance analysis

correction of a scholarly article

Reply to: Eurasian cooling in response to Arctic sea-ice loss is not proved by maximum covariance analysis

scientific article published in 2021

Seasonal variations of the Hawaiian Lee Countercurrent induced by the meridional migration of the trade winds

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