The effects of optimal initial error on the short-range prediction of transition processes between the Kuroshio Extension (KE) bimodalities are analyzed using a reduced-gravity shallow-water model and the singular vector (SV) approach. Emphasis is placed on the spatial structures, growing processes, and effects of the SVs. The results show that the large values of the SVs are mainly located in the first crest region of the KE (around 35°N, 144°E) and in the Kuroshio large meander (KLM) region south of Japan (around 32°N, 139.5°E). The fast growths of the SVs have important impacts on the prediction of transition of the KE bimodality. The initial error with +SV pattern (with positive anomalies in the first crest region of the KE and nega...
Altimetry data from the first 7-yr TOPEX/Poseidon (T/P) mission (October 1992–September 1999) are an...
The atmosphere is a chaotic dynamical system, small errors in the initial condition of an atmospheri...
Through analysis of a hindcast integration of an eddy-resolving quasi-global ocean general circulati...
In this study, the predictability of the Kuroshio Extension (KE) transition processes is explored fr...
In this study, the initial perturbations that are the easiest to trigger the Kuroshio Extension (KE)...
In this paper, sequential importance sampling is used to assess the impact of observations on an ens...
For large dynamical systems, the evolution of a small initial perturbation is often examined in term...
The Kuroshio Current, a mid-latitude western boundary current in the North Pacific, is the main tran...
Small meanders of the Kuroshio Extension (KE) were examined in the three vessel simultaneous observa...
Being the extension of a wind-driven western boundary current, the Kuroshio Extension (KE) has long ...
Investigations of the intrinsic low-frequency variability and predictability of the Kuroshio Curren...
The Kuroshio Extension (KE) plays an important role in climate and environmental change in the North...
We propose a non-linear forcing singular vector (NFSV) approach to infer the effect of non-linearity...
The Kuroshio Extension (KE) is the eastward-flowing, free, inertial meandering jet formed by the con...
In 2004 an array of current and pressure recording inverted echo sounders was deployed within the Ku...
Altimetry data from the first 7-yr TOPEX/Poseidon (T/P) mission (October 1992–September 1999) are an...
The atmosphere is a chaotic dynamical system, small errors in the initial condition of an atmospheri...
Through analysis of a hindcast integration of an eddy-resolving quasi-global ocean general circulati...
In this study, the predictability of the Kuroshio Extension (KE) transition processes is explored fr...
In this study, the initial perturbations that are the easiest to trigger the Kuroshio Extension (KE)...
In this paper, sequential importance sampling is used to assess the impact of observations on an ens...
For large dynamical systems, the evolution of a small initial perturbation is often examined in term...
The Kuroshio Current, a mid-latitude western boundary current in the North Pacific, is the main tran...
Small meanders of the Kuroshio Extension (KE) were examined in the three vessel simultaneous observa...
Being the extension of a wind-driven western boundary current, the Kuroshio Extension (KE) has long ...
Investigations of the intrinsic low-frequency variability and predictability of the Kuroshio Curren...
The Kuroshio Extension (KE) plays an important role in climate and environmental change in the North...
We propose a non-linear forcing singular vector (NFSV) approach to infer the effect of non-linearity...
The Kuroshio Extension (KE) is the eastward-flowing, free, inertial meandering jet formed by the con...
In 2004 an array of current and pressure recording inverted echo sounders was deployed within the Ku...
Altimetry data from the first 7-yr TOPEX/Poseidon (T/P) mission (October 1992–September 1999) are an...
The atmosphere is a chaotic dynamical system, small errors in the initial condition of an atmospheri...
Through analysis of a hindcast integration of an eddy-resolving quasi-global ocean general circulati...