Basic concepts
Climate variability diagnosed in spherical coordinates
Climate variability diagnosed in z-coordinate
External/internal modes in meridional/zonal directions
Adiabatic signals in the upper ocean
The regulation of MOC (MHF) by wind stress and buoyancy anomaly
Adiabatic Heaving signals in the deep ocean
Heaving, stretching, spicing and isopycnal analysis
Heaving, stretching and spicing modes
Potential Spicity
Sigma-pi diagram and its application
Isopycnal analysis
Heaving modes in the world oceans
Heaving induced by wind stress anomaly
Heaving induced by anomalous freshwater forcing
Heaving induced by anomalous wind, freshening and warming
Heaving induced by convection generated gravity anomaly
Heaving induced by deep convection generated volume loss
ENSO events and heaving modes
Heaving signals in the isopycnal coordinate
Introduction
Coordinate transformation by the casting method
Coordinate transformation by the projecting method
Difference between the casting method and the projecting method
Isopycnal layer analysis for the world oceans
Isopycnal layer analysis based on
Heaving signals for the shallow water in the Pacific-Indian basin
Heaving signal propagation through the equatorial sections
Heaving signals in the isothermal coordinate
Introduction
Casting method
Casting method applied to the GODAS data
Projecting method
Signal of layer depth and zonal velocity in the Pacific basin
Z-theta diagram and its application to climate variability analysis
Climate signals in the salinity coordinates
Introduction
Casting method
Separating the signals into external and internal modes
Analysis based on the GODAS data
Shallow salty water sphere in the Atlantic Ocean.