Pages that link to "Item:Q4277875"
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The following pages link to Nonlinear stability of intermediate baroclinic flow on a sloping bottom (Q4277875):
Displaying 13 items.
- Nonlinear stability of one-layer geostrophic fronts (Q1816824) (← links)
- Nonlinear phenomena in ocean dynamics. Special issue originating from the 15th annual international conference of the Center for Nonlinear Studies, Los Alamos, NM, USA, May 15--19, 1995 (Q1816890) (← links)
- A note on the stability theory of buoyancy-driven ocean currents over a sloping bottom (Q1909917) (← links)
- Note on the nonlinear stability of equivalent barotropic flows (Q1965347) (← links)
- Coherent structures of nonlinear barotropic-baroclinic interaction in unequal depth two-layer model (Q2243333) (← links)
- A unified asymptotic derivation of two-layer, frontal geostrophic models including planetary sphericity and variable topography (Q3543813) (← links)
- Sub–inertial dynamics of density–driven flows in a continuously stratified fluid on a sloping bottom. II. Isolated eddies and radiating cold domes (Q4262194) (← links)
- On the baroclinic dynamics, hamiltonian formulation and general stability characteristics of density-driven surface currents and fronts over a sloping continental shelf (Q4301204) (← links)
- Nonlinear Stability of Baroclinic Fronts in a Channel with Variable Topography (Q4890199) (← links)
- Baroclinic instability of axially symmetric flow over sloping bathymetry (Q4976694) (← links)
- Finite-amplitude baroclinic instability of a mesoscale gravity current in a channel (Q5187794) (← links)
- Ekman destabilization of inertially stable baroclinic abyssal flow on a sloping bottom (Q5304760) (← links)
- On the collision between deep anticyclones and seamounts (Q5950216) (← links)
