Add to ORKGThe effects of Fourier components of cross-stream topographic slope are included in the classical linear theory of quasigeostrophic baroclinic instability. The effect of uniformly sloping topography is reviewed, emphasis being placed on the possibility of destabilization through interaction between long topographic baroclinic Rossby waves and short thermal baroclinic Rossby waves with the same downstream wave number and phase speed...
Barotropic current rectification by topographic irregularities is treated for a case with bottom fri...
The two-layer baroclinic instability model of the California Undercurrent from Mysak (1977) is modif...
The two-layer baroclinic instability model of the California Undercurrent from Mysak (1977) is modif...
A simple analysis shows the analogy between Rossby waves and waves caused by irregularities in the d...
Observations and numerical experiments that suggest that sea-floor roughness can enhance the ratio o...
This thesis examines the generalization of the classical quasigeostrophic baroclinic linear-stabilit...
This thesis examines the generalization of the classical quasigeostrophic baroclinic linear-stabilit...
This thesis examines the generalization of the classical quasigeostrophic baroclinic linear-stabilit...
This paper examines the interaction between continuously stratified horizontal shear flow and topogr...
As a sequel to Schmitz and Hogg (1978), nine-month moored observations of current and temperature fr...
The influence of bottom topography on the westward propagation of long, baroclinic Rossby waves is s...
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Meteorology, 1979.Vita.Bibliography:...
Author Posting. © Sears Foundation for Marine Research, 2016. This article is posted here by permis...
A study has been made of steady barotropic flows on the β plane over a bottom topography that varies...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary S...
Barotropic current rectification by topographic irregularities is treated for a case with bottom fri...
The two-layer baroclinic instability model of the California Undercurrent from Mysak (1977) is modif...
The two-layer baroclinic instability model of the California Undercurrent from Mysak (1977) is modif...
A simple analysis shows the analogy between Rossby waves and waves caused by irregularities in the d...
Observations and numerical experiments that suggest that sea-floor roughness can enhance the ratio o...
This thesis examines the generalization of the classical quasigeostrophic baroclinic linear-stabilit...
This thesis examines the generalization of the classical quasigeostrophic baroclinic linear-stabilit...
This thesis examines the generalization of the classical quasigeostrophic baroclinic linear-stabilit...
This paper examines the interaction between continuously stratified horizontal shear flow and topogr...
As a sequel to Schmitz and Hogg (1978), nine-month moored observations of current and temperature fr...
The influence of bottom topography on the westward propagation of long, baroclinic Rossby waves is s...
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Meteorology, 1979.Vita.Bibliography:...
Author Posting. © Sears Foundation for Marine Research, 2016. This article is posted here by permis...
A study has been made of steady barotropic flows on the β plane over a bottom topography that varies...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary S...
Barotropic current rectification by topographic irregularities is treated for a case with bottom fri...
The two-layer baroclinic instability model of the California Undercurrent from Mysak (1977) is modif...
The two-layer baroclinic instability model of the California Undercurrent from Mysak (1977) is modif...