### Abstract

The effect of a finite density scale height on steady quasi-geostrophic flow over an isolated mountain is examined using analytic solutions for an isothermal, uniformly stratified, vertically semi-infinite atmosphere on an f-plane. A nondimensional measure of the depth of flow and hence of the importance of the vertical density variations of the basic state is the ratio of the Rossby height of the flow to the density scale height. It is found that the mountain-induced surface anticyclone is stronger for a deep flow than for a shallow one. Unlike the shallow case, no region of cyclonic vorticity is generated. The enhanced response for deep flow decreases the critical mountain height necessary for the formation of a stagnation point (eg Taylor cone). This critical height decreases with decreasing scale height and with increasing stratification. In addition, the mountain's influence decays less rapidly with height for deep flow. The far-field response for the deep case exhibits a circulation consistent with the lift force acting on the mountain. - from Author

Original language | English (US) |
---|---|

Pages (from-to) | 162-169 |

Number of pages | 8 |

Journal | Tellus, Series A |

Volume | 38 A |

Issue number | 2 |

State | Published - Jan 1 1986 |

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### All Science Journal Classification (ASJC) codes

- Oceanography
- Atmospheric Science

### Cite this

*Tellus, Series A*,

*38 A*(2), 162-169.

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*Tellus, Series A*, vol. 38 A, no. 2, pp. 162-169.

**Deep and shallow quasi-geostrophic flow over mountains.** / Bannon, Peter R.

Research output: Contribution to journal › Article

TY - JOUR

T1 - Deep and shallow quasi-geostrophic flow over mountains.

AU - Bannon, Peter R.

PY - 1986/1/1

Y1 - 1986/1/1

N2 - The effect of a finite density scale height on steady quasi-geostrophic flow over an isolated mountain is examined using analytic solutions for an isothermal, uniformly stratified, vertically semi-infinite atmosphere on an f-plane. A nondimensional measure of the depth of flow and hence of the importance of the vertical density variations of the basic state is the ratio of the Rossby height of the flow to the density scale height. It is found that the mountain-induced surface anticyclone is stronger for a deep flow than for a shallow one. Unlike the shallow case, no region of cyclonic vorticity is generated. The enhanced response for deep flow decreases the critical mountain height necessary for the formation of a stagnation point (eg Taylor cone). This critical height decreases with decreasing scale height and with increasing stratification. In addition, the mountain's influence decays less rapidly with height for deep flow. The far-field response for the deep case exhibits a circulation consistent with the lift force acting on the mountain. - from Author

AB - The effect of a finite density scale height on steady quasi-geostrophic flow over an isolated mountain is examined using analytic solutions for an isothermal, uniformly stratified, vertically semi-infinite atmosphere on an f-plane. A nondimensional measure of the depth of flow and hence of the importance of the vertical density variations of the basic state is the ratio of the Rossby height of the flow to the density scale height. It is found that the mountain-induced surface anticyclone is stronger for a deep flow than for a shallow one. Unlike the shallow case, no region of cyclonic vorticity is generated. The enhanced response for deep flow decreases the critical mountain height necessary for the formation of a stagnation point (eg Taylor cone). This critical height decreases with decreasing scale height and with increasing stratification. In addition, the mountain's influence decays less rapidly with height for deep flow. The far-field response for the deep case exhibits a circulation consistent with the lift force acting on the mountain. - from Author

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M3 - Article

AN - SCOPUS:0022848074

VL - 38 A

SP - 162

EP - 169

JO - Tellus, Series A: Dynamic Meteorology and Oceanography

JF - Tellus, Series A: Dynamic Meteorology and Oceanography

SN - 0280-6495

IS - 2

ER -