## Abstract

A numerical study of stably stratified flow over a three-dimensional hill is presented. Large-eddy simulation is used here to examine in detail the laboratory experimental flows described in the landmark work of Hunt and Snyder about stratified flow over a hill. The flow is linearly stratified and ∞/N h is varied from 0.2 to 1.0. Here N and ∞ are the buoyancy frequency and freestream velocity respectively, and h is the height of the hill. The Reynolds number based on the hill height is varied from 365 to 2968. The characteristic flow patterns at various values of ∞/ N h have been obtained and they are in good agreement with earlier theoretical and experimental results. It is shown that the flow field cannot be predicted by Drazin's theory when recirculation exists at the leeside of the hill even at ∞/ N h ≪ 1. The wake structure agrees well with a two-dimensional wake assumption when ∞/ N h ≪ 1 but lee waves start to influence the wake structure as ∞/N h increases. The dividing-streamline heights obtained in the simulation are in accordance with experimental results and Sheppard's formula. The energy loss along the dividing streamline due to friction/turbulence approximately offsets the energy gained from pressure field. When lee waves are present, linear theory always underestimates the amplitude and overestimates the wavelength of three-dimensional lee waves. The simulated variations of drag coefficients with the parameter K (= N D / ∏ U ∞) are qualitatively consistent with experimental data and linear theory. Here D is the depth of the tank.

Original language | English (US) |
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Pages (from-to) | 81-114 |

Number of pages | 34 |

Journal | Boundary-Layer Meteorology |

Volume | 107 |

Issue number | 1 |

DOIs | |

State | Published - Apr 2003 |

Externally published | Yes |

## Keywords

- Dividing streamline
- Drag
- Hill
- Large-eddy simulation
- Lee waves
- Stratified flow

## ASJC Scopus subject areas

- Atmospheric Science