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Journal ArticleDOI

Numerical Simulation of Mesoscale Eddies over Melbourne

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TLDR
In this article, a mesoscale wind field model was used to simulate a cyclonic nocturnal eddy which may form over Melbourne under stable conditions with light synoptic winds.
Abstract
A mesoscale wind field model is used to simulate a cyclonic nocturnal eddy which may form over Melbourne under stable conditions with light synoptic winds. Two types of eddy (Mel-I and Mel-II) are identified, with separate formation mechanisms. Mel-I is generated by vorticity shed from the upstream mountain ranges. Daytime anabatic effects enhance the strength of the eddy. When surface heat fluxes are suppressed, the numerical simulations are found to parallel previous to laboratory experiments, but with a somewhat relaxed Froude number formation criterion. The second type of eddy, Mel-II, is generated by interaction of the sea breeze front with the synoptic flow. The eddies are compared with the Kanto plain eddy modeled by Kimura.

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Book ChapterDOI

Hydrostatic airflow over mountains

TL;DR: In this article, the authors describe the hydrostatic airflow over mountains and construct an approximate regime diagram depicting how the nature of mountain-induced flow disturbance depends on the control parameters of the problem.
Book ChapterDOI

Boundary Layers and Air Quality in Mountainous Terrain

TL;DR: In this paper, the general problem of air pollution in mountainous terrain is discussed, including specific effects encountered in stable-and convective boundary layers and under dynamically driven conditions, using numerical models, scale models, and observational studies.
Journal ArticleDOI

The Australian Air Quality Forecasting System. Part III: Case Study of a Melbourne 4-Day Photochemical Smog Event

TL;DR: The performance of the Australian Air Quality Forecasting System (AAQFS) is examined by means of a case study of a 7-day photochemical smog event in the Sydney region as mentioned in this paper.
Journal ArticleDOI

Observations and numerical modelling of Lake Ontario breezes

Neil T. Comer, +1 more
- 01 Dec 1993 - 
TL;DR: In this article, two years of land-based data showed that the Lake Ontario breeze develops on 30% of the days during summer and typically develops in mid-morning and persists until the late evening when it is replaced by a well developed landbreeze regime.
Journal ArticleDOI

Review: Mesoscale modelling in complex terrain

W.L. Physick
TL;DR: In this article, the authors focus on those aspects of mesoscale models which require special techniques and parameterizations when modelling flow over complex terrain, and the basic concepts and limitations of various approaches are discussed.
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