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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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421<br />

the rugged coastline terrain. A model study can be performed using the<br />

observed sea breeze characteristics.<br />

Mathematical model using equations of fluid motion had been<br />

developed to model sea breeze fronts, Clarke( 2 ).<br />

Three dimensional model is<br />

needed for the complex terrains in Hong Kong. Three dimensional<br />

calculations<br />

for flow past non-rectangular bodies are notoriously difficult<br />

<strong>and</strong> time consuming on the computer.<br />

The other alternative is the use of<br />

scale modelling. A wind tunnel with the capability for cooling a<br />

significant portion of the test section floor is required for simulating sea<br />

breeze, Meroney et al( 5 ). This type of meteorological wind tunnel is<br />

expensive to build <strong>and</strong> run. There are only a few existing in this world. A<br />

cheaper alternative has to be found for modelling sea breeze intrusion.<br />

Fortunately<br />

SimpsonW noticed the internal structure of sea breeze front<br />

was similar to the gravity current formed when a lock-gate separating two<br />

fluids of different density was opened suddenly.<br />

This experiment can be<br />

performed very inexpensively in the laboratory with a long water<br />

channel.<br />

To see whether the laboratory experiment can really model the<br />

nature, a particularly complex situation of the crossing of two fronts was<br />

simulated in the water tank. Sometimes, the interaction between a<br />

thunderstorm outflow <strong>and</strong> a sea/lake breeze may occur. Observations of<br />

such interactions were reported by Boyd(^), Moraz <strong>and</strong> Hewson(^). For<br />

large isl<strong>and</strong>s or peninsulas, collision of sea breeze fronts had been also<br />

observed. A well documented case near Stansted was reported by Rider <strong>and</strong><br />

S imp son (7). The movement of the fronts were followed by the radar echos<br />

of swifts. Some qualitative <strong>and</strong> quantitative results were published in that<br />

paper. Clarke(^) also performed a numerical computation on a two<br />

dimensional double sea breeze collision.<br />

In this paper the experimental procedure on the collision between<br />

two gravity currents is described. Suggestions for performing a sea breeze<br />

intrusion into complex terrain in a water tank is put forward.

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