Clerestory Windows

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ELEMENT:

Breezway Louvres with timber and glass blades

AIM:

A passive ventilation system is used in place of electrical energy intensive climate control devices such as air conditioners. The louvred window openings give a greater control over the direction and velocity of air entering the building.

STRATEGY:

Optimise Passive Design

In moderate warm climates the purpose of ventilation is to provide fresh air to the occupants, cool the building fabric and cool the occupants though air movement and heat loss. Cross ventilation is horizontal and is usually wind driven. Stack ventilation is usually vertical and driven by thermal difference.

Clerestory windows provide for a stack ventilation effect in the house. The positioning of clerestory windows high in the building envelope adds to the natural airflow effect from low to high with the warmer air escaping through the high window opening.

In periods of calm, stack ventilation is used; air rises into the atrium and siphons through popup roof monitors. To facilitate this type ventilation system a pavilion form is used with the building split into two sections connected by a breezeway. The portal frame structure allows the building to be open inside to facilitate air movement without the need for bracing walls.

Louvered windows provide a potential 100% surface area opening for airflow into the building. Adjusting the angles of the louvred blades can also control airflow direction which provides for a greater control over the desired air movement.

Timber louvre blades are used for the clerestory windows facing north to reduce the solar penetration through the window. Glass louvre blades are used for the clerestory windows facing south to increase the natural daylight to the atrium space. This lighting is diffuse (reflected) light rather than direct sunlight so the heat gain from this type of light is negligible.

REFERENCE:

Breezway Louvres Techinical Information. June 1999.
Hyde, R, Climate Responsive Design. A Study of Buildings in Moderate and Hot Humid Climates. E and FN Spon, London 2000.