Council’s Blenheim office will be closed Friday 25 April for Anzac Day. See details of transfer station opening hours and kerbside collections
Council’s Blenheim office will be closed Friday 25 April for Anzac Day. See details of transfer station opening hours and kerbside collections
The phenomena of smoke and smog is created when tiny particles become concentrated in the air. These particles are commonly referred to as PM10. PM10 refers to the size of these particles, ie; the particles are less then 10 microns in diameter - that is less than a fifth of the width of a human hair.
These particles are commonly produced as by-products of combustion and can come from vehicle exhausts, industry, outdoor burning and domestic fires (coal and wood). There are also natural' sources of PM10, which include sea spray and dust particles.
PM10 is a problem in winter because domestic heating in the form of wood and coal fires increases. Wood is a valuable fuel source for Marlborough and its urban centres, but in order to ensure clean air and warm homes more efficient, cleaner methods of burning wood are required.
Winter is also when Marlborough experiences inversion events. Inversion events are characterised by cold, still, frosty nights. An inversion layer acts to trap air pollutants, in this case PM10, and thereby increases its concentration.
Diagram from: Environment and Climate Change Canada
A clear winter day with air contaminants visibly trapped by an inversion layer over Blenheim.
Normally, hot air rises and disperses pollutants upwards but during a temperature inversion event a layer of warm air traps the movement of pollutants, effectively creating a ceiling and concentrating the pollutants close to ground level. The height of the inversion layer is not fixed and can vary.
Often an inversion layer can be visible when a plume of smoke is seen to rise and then stops and moves sideways as though it has just hit an invisible ceiling.