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Report - London Borough of Hillingdon

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WINTER SERVICE OPERATIONAL PLAN<br />

74BPeriod<br />

Used to describe the length <strong>of</strong> cloud breaks or amounts <strong>of</strong> sunshine, generally <strong>of</strong> two hours<br />

or more duration.<br />

75BPowder Snow<br />

The form <strong>of</strong> snow that occurs when air temperatures are well below freezing, (-2 o C or less).<br />

This form <strong>of</strong> snow is very fine (like sugar crystals), drifts very easily, but does not tend to<br />

stick to objects, (no accretion). It can be handled by snow blowers. Salt is usually less<br />

effective.<br />

76BPrecipitation<br />

A general term that covers all water (or ice), which ‘falls’ from the skies. As well as rain,<br />

sleet, snow and hail it also includes dew, hoar frost and fog.<br />

7BPrecipitation Type<br />

The individual type <strong>of</strong> precipitation. In winter maintenance activities, this will be one <strong>of</strong> rain,<br />

drizzle, sleet, wet snow, dry snow, hail, freezing rain and freezing drizzle, (see Precipitation).<br />

78BProlonged<br />

Used to describe showers that merge together producing a spell or continuous precipitation,<br />

generally lasting more than one hour and covering a relatively large area.<br />

79BRain<br />

Water droplets that fall from clouds. Rain takes many forms, and can be <strong>of</strong> many different<br />

intensities and duration’s. Within road weather forecasts there will <strong>of</strong>ten be differentiation<br />

between rain and showers, the former usually referring to longer-lived but light intensity<br />

precipitation, and the latter to short duration but heavy intensity.<br />

80BRelative Humidity<br />

This is the amount <strong>of</strong> actual water vapour held in a sample <strong>of</strong> air at a given temperature,<br />

divided by the maximum amount <strong>of</strong> water that could be held in that sample <strong>of</strong> air at that<br />

temperature, expressed as a percentage. Within fog or heavy rain, humidities may reach<br />

100%. On a sunny, warm afternoon in summer, humidities may fall to 30%. On an average<br />

night in winter, humidities rarely fall below 80%, (which is the minimum humidity at which salt<br />

crystals will start to absorb water).<br />

81BRime<br />

Deposition <strong>of</strong> ice from freezing fog. It is a white form <strong>of</strong> ice, similar to hoar frost, but has a<br />

finer (at times feathery), structure. On roads, tends to be more <strong>of</strong> a problem at higher levels<br />

than lower levels.<br />

RST<br />

Common abbreviation for road surface temperature. Saturated Air is said to be saturated<br />

when, at a given temperature, it holds the maximum amount <strong>of</strong> water vapour possible. Any<br />

cooling below its current temperature will result in condensation. The relative humidity <strong>of</strong><br />

saturated air is 100%.<br />

Saturated<br />

The rate at which air temperature falls with height within adiabatic lapse saturated air, e.g.,<br />

within fog or cloud. It is less than the rate dry adiabatic lapse rate, 0.49 o C per 100 metres or<br />

around 1.5 o C per 1,000 feet.<br />

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