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Stevenson Screen
Maximum and minimum temperature thermometers are placed inside a Stevenson Screen. The screen allows good air flow across the thermometers but prevents heating from direct sunlight.

White or hoar frost
These frozen dew drops on a pine tree are an example of a white, or hoar frost. This was most likely caused by radiative cooling overnight (radiation frost).
Frost is a localised phenomenon which is fairly common in parts of southern Australia.
Frost is defined as a deposit of soft white ice crystals or frozen dew drops on objects near the ground; formed when the surface temperature falls below freezing point.
There are two main ways that frost can form, with radiation being the most common method of formation in Australia.
Frost can also take several forms, including:
Some areas, on a regional scale, are particularly prone to frost. These are sometimes referred to as frost hollows, or frost pockets if they are very small. Frost hollows often occur in valleys due to cold air drainage. As the air at the top of a hill cools at night, it becomes dense and heavy compared to surrounding air, and will drain to lower levels. This is referred to as a katabatic wind, and can result in frost forming in valleys when surrounding areas remain frost-free.
Frost formation is affected by a series of factors including cloud coverage, humidity, surface winds, topography and location. In Australia, frost is more likely to form under a clear sky, with low humidity and light surface winds.
Temperature is measured by standard instruments which are located in a shelter (Stevenson screen) at a height of approximately 1.2 m above the ground. These observations are then used to approximate the conditions at surface level. An observed temperature of 2.2°C at screen level indicates that the temperature at the surface is approaching 0°C.
A set of frost potential climate maps has been produced to give you an indication of areas that may be affected by frost. These maps show the average number of days (annually and monthly) where the minimum temperature falls below a given threshold.
The occurrence of frost can have a devastating effect on vegetation and crops. Frost potential maps and frost warnings are used by the agriculture industry to manage the risks associated with frost. Frost information is also used by the home gardener to minimise damage to gardens.
The impact that a particular frost event will have on a crop or garden depends upon the severity of the frost and the crop or plants in question. Frost is a localised phenomenon, the severity of which can vary significantly over a very small area. Different crops and plants have different tolerances to frost. Crop type, variety, sowing date, nutrition and stage of growth can all determine the extent to which the crop is affected by a frost.
Have a look at the most recent frost potential forecasts.
Use the frost potential climate maps to see the average frost potential in your area.
Climate extreme trend maps show the trend in nights with a minimum temperature below 0°C.
See recent minimum temperatures in your area (past fourteen months).
Your local state government departments may be able to help you with information about measures to reduce frost risk:
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