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Mildura 128km Radar/Lightning

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Bureau of Meteorology Weather Radar

Lightning Data Upgrade - NEW

Lightning Events

lightning Lightning strikes are displayed as crosses (ground events) or squares (cloud events) and fade from white (current) to red (30 minutes ago) to blue (60 minutes ago).

In December 2014 we upgraded our lightning network to the latest in sensor technology as used by the world's leading meteorological agencies. This has resulted in changes and improvements to the lightning data you will now see. The main changes are:

  • Much better detection of cloud to cloud strikes. Our upgraded network detects more CC strikes and better reflects research that shows typical storm cells produce approximately 75% cloud strikes and 25% ground strikes.
  • We have modified the display to show cloud to cloud strikes in smaller boxes and ground strikes above as "+" symbols. Temporal colouring remains the same.
  • Greater network coverage right across the country.

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About Weatherzone Radar

distance measuring Distance and latitude/longitude coordinates are displayed when you mouse over the map. The origin for distance measuring is indicated by a red dot and defaults to either your location, if specified and in range, or the location of the radar/the centre of the map. The origin may be changed by clicking elsewhere on the map.

The colours and symbols used on the radar and satellite maps are described on our legend page. View legend »

Lightning data supplied by GPATS

Radar Details

Mildura Wind Finding and Weather Watch Radar
Victoria
34.2330°S  142.0830°E  53m AMSL

LocationMildura Airport Radar TypeWF 100 C Band Typical Availability0000-0300; 0430-0900; 1030-1500; 1630-2100; 2230-0000

The Mildura radar has a very good view in all directions as there are no significant geographic features in the area. Its only limitations are those common to all C Band radar, that is that if there are large thunderstorms around, the radar will not be able to detect accurately the strength of storms located behind the closest storms. This will also lead to the underestimation of the strength, at times, of very intense isolated storms. False echoes are sometimes observed very close to the radar especially in stable conditions. Echoes within five or so kilometres of the radar and overhead are poorly resolved as the scanning elevation is too low.

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