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Ceduna 256km 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

Ceduna Windfinding and Weather Watch Radar
South Australia
32.1310°S  133.6950°E  16m AMSL

LocationCeduna Airport Radar TypeWF 100 C Band Typical Availability2145-0215; 0345-0815; 0945-1415; 1545-2015

The Ceduna radar is located at the Meteorological Office which is 3 km east of the township of Ceduna. The surrounding terrain is generally low lying and featureless. The waters of the Great Australian Bight are about 5 km to the southwest of the radar. The radar antenna elevation is 25 metres above sea level. The radar has very good coverage in all directions up to a range of about 250 km. "False echoes" or Anomalous Propagation (AP) can occur on limited occasions in summer where a sea breeze inversion becomes established over the coastal waters. AP can be identified by its static appearance and can normally be distinguished from "real" echoes which exhibit some movement. Heavy rain directly over the radar site can cause attenuation of all signals. Path attenuation can also occur when the radar beam passes through intense rainfall, with the returned signal from cells further along that path reduced.

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