Find weather for


SEEK Job Search

Gove Radar/Lightning

Monday 08:30 CST
Bureau of Meteorology Weather Radar
loading...
 
 
   
duration    speed    dwell   

Map
Radar
Rivers
Roads
Borders
Towns
Rainfall
Weatherzone radar light dBz scale heavy precipitation

Related Links

About ninemsn weather Radar

rainfall Rainfall since 9am local time is displayed with coloured dots.

distance measuring On local radar pages distance and latitude/longitude coordinates are displayed next to the time stamp 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.

Radar Details

Gove Windfinding and Weather Watch Radar
Northern Territory
12.2750°S  136.8230°E  50m AMSL

LocationGove Airport Radar TypeWF 100 C Band Typical Availability2130-0815; 1030-1415; 1530-2115

The Gove radar has a nearly unrestricted view in all directions. Local topography can produce a single weak false echo immediately adjacent the radar centre to the southeast. During the wet season, thunderstorm tops will be visible out to the effective range of the radar at around 250km although smaller showers frequently associated with these storms will not be visible at that range. Tropical cyclones may be seen during the wet season months November to April, although lesser category 1 cyclones may not be sufficiently developed to be easily discernable. The higher category tropical cyclones will display rain echoes in spiral bands rotating about a central clear eye with the highest intensity rainfall about the eye. The structure of the cyclone in the arc facing the radar centre will be seen, although the far side will be less clear due to the weakening of the radar signal by heavy rain (attenuation). The closer the cyclone is to the radar centre the clearer the structure will be viewed. Rain showers during the dry season are common; most frequently moving from east to west, often in organized lines (known as Gulf Lines) orientated approximately north-south. Cooling after midnight during the dry season frequently results in false echoes (Anomalous Propagation) appearing over the land as isolated weak areas with sometimes up to 80% coverage. These echoes are identified by their random appearance and disappearance between sequences with no general direction of movement and total dissipation after sunrise. They only appear over land and are displayed as the weakest level echoes.

powered by The Weather Co.
Based on information from the Bureau of Meteorology and other providers