detects objects by transmitting a pulse of radio waves and
looking for signals reflected back from the object.
By measuring the time taken for the pulse to reach the
object and travel back to the radar, the distance can be
calculated. By rotating the antenna and sending out a stream
of pulses, the radar can build up a picture of objects.
Rain, snow and hail reflect radar waves. Using radar we
can get a picture of the extent and intensity - the greater
the intensity of rainfall, the stronger the signal returned
- of the rainfall.
At longer ranges, typically over 100km, the accuracy falls
off due to the curvature of the Earth. Sometimes the radar
will not 'see' rain at long ranges or report rain at high
altitudes that does not reach the ground.
Radars also ‘see’ the ground and while measures are taken
to reduce echoes returned from the ground, some appear on
the images. Frequently echoes can be seen from the Mourne
and Galtee mountains even when no rainfall is present.
The images here are a composite of data from two radars
- one at Dublin Airport and the other at Shannon Airport.
The shaded area shows the coverage of the radars that are
present. Data are updated every 30 minutes.