This system detects all types of lightning but is biased towards detecting cloud to ground strikes. The majority of lightning occurs in the storm cloud itself or between clouds. On average approximately 10 to 20 percent of all lightning over Ireland are cloud-to-ground strikes.
Lightning locations are sourced from the WMO SFERIC (SFUK) messages. Some atmospherics may not be detected. Isolated spurious returns can also occur. Detection efficiency is variable, ATDnet records approximately 60% of all medium to strong lightning strikes over Europe. Further information about lightning detection at Valentia Observatory is available here.
We are most grateful to the UK Met Office for the use of their Arrival Time Difference (ATD) lightning location data.
Lightning strikes, when they occur, are displayed as a cross. Initially they are red but change to orange and then yellow after a period, then disappear.