Abstract
WWLLN (World Wide Lightning Location Network) data on global lightning
are used to investigate the increase of total lightning strokes at
Arctic latitudes. We focus on the summertime data from June, July and
August, which average >200,000 strokes each year above
65o North latitude, for each of the years from 2010 –
2020. The influence of WWLLN network detection efficiency increases is
minimized by normalizing to the total global strokes for each northern
summer.
The ratio of strokes occurring above 65o increases
with latitude, showing that the Arctic is becoming much more influenced
by lightning. We compare the increasing fraction of strokes with the
global temperature anomaly for those months, and find that the fraction
of strokes above 65o to total global strokes for these
months increases linearly with the temperature anomaly and grows by a
factor of 3 as the anomaly increases from 0.65 to 0.95 degrees C.