Analysis of lightning outliers in the EUCLID network
Lightning data as observed by the European Cooperation for Lightning Detection (EUCLID) network are used in combination with radar data to retrieve the temporal and spatial behavior of lightning outliers, i.e., discharges located in a wrong place, over a 5-year period from 2011 to 2016. Cloud-to...
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doaj-b7a7b1fabb664daa9f64e4e7fcdfdd642020-11-24T23:58:08ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482017-11-01104561457210.5194/amt-10-4561-2017Analysis of lightning outliers in the EUCLID networkD. R. Poelman0W. Schulz1R. Kaltenboeck2L. Delobbe3Royal Meteorological Institute of Belgium, Brussels, BelgiumOVE–ALDIS, Vienna, AustriaAustro Control, Innsbruck, AustriaRoyal Meteorological Institute of Belgium, Brussels, BelgiumLightning data as observed by the European Cooperation for Lightning Detection (EUCLID) network are used in combination with radar data to retrieve the temporal and spatial behavior of lightning outliers, i.e., discharges located in a wrong place, over a 5-year period from 2011 to 2016. Cloud-to-ground (CG) stroke and <span style="" class="text">intracloud</span> (IC) pulse data are superimposed on corresponding 5 min radar precipitation fields in two topographically different areas, Belgium and Austria, in order to extract lightning outliers based on the distance between each lightning event and the nearest precipitation. It is shown that the percentage of outliers is sensitive to changes in the network and to the location algorithm itself. The total percentage of outliers for both regions varies over the years between 0.8 and 1.7 % for a distance to the nearest precipitation of 2 km, with an average of approximately 1.2 % in Belgium and Austria. Outside the European summer thunderstorm season, the percentage of outliers tends to increase somewhat. The majority of all the outliers are low peak current events with absolute values falling between 0 and 10 kA. More specifically, positive cloud-to-ground strokes are more likely to be classified as outliers compared to all other types of discharges. Furthermore, it turns out that the number of sensors participating in locating a lightning discharge is different for outliers versus correctly located events, with outliers having the lowest amount of sensors participating. In addition, it is shown that in most cases the semi-major axis (SMA) assigned to a lightning discharge as a confidence indicator in the location accuracy (LA) is smaller for correctly located events compared to the semi-major axis of outliers.https://www.atmos-meas-tech.net/10/4561/2017/amt-10-4561-2017.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
D. R. Poelman W. Schulz R. Kaltenboeck L. Delobbe |
spellingShingle |
D. R. Poelman W. Schulz R. Kaltenboeck L. Delobbe Analysis of lightning outliers in the EUCLID network Atmospheric Measurement Techniques |
author_facet |
D. R. Poelman W. Schulz R. Kaltenboeck L. Delobbe |
author_sort |
D. R. Poelman |
title |
Analysis of lightning outliers in the EUCLID network |
title_short |
Analysis of lightning outliers in the EUCLID network |
title_full |
Analysis of lightning outliers in the EUCLID network |
title_fullStr |
Analysis of lightning outliers in the EUCLID network |
title_full_unstemmed |
Analysis of lightning outliers in the EUCLID network |
title_sort |
analysis of lightning outliers in the euclid network |
publisher |
Copernicus Publications |
series |
Atmospheric Measurement Techniques |
issn |
1867-1381 1867-8548 |
publishDate |
2017-11-01 |
description |
Lightning data as observed by the European Cooperation for Lightning
Detection (EUCLID) network are used in combination with radar data to retrieve
the temporal and spatial behavior of lightning outliers, i.e., discharges
located in a wrong place, over a 5-year period from 2011 to 2016.
Cloud-to-ground (CG) stroke and <span style="" class="text">intracloud</span> (IC) pulse data are superimposed on
corresponding 5 min radar precipitation fields in two topographically
different areas, Belgium and Austria, in order to extract lightning
outliers based on the distance between each lightning event and the nearest
precipitation. It is shown that the percentage of outliers is sensitive to
changes in the network and to the location algorithm itself. The total
percentage of outliers for both regions varies over the years between 0.8 and
1.7 % for a distance to the nearest precipitation of 2 km, with an
average of approximately 1.2 % in Belgium and Austria. Outside the
European summer thunderstorm season, the percentage of outliers tends to
increase somewhat. The majority of all the outliers are low peak current
events with absolute values falling between 0 and 10 kA. More specifically,
positive cloud-to-ground strokes are more likely to be classified as outliers
compared to all other types of discharges. Furthermore, it turns out that the
number of sensors participating in locating a lightning discharge is
different for outliers versus correctly located events, with outliers having
the lowest amount of sensors participating. In addition, it is shown that in
most cases the semi-major axis (SMA) assigned to a lightning discharge as a
confidence indicator in the location accuracy (LA) is smaller for correctly
located events compared to the semi-major axis of outliers. |
url |
https://www.atmos-meas-tech.net/10/4561/2017/amt-10-4561-2017.pdf |
work_keys_str_mv |
AT drpoelman analysisoflightningoutliersintheeuclidnetwork AT wschulz analysisoflightningoutliersintheeuclidnetwork AT rkaltenboeck analysisoflightningoutliersintheeuclidnetwork AT ldelobbe analysisoflightningoutliersintheeuclidnetwork |
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