Negative first stroke leader characteristics in cloud-to-ground lightning over land and ocean

We examine downward leader characteristics for negative first return strokes, along with estimated first stroke peak currents, for lightning occurring over land and ocean reported by the U. S. National Lightning Detection Network (NLDN). For the first time, to the best of our knowledge, we report in...

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Main Authors: Nag, Amitabh, Cummins, Kenneth L.
Other Authors: Univ Arizona, Hydrol & Atmospher Sci
Language:en
Published: AMER GEOPHYSICAL UNION 2017
Online Access:http://hdl.handle.net/10150/623001
http://arizona.openrepository.com/arizona/handle/10150/623001
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spelling ndltd-arizona.edu-oai-arizona.openrepository.com-10150-6230012017-04-06T03:00:38Z Negative first stroke leader characteristics in cloud-to-ground lightning over land and ocean Nag, Amitabh Cummins, Kenneth L. Univ Arizona, Hydrol & Atmospher Sci Department of Physics and Space Sciences; Florida Institute of Technology; Melbourne Florida USA Department of Physics and Space Sciences; Florida Institute of Technology; Melbourne Florida USA We examine downward leader characteristics for negative first return strokes, along with estimated first stroke peak currents, for lightning occurring over land and ocean reported by the U. S. National Lightning Detection Network (NLDN). For the first time, to the best of our knowledge, we report independent evidence that supports the observations by lightning locating systems of higher first stroke peak currents for lightning occurring over ocean than land. We analyzed lightning occurring in five circular regions, each with 50 km diameter. In western Florida, the median stepped-leader duration was 17% shorter over ocean than over land and in eastern Florida the median durations were 21% and 39% shorter over two oceanic regions than over land. We infer that the shorter durations over ocean simply reflect the higher (25% in western Florida and 11%-16% in eastern Florida) oceanic return stroke peak currents reported by the NLDN. These findings indicate that the cloud charge structure for (at least some) oceanic storms are different than those for storms over land. The percentage of flashes that had at least one NLDN-reported negative cloud pulse prior to the first negative cloud-to-ground stroke was found to be about the same over land and ocean. Using regression analysis, we found no evidence that the relationship between leader duration and first return stroke peak current is different over land and ocean. 2017 Article Negative first stroke leader characteristics in cloud-to-ground lightning over land and ocean 2017 Geophysical Research Letters 00948276 10.1002/2016GL072270 http://hdl.handle.net/10150/623001 http://arizona.openrepository.com/arizona/handle/10150/623001 Geophysical Research Letters en http://doi.wiley.com/10.1002/2016GL072270 ©2017. American Geophysical Union. All Rights Reserved. AMER GEOPHYSICAL UNION
collection NDLTD
language en
sources NDLTD
description We examine downward leader characteristics for negative first return strokes, along with estimated first stroke peak currents, for lightning occurring over land and ocean reported by the U. S. National Lightning Detection Network (NLDN). For the first time, to the best of our knowledge, we report independent evidence that supports the observations by lightning locating systems of higher first stroke peak currents for lightning occurring over ocean than land. We analyzed lightning occurring in five circular regions, each with 50 km diameter. In western Florida, the median stepped-leader duration was 17% shorter over ocean than over land and in eastern Florida the median durations were 21% and 39% shorter over two oceanic regions than over land. We infer that the shorter durations over ocean simply reflect the higher (25% in western Florida and 11%-16% in eastern Florida) oceanic return stroke peak currents reported by the NLDN. These findings indicate that the cloud charge structure for (at least some) oceanic storms are different than those for storms over land. The percentage of flashes that had at least one NLDN-reported negative cloud pulse prior to the first negative cloud-to-ground stroke was found to be about the same over land and ocean. Using regression analysis, we found no evidence that the relationship between leader duration and first return stroke peak current is different over land and ocean.
author2 Univ Arizona, Hydrol & Atmospher Sci
author_facet Univ Arizona, Hydrol & Atmospher Sci
Nag, Amitabh
Cummins, Kenneth L.
author Nag, Amitabh
Cummins, Kenneth L.
spellingShingle Nag, Amitabh
Cummins, Kenneth L.
Negative first stroke leader characteristics in cloud-to-ground lightning over land and ocean
author_sort Nag, Amitabh
title Negative first stroke leader characteristics in cloud-to-ground lightning over land and ocean
title_short Negative first stroke leader characteristics in cloud-to-ground lightning over land and ocean
title_full Negative first stroke leader characteristics in cloud-to-ground lightning over land and ocean
title_fullStr Negative first stroke leader characteristics in cloud-to-ground lightning over land and ocean
title_full_unstemmed Negative first stroke leader characteristics in cloud-to-ground lightning over land and ocean
title_sort negative first stroke leader characteristics in cloud-to-ground lightning over land and ocean
publisher AMER GEOPHYSICAL UNION
publishDate 2017
url http://hdl.handle.net/10150/623001
http://arizona.openrepository.com/arizona/handle/10150/623001
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AT cumminskennethl negativefirststrokeleadercharacteristicsincloudtogroundlightningoverlandandocean
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