Why do oceanic negative cloud‐to‐ground lightning exhibit larger peak current values?
Author:
Affiliation:
1. Earth System Science Center University of Alabama in Huntsville Huntsville Alabama USA
2. Earth Science Office, ZP11 NASA Marshall Space Flight Center Huntsville Alabama USA
3. Universities Space Research Association Huntsvillle Alabama USA
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JD024129
Reference85 articles.
1. Anderson R. B. andA. J.Eriksson(1980) Lightning parameters for engineering application published in Electra 69.
2. Effects of the Large-Scale Flow on Characteristic Features of the Sea Breeze
3. The effect of the cloud-droplet spectrum on electrical-charge transfer during individual ice-ice collisions
4. Global patterns of lightning properties derived by OTD and LIS
5. National Lightning Detection Network (NLDN) performance in southern Arizona, Texas, and Oklahoma in 2003–2004
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