HR: 1330h
AN: AE32A-0162 [PDF]
TI: Lightning Climatology: Median Peak Current Increase Along the U.S. Coast
AU: * Ely, B L
EM: bely@tamu.edu
AF: Texas A\&M University, Department of Atmospheric Sciences, College Station, TX 77843-3150 United States
AU: Orville, R E
EM: rorville@tamu.edu
AF: Texas A\&M University, Department of Atmospheric Sciences, College Station, TX 77843-3150 United States
AB:
Climatological studies of cloud-to-ground (CG) lightning have discovered interesting features across the United States. One
such feature that has been noted in previous research is a sharp increase in the median negative peak currents along the U.S.
coasts. The values over the ocean are consistently higher than over land with a rapid increase of approximately 4kA at the
coastline. The median positive peak currents also show an increase offshore. However, there is no distinct change at the
coastline. One explanation for this observation is the higher conductivity of the salt water decreases the attenuation of the
electromagnetic signal of the CG flashes over the water. This would lead to a flash that would appear stronger to the NLDN
sensors. However, there is a problem with this hypothesis. If the attenuation explanation is correct, the same sharp
transition at the coastline should be seen in the positive peak current.
A possible explanation for the absence of the sharp coastline increase in the positive peak currents is due to intracloud
flashes, which are detected as weak positive CG flashes and contaminate the dataset. To minimize contamination all positive
flashes below 10kA are omitted. However, this cutoff can also remove weak positive CG flashes and leave strong intracloud
flashes in the dataset. Analyses of the peak currents for selected locations along the U.S. coasts are performed to
determine the validity of this hypothesis.
DE: 3300 METEOROLOGY AND ATMOSPHERIC DYNAMICS
DE: 3304 Atmospheric electricity
DE: 3309 Climatology (1620)
DE: 3324 Lightning
SC: Atmospheric and Space Electricity [AE]
MN: 2003 Fall Meeting