Investigation of Lightning Patterns Over New Jersey and Surrounding Area Al Cope National Weather...
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Invesgaon of Lightning Paerns Over New Jersey and Surrounding Area Al Cope Naonal Weather Service Mount Holly, NJ Adam Gonsiewski Millersville University
Investigation of Lightning Patterns Over New Jersey and Surrounding Area Al Cope National Weather Service Mount Holly, NJ Adam Gonsiewski Millersville
Investigation of Lightning Patterns Over New Jersey and
Surrounding Area Al Cope National Weather Service Mount Holly, NJ
Adam Gonsiewski Millersville University
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Introduction Research on lightning patterns in New Jersey and
surrounding areas, with a focus on the summertime months of June,
July, and August, was conducted during the summer of 2010 at the
National Weather Service Forecast Office in Mount Holly, New
Jersey. The goal was to see whether or not lightning had different
tendencies across the region based on month, hour of the day, 500
mb flow direction, synoptic regime, and day classification (event,
contaminate, or null). This work was designed to coincide with a
related study on summertime convective initiation over New Jersey,
being conducted by NWS Mount Holly and Kean University.
Slide 3
Procedure 1.Obtain CG-Lightning from Vaisala for 2004-08.
Extract a subset of lightning data over the study area. 2.Use
spreadsheet program to sort the data by month, hour of the day,
upper-air flow, synoptic regime, and day classification (event,
contaminate, and null). 3.Create tables and graphs showing
lightning distribution by day and time. 4.Write a FORTRAN program
to put the data into a 21km x 22km grid array (sort lightning by
location). 5.Upload the array output from the FORTRAN program onto
www.GPSvisualizer.com in order to produce flash frequency
maps.
Slide 4
The map to the left shows the total summertime lightning
strikes from 2004- 2008 across the region. The overall lightning
distribution shows a maximum over the Chesapeake Bay region
extending north across eastern PA. There is a minimum in strikes
off the coast of New Jersey (due to colder waters?)
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Daytime T-Storm Trends: SW vs. NW Flow Aloft
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Daytime T-Storm Trends: Cold Front vs. High Pressure
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Conclusions Lightning activity peaks in late afternoon
(diurnally) and in mid-summer (annually) For any given month, large
inter-annual variation is possible Diurnal maximum becomes earlier
from spring into summer Half of all summer lightning occurs with SW
flow aloft; half is associated with cold fronts Diurnal trends vary
somewhat with flow aloft and surface synoptic pattern
Slide 34
Future Work Obtain and analyze lightning data from additional
years Examine diurnal trends past 00Z Create contoured analyses of
flash density
Slide 35
Acknowledgements Lightning data provided by Vaisala (gratis)
THE END