Dry lightning occurrence is of critical importance to land management agencies since this type is most likely to cause wildland fires. Dry lightning is cloud-to-ground (CG) lightning without any accompanied rainfall nearby. Recent dry lightning research has concentrated on using upper air measurements--atmospheric stability and moisture content to predict dry lightning episodes in advance (Rorig and Ferguson 1999). Spatial products are needed to give managers an idea of where dry lightning has occurred immediately after the storms have passed.
The Dry Lightning Map is made by merging daily estimated rainfall grids, produced by Advanced Hydrologic Prediction Service (AHPS), with two polarity based lightning density grids, produced from daily cloud to ground lightning strike data (Cummings et. al 1998). A Lightning Fuel type grid converted from a cover type map (Schmidt and others, 2002) is used in the dry lightning cell calculation. The lightning strike and estimated rainfall data are adjusted for the 24-hour hydrologic day (ending at 1200GMT) used by AHPS.
Two lightning density grids are created, one for positive and one for negative lightning strikes. All grids have a 4km pixel size in which the lightning fuel type grid is static and the lightning density and estimated rainfall grids are recreated daily. A dry lightning cell exists when it has met three criteria: rainfall less than 0.10in (0.25in for the Southern and Eastern map), fuel (not classified as barren, urban or water), and a positive or negative cloud to ground lightning strike. Dry lightning cells are displayed based on strike polarity. If both positive and negative strikes occur in a cell, the cell is classified as “positive”. Estimated rainfall is displayed for reference purposes.
There are regional differences in the the definition of a dry lightning strike. Maps are available based on Geographic Area Coordination Center (GACC) boundaries. The Eastern and Southern area maps have a rainfall threshold for a dry lightning event of 0.25 inches or less. All other regions use an estimated rainfall threshold of 0.10 inches.
Cummins, K.L.; Murphy, M.J.; Bardo, E.A.; Hiscox, W.L.; Pyle, R.B.; Pifer, A.E. 1998. A combined TOA/MDF technology upgrade of the U.S. National Lightning Detection Network. J. Geophys. Res. 103: 9035-9044.
Rorig, M.L. and S.A. Ferguson, 1999: Characteristics of lightning and wildland fire ignition in the Pacific Northwest. J. Appl. Meteor., 38: 1565-1575.
Schmidt, K.M., J. P. Menakis, C. C. Hardy, W. J. Hann, and D. L. Bunnell. 2002: Development of coarse-scale spatial data for wildland fire and fuel management. General Tech. Rep. RMRS-GTR-87. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, 41 pp. +CD