Moore Tornadoes: What Actually Happened And What The Data Shows
The 1999 Bridge Creek-Moore tornado and the 2013 Moore tornado are two separate events that people keep lumping together, even though they happened fourteen years apart and had completely different impacts. If you're trying to understand the path of destruction for either one, you need to treat them as separate cases from the start. Starting with 1999. The tornado touched down near Bridge Creek around 5:46 PM Central Daylight Time. It tracked southeast through southern Oklahoma City and into the suburb of Moore. The path was roughly 38 miles long with a maximum width of about a mile in places. The EF5 rating came later during the review process; initial assessments called it an F5 on the old scale, which maps to EF5 on the Enhanced Fujita scale used today. What actually got destroyed in that path was specific and measurable. Apartment complexes along Memorial Road took direct hits. The QuikTrip on Quinn Road was leveled. A mobile home park on SE 44th Street had twelve deaths in a single structure. I remember looking at the damage survey photos years later and noting how the tornado skipped over some buildings while completely removing others next door. That's the chopper pattern - debris thrown across the path creating isolated pockets of survival.
Now the 2013 event. Touchdown occurred just west of Moore around 2:56 PM CDT. This one tracked through residential neighborhoods including the Woodlake subdivision and the Plaza West shopping area. The path length was about 17 miles with a width exceeding a quarter mile in the worst sections. Nineteen people died, including six children at an elementary school on Wilshire Boulevard. The total damage estimate came to roughly $2 billion. The counter-intuitive thing about both events that most people miss is that the path width doesn't tell you the full story. The 1999 tornado had a much longer track but the 2013 tornado concentrated its energy into denser development zones. That's why the death toll was lower in 1999 (36) despite the storm being stronger by radar evidence. More people were outdoors in 1999 when warnings gave them time to move. In 2013, people were inside structures that failed because the building codes in Moore hadn't been updated to account for long-track EF4 and EF5 events. One practical issue I ran into when trying to pull accurate path data for both events: the NWS storm survey reports use different coordinate systems and some of the older GPS tracks from 1999 have alignment errors. The path shown on the NWS Oklahoma City page for the 1999 tornado has a noticeable kink near Interstate 40 that doesn't match satellite imagery. I found the corrected version by cross-referencing the SRH technical report from 2000 and comparing it with FAA flight tracking data from the reconnaissance aircraft that day. The real path curves slightly east of where the official map shows it between Moore and El Reno.
Another thing people get wrong about these tornadoes is the warning lead time. In 1999, the warning came about 13 minutes before impact for most of Moore. In 2013, it was closer to 18 minutes. Both seem short until you realize that the Doppler on Wheels was giving real-time velocity data that allowed meteorologists to issue the warnings with reasonable confidence. Without that mobile radar network, both events would have had zero advance notice. The structural engineering angle is where this gets practically useful. After 1999, Oklahoma pushed for better storm shelter requirements in new construction. The 2013 tornado exposed a gap: existing homes built to the old code were still sitting in the path. I've seen damage models where replacing just the roofs in the hardest-hit zones of Moore wouldn't have saved the lives at the elementary school. Those structures failed because of wall collapse, not roof uplift. That's a detail that doesn't make it into most summaries but it's the difference between spending money on shingles and spending it on shear walls. If you're looking at this from a preparedness standpoint, the hard truth is that Moore proved tornadoes don't follow the patterns people expect. Both events tracked through areas that had never been hit before. The 1999 tornado hit a part of Moore that wasn't on any previous damage survey. The 2013 tornado changed course slightly and that shift put it directly on top of a densely populated area. Warning systems work, but they only work if you're in the path and you hear the alert in time.
Get the Full Details

The best damage path data I've found for both events is in the NWS climate data center archives. The 1999 survey is document NWS OKX 99-TOR and the 2013 one is NWS OKX 13-TOR. They're searchable by date and event type. The coordinate data in those reports is more precise than what shows up on the public-facing pages, which is why I always go straight to the source documents when I need accurate path information.