Index
- Alaska Climate Divisions FAQs
- Anomalies vs. Temperature
- Arctic Sea Ice Measurements
- Billion-Dollar Disasters: Calculating the Costs
- Binomial Filter
- Climate Division Dataset Transition
- Climate Extremes Index
- CLIMAT Messages
- Climatological Rankings
- Coral Reef Bleaching
- Dead Fuel Moisture
- Definition of Drought
- Drought Indicators
- Drought in the Colorado River Basin
- Drought vs. Aridity
- El Niño: A Historical Perspective
- Explanation of the 500 mb Flow
- Future Drought
- Global Precipitation Percentile Maps
- Global Regions Definitions
- Global Temperature Anomaly Percentile Maps
- Global Temperature Uncertainty
- Groundwater Drought Indicators
- Hawaiʻi Climate Divisions FAQs
- LOESS
- Measuring Drought
- Monthly Releases
- Monthly Report RSS Feed
- National Data Flow
- nClimDiv Maximum and Minimum Temperatures
- Palmer Drought Index
- Potential Evapotranspiration
- Reforestation of Bastrop Lost Pines
- Regional Climate Centers
- Regional Snowfall Index (RSI)
- Satellite-Based Drought Indicators
- Soil Moisture Water Balance Models
- Southern Hemisphere Snow Cover Extent
- Standardized Precipitation Index
- Streamflow Drought Indicators
- Subtropical Highs
- Tornado Count
- U.S. Climate Divisions
- U.S. Climate Normals
- U.S. Drought Monitor Scale
- USHCN Version 2.5 Transition
- Water Supply vs. Water Demand
Tornado Count
Final monthly tornado counts are typically less than the preliminary count. This can be due to some phenomena being inaccurately reported as tornadic activity or a single tornado being reported multiple times. Tornado accounts are reported to the local National Weather Service forecast offices who are responsible for going into the field and verifying each tornado reported. This process often takes several months to complete. Once all reports have been investigated, the final count is published by the Storm Prediction Center (SPC).
The Tornado Monthly Climate Reports are written using the preliminary numbers because the final data is not available at the time of production. Historically, for every 100 preliminary tornado reports, at least 65 tornadoes are confirmed. An error bar is depicted on the tornado count graphic representing this uncertainty in the preliminary tornado count.
The following U.S. studies performed by SPC meteorologists offer deeper context and discussion regarding the frequency and distribution of tornado intensity climatologies:
-
Edwards, R., H. E. Brooks, and H. Cohn, 2021: Changes in tornado climatology accompanying the Enhanced
Fujita scale. J. Appl. Meteor. Climatol., 60, 1465-1482
DOI: 10.1175/JAMC-D-21-0058.1. - Mccarthy, Daniel & Schaefer, Joseph. (2004). Tornado trends over the past thirty years. paper presented at 14th Conference on Applied Meteorology.