CAOs are identified using daily minimum temperature data extracted from 53 stations within the Global Historical Climatology Network-Daily dataset over a 68-year period from January 1948 through December 2015. Stations are evenly distributed across the contiguous U.S. and the nine National Centers for Environmental Information (NCEI) U.S. Standard Regions. Days that have minimum temperatures at a station fall below the 31-day centered moving average of the daily fifth percentile temperature are designated as anomalously cold days, and sequences of three or more such days are classified as CAOs. A regional CAO is diagnosed whenever two or more stations within the same NCEI U.S. Standard Region experience an overlap of the same sequence of anomalously cold days.
Preliminary statistical trends for the meteorological spring, summer, fall, and winter seasons show that there has been a decrease in the annual frequency of anomalously cold days for the northeastern U.S. across all four seasons. There has also been a decrease in the annual frequency of northeastern U.S. CAOs across all four seasons. Additional regions will be studied to determine annual statistical trends in the frequency of anomalously cold days and CAOs. CAO-relative composites using NCEP–NCAR reanalysis data will be constructed to identify region-specific patterns in the planetary- and synoptic-scale flow patterns that accompany the development of CAOs.