Snow accumulation season is the season of drift growth, beginning with the first blowing snow event that causes drifts persisting through the winter, and ending when snowdrifts reach their maximum volume (Tabler 1994).
Onset Date
Average start date for the first blowing snow event causing drifts that remain persistent throughout the winter. The product was generated using methodology of Tabler and based on the 1971–1996 mean monthly temperature records.
End Date
Average end date for the period of persistent drifting in which snowdrifts reach maximum volume. The product was generated using methodology of Tabler and based on the 1971–1996 mean monthly temperature records.
Tabler Methodology
The snow accumulation season is indicated by the time period in which the average air temperature reaches the freezing point, 0° C (Tabler 1994). The beginning and ending dates are found using the following equation, based on mean monthly temperatures:
T+ and T- are the mean monthly temperatures of the warmer (above 0° C) and colder (below 0° C) months, respectively. The equation yields a number of days, n, which is added to the middle of the warmer month for the onset date, and subtracted from the middle of the warmer month for the end date.
Reference
Tabler, R.D., 1994. Design Guidelines for the Control of Blowing and Drifting Snow, Strategic Highway Research Program, Washington D.C., 364 pp.