Most studies on Northeast U.S. snow events have focused on cases with large snowfall amounts, often in excess of 15.2 cm (6 in). A snow event does not need to have such high snow amounts to be impactful; for instance, frequency of snow events generally increases with latitude, thus snow events in lower latitudes are often more impactful than similar accumulations at higher latitudes, and even minor snow events can cause socioeconomic disruption.
This study utilizes an individually created and quality controlled climatology of the majority of Northeast U.S. snow events during 2000–2019 for any synoptically forced event, including mesoscale bands or upslope enhanced precipitation but removing lake effect snow, that produced over 7.6 cm (3 in) of snowfall in multiple observation sites within the region. This presentation will show how this gridded climatology can be used for various applications, such as constructing a modified NESIS scale utilizing normalized anomalies of snow events relative to a local climatological distribution, spatial frequency of snow events and associated cyclone tracks by accumulation threshold, and comparison of synoptic regimes and teleconnections associated with periods of frequent minor snow events, frequent major snow events, or infrequent major snow events.