Maryland SNOW REPORT
March 29 2024
Snowpack conditions in Maryland vary based on the state's diverse topography and climate. The state's highest mountain ranges, including the Appalachian and Blue Ridge Mountains, contribute significantly to snow accumulation. These ranges receive an average annual snowfall of 30-60 inches, with the highest peaks often experiencing more substantial snowpack.
The resulting snowmelt from these mountain ranges feeds into several important rivers and watersheds, such as the Potomac, Patapsco, and Monocacy Rivers. These water sources play a crucial role in supplying drinking water and supporting ecosystems throughout the state.
Maryland's winter climate is influenced by its proximity to the Atlantic Ocean and the Appalachian Mountains. It experiences a mix of cold Arctic air, coastal storms, and occasional snowstorms. The snowfall pattern varies, with western regions typically receiving more snow than the eastern coastal areas.
Interesting snow science and history in Maryland include the role of the Cryosphere Innovation Hub at the University of Maryland, which focuses on researching snow and ice processes. Additionally, Maryland's record snowfall occurred during the "Knickerbocker Storm" in 1922, which dumped over 2 feet of snow in parts of the state.