Maryland Geography and Topography
Two majors influences on the weather is land near water and elevation.
Proximty to Water
Places near the water tend to be warmer in the winter and cooler in the summer. Maryland has plenty of water. It’s a lot more than the border on the Atlantic Ocean. If you include all the shoreline around the Chesapeak Bay, the total length is 3,190 miles. According to NOAA, that ranks 10th in the US.
A little more half of Maryland is realtively flat and near sea level in the coasrtal plain. I-95 is arond the deviding line of the Fall Line. West and north of this boundary is where the hills gradually get higher.
A general rule of weather on a dry day is that temperatures will be 5ºF cooler for every 1,000 feet in elevation.
Atlantic Coastal Plain: Generally flat, influenced by the Atlantic Ocean and Chesapeake Bay water keeping it warmer than freezing in most events.
Western Shore Uplands Region: Marked very close to I-95.
Some rolling hills, but still influenced by Chesapeake Bay warmer water.
Upland Section: Rolling hills, increase in elevation close to 1000 Ft above sea level. This includes the Hereford Zone in northern Baltimore County, but that ridge extends to northern Harford, much of Carroll, and western Howard Counties. The higher elevation and distance away from the water can often be cool enough to allow more more snow to fall and stick.
Lowland Section: This is broad valley between Frederick and Mount Airy. Temperatures can be warmer at lower elevations and trap cold air near the surface in some winter storms while warmer air is pushed above mountains. This is a prime target for sleet and freezing rain = ice storms.
Blue Ridge Province= Catoctin Ridge. Mountains reach up to around 1,500 Ft.
Great Valley Section, Folded Appalachian, and Allegheny Mountain Section and Appalachian Plateau
This region has steep mountains and valleys. The elevation reaches above 3,000 Ft in far western Maryland- Garrett County. This can catch Lake Effect Snow from Lake Erie in addition to larger coastal storms.
Split NWS Weather Zones
Topgraphy and Geography have led The National Weather Service to split some counties into differnt zones for weather advisories (alerts, watches, and warnings) in all seasons.
These split county zones in the ‘north and west’ areas of Baltimore are based on the elevation factor and proximity to the Chesapeake Bay