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Welcome to Baltimore

Baltimore is the largest independent city in the United States and the largest city and cultural center of the U.S. state of Maryland.

Baltimore is in north-central Maryland on the Patapsco River close to where it empties into the Chesapeake Bay. The city is also located on the fall line between the Piedmont Plateau and the Atlantic Coastal Plain, which divides Baltimore into "lower city" and "upper city". The city's elevation ranges from sea level at the harbor to 480 feet (150 m) in the northwest corner near Pimlico.

According to the U.S. Census Bureau, the city has a total area of 92.1 square miles (239 km2), of which 80.8 square miles (209 km2) is land and 11.3 square miles (29 km2) is water. The total area is 12.24 percent water.

Baltimore Climate

Baltimore lies within the humid subtropical climate zone (Cfa), according to the Köppen classification. July is typically the hottest month of the year, with an average temperature of 81.7 °F (27.6 °C). Summer is also a season of high (generally, not consistently) humidity in the Baltimore area. The record high for Baltimore is 107 °F (42 °C), set in 1936. January is the coldest month, with an average temperature of 36.8 °F (2.7 °C). However, subtropical air masses can bring periods of springlike weather, and Arctic fronts sometimes push nighttime low temperatures into the teens (< −7 °C) and more rarely, single digits (< −12 °C). The record low temperature for Baltimore is −7 °F (−22 °C), set in 1934. Due to an urban heat island effect in the city proper and a moderating effect of the Chesapeake Bay, the outlying and inland parts of the Baltimore metro area are usually cooler than the city proper and the coastal towns.

As is typical in most East Coast cities, precipitation is generous and very evenly spread throughout the year. Every month typically brings 3–4 inches of precipitation, averaging around 43 inches (1,100 mm) annually. Spring, summer and fall bring frequent showers and thunderstorms, with an average of 105 sunny days a year. Winter often brings lighter rain showers of longer duration, and generally less sunshine and more clouds. Snowfall occurs occasionally in the winter, with an average annual snowfall of 18.8 inches (48 cm), In the northern and western suburbs, temperatures tend to be cooler, and winter snowfall is more significant, where some areas average more than 30 inches (76 cm) of snow per year. Freezing rain and sleet occurs a few times each winter in Baltimore, as warm air overrides cold air at the low-mid levels of the atmosphere. When the wind blows from the east, the cold air gets dammed against the mountains to the west and the result is freezing rain or sleet. The average date of first freeze in Baltimore is November 13, and the average last freeze is April 2.