structural:summarization, stylistic:style_transfer
Climate

Like much of the Piedmont region of the southeastern United States, Charlotte has a humid subtropical climate (Köppen Cfa), with four distinct seasons; the city itself is part of USDA hardiness zone 8a, transitioning to 7b in the suburbs in all directions except the south. The following narrative reflects 1991–2020 climate data. Winters are short and fairly mild, with a normal January daily mean temperature of 42.1 °F (5.6 °C). On occasion the temperature can fall below 20 °F (−6.7 °C) but Charlotte also enjoys multiple warm winter days in excess of 65 °F (18.3 °C). On average, there are 59 nights per year that drop to or below freezing, and only 1.5 days that fail to rise above freezing. Precipitation is evenly distributed through the year; only August stands out as a slightly wetter month, averaging 4.35 inches of rainfall. Summers are hot and humid, with a normal July daily mean temperature of 80.1 °F (26.7 °C). Hot and humid days can arrive as early as May and last through the end of September. There is an average of 44 days per year with highs at or above 90 °F (32 °C). Official record temperatures range from 104 °F (40 °C) recorded six times, most recently from June 29 to July 1, 2012, down to −5 °F (−21 °C) recorded on January 21, 1985, the most recent of three occasions. The record cold daily maximum is 14 °F (−10 °C) on February 12 and 13, 1899, and the record warm daily minimum is 82 °F (28 °C) on August 13, 1881. The average window for freezing temperatures is November 5 through March 30, allowing a growing season of 220 days.

Charlotte is directly in the path of subtropical moisture from the Gulf of Mexico as it heads up the eastern seaboard, thus the city receives ample precipitation throughout the year but also many clear, sunny days; precipitation is generally less frequent in autumn than in spring. On average, Charlotte receives 43.60 inches (1,110 mm) of precipitation annually, evenly distributed throughout the year. Annual precipitation has historically ranged from 26.23 in (666 mm) in 2001 to 68.44 in (1,738 mm) in 1884. There is an average of 3.5 inches (8.9 cm) of snow, mainly in January and February and rarely December or March, with more frequent ice storms and sleet mixed in with rain; seasonal snowfall has historically ranged from trace amounts in 2011–12 to 22.6 in (57 cm) in 1959–60. Snow and ice storms can have a major impact on the area, as they often pull tree limbs down onto power lines and make driving hazardous. Snow has been recorded a small number of times in April, most recently on April 2, 2019.

As of 2020, the Charlotte metropolitan area as a whole is noted for having one of the worst weather radar gaps among any major U.S. East Coast city, with little to no coverage in a roughly quadrilateral area spanning Concord, Salisbury and much of Statesville. As the nearest NWS -owned NEXRAD is located in Greer, South Carolina, more than 80 mi (130 km) to the west-southwest of Charlotte, this deficit is particularly problematic during severe thunderstorm or tornado episodes. The current lowest angle of the radar, based in Greer, is quite far above the surface over Charlotte, so the velocities measurement for detecting rotations cannot be below mid-level in potential tornado-forming storms and thus cannot indicate whether said rotation extends closer to the ground (below 5,000 ft (1,500 m)).