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New Mexico, United States of America (34.57082 -105.99301)
The climate of New Mexico is generally semiarid to arid, though areas of continental and alpine climates exist, and its territory is mostly covered by mountains, high plains, and desert. The Great Plains (High Plains) are in eastern New Mexico, similar to the Colorado high plains in eastern Colorado. The two states share similar terrain, with both having plains, mountains, basins, mesas, and desert lands. New Mexico's statewide average precipitation is 13.9 inches (350 mm) a year, with average monthly amounts peaking in the summer, as at Albuquerque, and Las Cruces in the south. The average annual temperatures can range from 64 °F (18 °C) in the southeast to below 40 °F (4 °C) in the northern mountains. During the summer, daytime temperatures can often exceed 100 °F (38 °C) at elevations below 5,000 feet (1,500 m), the average high temperature in July ranges from 97 °F (36 °C) at the lower elevations down to 78 °F (26 °C) at the higher elevations. In the colder months of November to March, many cities in New Mexico can have nighttime temperature lows in the teens above zero, or lower. The highest temperature recorded in New Mexico was 122 °F (50 °C) at the Waste Isolation Pilot Plant (WIPP) near Loving on June 27, 1994, and the lowest recorded temperature is −50 °F (−46 °C) at Gavilan on February 1, 1951.