Clima en fayetteville arkansas In the fall (September-November), the temperatures begin to cool down, with the average high temperature in the mid-70s and the average low temperature in the mid-50s. The fall months are also relatively dry, with an average of 2-3 inches of rainfall per month. Winter (December-February) is the driest time of year in Fayetteville, with an average of 2 inches of rainfall per month. The average high temperature during the winter months is around 50 degrees Fahrenheit, with the average low temperature in the mid-30s. Snow is rare in Fayetteville, but the city does see an average of 2-3 inches of snowfall per year. Spring (March-May) is a transitional season in Fayetteville, with temperatures gradually warming up and rainfall increasing. The average high temperature in the spring is around 70 degrees Fahrenheit, with the average low temperature in the mid-50s. The average rainfall in the spring is around 4-5 inches per month. Fayetteville's humid subtropical climate means that the city experiences all four seasons, but the summers are hot and humid, and the winters are mild and relatively dry. The city's location in the Ozark Mountains also contributes to its climate, with the mountains providing some protection from extreme temperatures and weather patterns. It is important to note that while this is the general climate pattern for Fayetteville, Arkansas, individual years can vary and it is always possible for temperatures and precipitation to be above or below average. Additionally, climate change may be affecting the long-term climate patterns in the region, leading to hotter summers and milder winters. Weather radar, also known as Doppler radar, uses radio waves to detect precipitation and determine its motion. The radar antenna emits a short burst of microwave radiation, which is reflected back to the radar by precipitation particles such as raindrops, snowflakes, or hailstones. The radar receiver then measures the time delay between the transmitted and received signals and the strength of the returned signal to estimate the location, intensity, and motion of the precipitation.