McAlester Weather
Loading current temperature, humidity, wind, and air quality context for McAlester, Oklahoma, United States.
Loading current temperature, humidity, wind, and air quality context for McAlester, Oklahoma, United States.
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McAlester, Oklahoma, sits within the rolling hills of the Ozark Plateau in Pittsburg County, a region historically shaped by coal mining and agriculture. Located at 34.9257° N, -95.7734° W, the city’s elevation ranges around 750 feet, contributing to localized weather patterns. The North Fork of the Canadian River meanders nearby, influencing humidity and occasionally trapping pollutants during stable atmospheric conditions. McAlester’s urban character is defined by a blend of historic downtown architecture and more sprawling residential areas, reflecting its growth as a regional trade and transportation hub. Surrounding McAlester is a landscape transitioning from forested hills to prairie grasslands, with significant agricultural activity – primarily cattle ranching and hay production – to the south and west. To the east, remnants of the once-dominant coal industry are visible in reclaimed mine lands. This mix of land use, coupled with the city’s position within a broader regional air basin, impacts air quality. The urban-rural gradient is relatively sharp, with noticeable differences in pollutant concentrations between the city center and outlying rural areas. Prevailing winds generally flow from the south, potentially transporting pollutants from agricultural sources northward towards McAlester. The terrain, while not mountainous, can create localized channeling effects, concentrating pollutants in valleys and low-lying areas.
McAlester’s air quality follows a distinct seasonal pattern. Spring (March-May) often sees elevated particulate matter due to agricultural burning and windblown dust from exposed soils as fields are prepared for planting. Rainfall is generally sufficient to mitigate prolonged pollution episodes. Summer (June-August) typically offers the cleanest air, with higher temperatures promoting atmospheric mixing and frequent convective thunderstorms effectively scouring the atmosphere. However, ozone formation can be a concern on hot, stagnant days. Autumn (September-November) brings a return of agricultural activity, with harvest operations contributing to dust and particulate pollution. Critically, temperature inversions become more frequent during this period, trapping pollutants near the ground. Winter (December-February) is often characterized by the highest pollution levels. Reduced sunlight and colder temperatures inhibit pollutant dispersion, while residential wood burning for heating significantly increases particulate matter concentrations. Sensitive groups – children, the elderly, and those with respiratory conditions – should limit outdoor exertion during inversion events, particularly in November-February. Monitoring wind direction is crucial; southerly winds can bring pollutants from larger regional sources. Avoiding strenuous activity during peak pollution times, typically early mornings and evenings in winter, is advisable.
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