In Arizona, as the seasons transition from summer to winter, abiotic factors such as temperature, precipitation, and soil moisture vary significantly. Summer temperatures can soar above 100°F, while winter temperatures can drop to near freezing, particularly at higher elevations. Precipitation typically increases during the winter months due to intermittent storms, contrasting with the drier, monsoon-influenced summer. Additionally, soil moisture levels fluctuate, generally decreasing in summer and increasing in winter due to rainfall and cooler temperatures.
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