Mid-latitudes, such as much of the U.S., typically experience four distinct seasons: spring, summer, fall, and winter.

This is because mid-latitude regions receive varying amounts of sunlight throughout the year due to the Earth's tilt, creating noticeable changes in temperature and weather. As a result, these regions experience the full cycle of seasons, each with its characteristics, such as warm summers, cold winters, and transitional spring and fall months. This seasonal variation is a hallmark of temperate climates, unlike tropical areas with year-round warmth or polar regions with extreme cold.