Seasons refer to the four distinct periods of the year, each characterized by specific climate conditions and natural phenomena. These periods—spring, summer, autumn (or fall), and winter—are primarily determined by the Earth’s axial tilt and orbit around the sun, leading to variations in sunlight and temperature.
Spring typically signifies renewal and growth, as temperatures begin to rise and plants begin to bloom. Summer is characterized by warmer temperatures and longer days, often associated with vibrant life and activity. Autumn marks the transition from summer to winter, often noted for the cooling temperatures and the shedding of leaves from deciduous trees. Winter is marked by cold temperatures, shorter days, and, in many regions, the presence of snow or frost.
The concept of seasons is significant in various fields, including agriculture, ecology, and culture, influencing human activities, wildlife behaviors, and the cyclical patterns of natural life. In temperate regions, these seasons are clearly defined, whereas in tropical areas, the changes may be less pronounced, often resulting in wet and dry seasons instead.