Subtrophic

Subtrophic is a term used in geography and ecology to describe regions that lie between the tropics and the temperate zones. These areas experience a transitional climate with characteristics of both tropical and temperate environments. They are typically located on the poleward sides of the tropics, generally between latitudes 23.5 and 40 degrees north and south of the equator.

The climate in subtrophic regions is often characterized by hot, humid summers and mild, wet winters. While they do not experience the extreme cold of temperate zones or the consistent high temperatures of the tropics, they can have distinct seasonal variations. Precipitation patterns can vary significantly within subtrophic zones, with some areas receiving abundant rainfall throughout the year and others experiencing dry seasons.

Vegetation in subtrophic areas is diverse, often a mix of tropical and temperate plant species. This can include evergreen forests, deciduous trees, and various shrubs and grasses adapted to the seasonal changes. Subtrophic climates are often favorable for agriculture, supporting a wide range of crops. Examples of subtrophic regions include the southeastern United States, the Mediterranean basin, parts of eastern Asia, and southern Australia. The specific characteristics of a subtrophic region can be influenced by factors such as ocean currents, proximity to large bodies of water, and elevation.