What Are Climate Zones? How Are They Categorized? (2024)

Earth's climate zones—the horizontal belts of different climates that encircle the planet—consist of tropical, dry, temperate, continental, and polar zones.

These major climate zones exist thanks to Earth’s diverse landscapes. Each country is located at a specific latitude and elevation, next to either a particular landmass, body of water, or both. As a result, they are impacted differently by certain ocean currents or winds. Likewise, a location’s temperatures and precipitation patterns are influenced in a unique way. And it’s this unique mix of influences that yields different climate types.

As abstract as climate zones may seem, they remain a key tool for understanding earth’s many biomes, tracking the extent of climate change, determining plant hardiness, and more.

The Discovery of Earth’s Climate Zones

The concept of climate zones dates back to ancient Greece. In the 6th century B.C., a pupil of Pythagoras was the first to suggest the idea.

A few centuries later, the famous Greek scholar Aristotle hypothesized that the earth’s five circles of latitude (the Arctic Circle, Tropic of Capricorn, Tropic of Cancer, Equator, and Antarctic Circle) divided the Northern and Southern hemispheres into a torrid, temperate, and frigid zone. However, it was Russian-German scientist Wladimir Köppen who, in the early 1900s, created the climate classification scheme we use today.

Because little climate data existed at that time, Köppen, who also studied botany, began observing the relationship between plants and climate. If a species of plant needed special temperatures and rainfall to grow, he thought, then a location’s climate could be inferred simply by observing the plant life native to that area.

The Main Climate Zones

Using his botanical hypothesis, Köppen determined that five major climates exist worldwide: tropical, dry, temperate, continental, and polar.

Tropical (A)

Tropical climate zones lie near the Equator and have continually high temperatures and high precipitation. All months have average temperatures above 64 degrees F (18 degrees C), and 59 plus inches (1,499 mm) of annual rainfall is normal.

Dry (B)

Dry or arid climate zones experience high temperatures year-round, but little annual precipitation.

Temperate (C)

Temperate climates exist in Earth’s middle latitudes and are influenced by both the land and water that surrounds them. In these zones, wider temperature ranges are experienced throughout the year, and seasonal variations are more distinct.

Continental (D)

Continental climates also exist in the mid-latitudes, but as the name implies, they’re generally found at the interiors of large landmasses. These zones are characterized by temperatures that swing from cold in winter to warm in summer, and moderate precipitation that occurs mostly in the warmer months or as snowstorms in the colder months.

Polar (E)

Polar climate zones are too harsh to support vegetation. Both winters and summers are very cold, and the warmest month has an average temperature below 50 degrees F (10 degrees C).

In later years, scientists added a sixth major climate zone—the highland climate. It includes the variable climates found in the world’s high mountain regions and plateaus.

Regional Climate Zones

Köppen’s five climate groups do a good job of telling us where the world’s hottest, coldest, and in-between climates are, but they don’t capture how local geographical features, such as mountains or lakes, influence seasonal precipitation and temperatures. Realizing this, Köppen split his main categories into subcategories called regional climates.