Recognizes five major climates based on temperature and precipitation averages:
Köppen Climate Classification System is the most widely used system for classifying the world's climates based on temperature and precipitation averages
MoisttropicalClimate (A):
High temperatures and precipitation year-round, no dry season
DryClimates (B):
Extremely high temperatures with little precipitation
ContinentalClimates (D):
Found in continental interiors
Characterized by low precipitation and varying temperatures
ColdClimates (E):
Extreme low temperatures
Permanent presence of ice and tundra
HumidMiddleLatitude Climates (C):
Characterized by warm, dry summers and cold, wet winters
Low-Latitude Climate groups are formed by converging trade winds around the equator, leading to tropical air masses
TropicalMoistClimates (AF):
Heavy year-round rainfall
Home to rainforest biomes
Average temperatures are mostly constant
Wet drytropicalClimates (AW):
Transition of very dry-wet season
Dry TropicalClimate (BW):
Trade winds and subtropical high-pressure belt end
Light winds allow rapid evaporation of moisture in high temperatures
Mid-Latitude Climates are formed by converging tropical and polar air masses
DryMid-LatitudeClimates (Bs):
Semi-arid landscapes covered by grasslands
Steppebiome:
Characterized by tall grasses and isolated trees
Experience long periods of drought and rain
MediterraneanClimates (Cs):
Wet winters and very dry summers caused by sinking subtropical air masses
Moistcontinentalclimate (Cf):
Polar and tropical air masses meet
Warm summers and cold winters
Chaparral biome:
Characterized by organisms adapted to long periods
Deciduousforestbiome:
Has four distinct seasons
High-Latitude Climates are dominated by polar and arctic air masses