U.S. Climate Zones Map
Discover the diverse climate zones of the United States using the Köppen climate classification system. From the arctic tundra of Alaska to the tropical warmth of Hawaii and southern Florida, explore how temperature, precipitation, and seasonal patterns create distinct climate regions across America.
Major U.S. Climate Zones
Humid Subtropical
CfaHot, humid summers and mild to cool winters with year-round precipitation.
- States: Southeast U.S. (Georgia, Alabama, Mississippi, Louisiana, South Carolina, North Carolina, Virginia, Arkansas, Tennessee)
- Average Temperature: 50-70°F (10-21°C)
- Precipitation: 40-60 inches/year
- Characteristics: Heavy summer thunderstorms, occasional winter snow in northern areas
Humid Continental
Dfa/DfbLarge temperature differences between summer and winter, four distinct seasons.
- States: Northeast and Midwest (New York, Pennsylvania, Ohio, Michigan, Wisconsin, Minnesota, Illinois, Indiana)
- Average Temperature: 40-55°F (4-13°C)
- Precipitation: 30-40 inches/year
- Characteristics: Warm summers, cold snowy winters, colorful fall foliage
Semiarid/Steppe
BSkModerate precipitation, grassland climate with hot summers and cold winters.
- States: Great Plains (Montana, Wyoming, Colorado, Kansas, Oklahoma, parts of Texas, New Mexico)
- Average Temperature: 45-60°F (7-16°C)
- Precipitation: 10-20 inches/year
- Characteristics: Short grass prairies, occasional droughts, strong winds
Arid/Desert
BWk/BWhVery low precipitation, extreme temperature variations between day and night.
- States: Southwest (Nevada, Arizona, parts of California, Utah, New Mexico)
- Average Temperature: 55-75°F (13-24°C)
- Precipitation: Less than 10 inches/year
- Characteristics: Sparse vegetation, dramatic landscapes, intense sunshine
Mediterranean
Csa/CsbDry summers and mild, wet winters characteristic of California coast.
- States: California coast, parts of Oregon
- Average Temperature: 55-65°F (13-18°C)
- Precipitation: 15-30 inches/year (mostly winter)
- Characteristics: Long dry summers, ideal for agriculture, wildfire season
Oceanic/Marine
CfbMild temperatures year-round with frequent cloud cover and precipitation.
- States: Pacific Northwest (Washington, Oregon coast)
- Average Temperature: 50-60°F (10-15°C)
- Precipitation: 40-100+ inches/year
- Characteristics: Overcast skies, lush vegetation, temperate rainforests
Subarctic
Dfc/DscVery cold winters, short cool summers, limited precipitation.
- States: Alaska interior, northern Minnesota
- Average Temperature: 20-35°F (-7 to 2°C)
- Precipitation: 10-20 inches/year
- Characteristics: Long, harsh winters, permafrost in some areas, taiga forests
Tundra
ETExtremely cold year-round, no true summer, permanently frozen subsoil.
- States: Northern Alaska, Alaska coastal areas
- Average Temperature: Below 32°F (0°C) most of year
- Precipitation: Less than 10 inches/year
- Characteristics: Permafrost, treeless landscape, brief growing season
Tropical
Af/AmWarm temperatures year-round with significant rainfall.
- States: Hawaii, southern tip of Florida
- Average Temperature: 70-80°F (21-27°C)
- Precipitation: 60-200+ inches/year
- Characteristics: No winter season, lush rainforests, high humidity
Understanding Köppen Climate Classification
The Köppen climate classification system, developed by climatologist Wladimir Köppen in 1900, is the most widely used system for classifying the world's climates. It categorizes climates based on average monthly temperature and precipitation patterns.
Climate Classification System
The system uses a letter code system:
| Code | Climate Type | Description |
|---|---|---|
| A | Tropical | Average temperature of coldest month above 64°F (18°C) |
| B | Arid | Evaporation exceeds precipitation |
| C | Temperate | Coldest month between 27-64°F (-3 to 18°C) |
| D | Continental | Coldest month below 27°F (-3°C), warmest above 50°F (10°C) |
| E | Polar | Warmest month below 50°F (10°C) |
Precipitation Patterns (Second Letter)
- f: Fully humid - Precipitation throughout the year
- s: Summer dry - Mediterranean pattern
- w: Winter dry - Monsoon pattern
- m: Monsoonal - Short dry season compensated by heavy monsoon rains
- W: Desert (arid)
- S: Steppe (semiarid)
Temperature Patterns (Third Letter)
- a: Hot summer - Warmest month above 72°F (22°C)
- b: Warm summer - Warmest month below 72°F (22°C)
- c: Cool summer - Fewer than 4 months above 50°F (10°C)
- d: Very cold winter - Coldest month below -36°F (-38°C)
- h: Hot arid - Mean annual temperature above 64°F (18°C)
- k: Cold arid - Mean annual temperature below 64°F (18°C)
Climate Zones by State
States with Multiple Climate Zones
Many large states span multiple climate zones due to variations in elevation, latitude, and proximity to water bodies:
California - The most climatically diverse state:
- Mediterranean (Csa/Csb) - Coastal areas
- Desert (BWh) - Southeastern California, Death Valley
- Semiarid (BSk) - Central Valley regions
- Highland (H) - Sierra Nevada mountains
- Oceanic (Cfb) - Northern coastal areas
Texas - Climate varies dramatically across the state:
- Humid Subtropical (Cfa) - Eastern Texas
- Semiarid (BSh/BSk) - Western Texas
- Desert (BWh) - Far western Texas
- Oceanic (Cfa) - Coastal areas
Alaska - Extreme climate diversity:
- Tundra (ET) - North Slope, Arctic coast
- Subarctic (Dfc/Dsc) - Interior regions
- Oceanic (Cfb/Cfc) - Southeast Alaska panhandle
- Subarctic oceanic (Dfc) - South-central coast
States with Uniform Climate
Some smaller states have relatively uniform climate zones:
- Hawaii: Tropical (Af/Am) throughout
- Florida: Primarily humid subtropical (Cfa), with tropical (Af) in the southern tip
- Rhode Island: Humid continental (Dfa) throughout
- Delaware: Humid subtropical (Cfa) throughout
Climate Change and Shifting Zones
Climate zones are not static. Scientific evidence shows that climate zones in the United States are shifting due to global climate change.
Observed Changes
- Northward Migration: Climate zones are shifting northward, with southern characteristics moving into traditionally cooler areas
- USDA Hardiness Zones: Plant hardiness zones have shifted significantly, with many areas now 5-10°F warmer than in 1990
- Precipitation Patterns: Changes in rainfall distribution affecting climate classifications
- Extreme Events: Increased frequency of extreme weather events challenging traditional classifications
Regional Impacts
Southwest:
- Expansion of arid and semiarid zones
- Longer and more severe drought periods
- Earlier snowmelt in mountain regions
Southeast:
- Longer, hotter summers
- Changes in precipitation intensity
- Increased tropical characteristics in southern areas
Northeast:
- Warmer winters with less snow
- Earlier spring onset
- Shift toward more temperate characteristics
Alaska:
- Rapid warming, especially in Arctic regions
- Shrinking tundra zones
- Thawing permafrost
- Changes in subarctic forest boundaries
Microclimates and Local Variations
While broad climate zones provide a general framework, local geography creates microclimates that can differ significantly from the surrounding region.
Factors Creating Microclimates
Elevation:
- Temperature drops approximately 3.5°F per 1,000 feet of elevation gain
- Mountain ranges create dramatically different climates on their eastern and western slopes
- Highland climates exist within states that are otherwise temperate or arid
Urban Heat Islands:
- Cities can be 5-15°F warmer than surrounding rural areas
- Affects growing seasons, energy use, and air quality
- Major metro areas like Phoenix, Las Vegas, and Los Angeles show significant heat island effects
Water Bodies:
- Great Lakes create "lake effect" snow in winter and cooler summers
- Coastal areas have moderated temperatures year-round
- Ocean currents influence coastal climates (California Current, Gulf Stream)
Rain Shadows:
- Mountain ranges block moisture, creating dry conditions on the leeward side
- Sierra Nevada creates rain shadow over Nevada
- Cascade Range affects eastern Washington and Oregon
- Rockies influence Great Plains climate
Notable Microclimates
San Francisco Bay Area: Contains numerous microclimates within a small region, from foggy coast to warm inland valleys, often varying dramatically within just a few miles.
Puget Sound: Protected waterways create milder, drier conditions than the surrounding Pacific Northwest rainforest climate.
Willamette Valley, Oregon: Rain shadow effect from Coast Range creates drier, warmer conditions ideal for wine production.
Climate and Human Activity
Population Distribution
Climate zones significantly influence where Americans choose to live:
- Temperate Zones: Highest population densities in humid subtropical and humid continental zones
- Coastal Areas: Mild oceanic and Mediterranean climates attract large populations
- Arid Zones: Lower population density but growing rapidly (Phoenix, Las Vegas) due to air conditioning
- Extreme Climates: Sparse population in tundra, subarctic, and hot desert regions
Economic Activities
Climate zones dictate agricultural possibilities and economic development:
Agriculture:
- Humid subtropical: Cotton, tobacco, rice, soybeans
- Mediterranean: Grapes, citrus, almonds, avocados
- Humid continental: Corn, wheat, dairy farming
- Semiarid: Wheat, cattle ranching
- Tropical: Sugarcane, pineapples, coffee (Hawaii)
Energy Use:
- Humid continental: High heating costs in winter
- Humid subtropical: High cooling costs in summer
- Desert: Extreme cooling demands, solar energy potential
- Oceanic: Moderate energy use year-round
Tourism and Recreation
Climate zones create diverse tourism opportunities:
- Winter Sports: Subarctic and highland climates (Alaska, Colorado, Vermont)
- Beach Tourism: Tropical and subtropical climates (Florida, Hawaii, California)
- Fall Foliage: Humid continental climate (New England states)
- Desert Recreation: Arid climates (Arizona, Utah, Nevada)
Frequently Asked Questions
What U.S. state has the most diverse climate?
California has the most diverse climate, featuring Mediterranean, desert, semiarid, oceanic, and highland climates all within one state. This diversity is due to its large size, varied topography, and range of latitudes and elevations.
Which climate zone covers the largest area in the U.S.?
The semiarid/steppe climate (BSk) covers the largest continuous area, spanning much of the Great Plains and interior West. However, if we include subarctic climates in Alaska, that would be the most extensive single climate type by total area.
Why doesn't the entire West Coast have the same climate?
The West Coast climate varies dramatically due to latitude, ocean currents, and topography. The Pacific Northwest has an oceanic climate with heavy rainfall, California has a Mediterranean climate with dry summers, and Southern California transitions to semiarid and desert climates. The California Current brings cool water to the coast, while mountain ranges create rain shadows inland.
How does climate affect where people live in the U.S.?
Climate is a major factor in population distribution. Most Americans live in temperate climates (humid subtropical and humid continental zones). Extreme climates like arctic tundra, hot deserts, and subarctic regions have much lower population densities. However, technology like air conditioning has enabled population growth in previously challenging climates like the desert Southwest.
Are U.S. climate zones changing?
Yes, climate zones are shifting due to global climate change. Many areas are experiencing warmer temperatures, altered precipitation patterns, and earlier springs. USDA plant hardiness zones have shifted northward, and some regions are transitioning between climate classifications. These changes affect agriculture, ecosystems, and human activities.