GRG301K - WEATHER AND CLIMATE
KOPPEN CLIMATE CLASSIFICATION FLOW CHART

PREPARED BY TROY M. KIMMEL, JR.
                             LECTURER, STUDIES IN WEATHER AND CLIMATE
                             MANAGER, WEATHER AND CLIMATE RESOURCE CENTER
                             DEPARTMENT OF GEOGRAPHY, UNIVERSITY OF TEXAS AT AUSTIN

"A" CLIMATES - TROPICAL / HOT

Af: TROPICAL RAINFOREST
     -ALL AVERAGE MONTHLY TEMPS GREATER THAN 18C/64.4F
     -DRIEST MONTH WITH AT LEAST 6CM/2.40" OF PRECIPITATION
     -LOCATIONS:
                 AMAZON RIVER BASIN (SOUTH AMERICA)
                 CONGO RIVER BASIN (AFRICA)
                 EASTERN COAST OF CENTRAL AMERICA
                 EASTERN COAST OF BRAZIL  PHILIPPINES
                 EASTERN COAST OF MADAGASCAR EASTERN INDIA
                 SOUTHERN BANGLADESH  MALAYSIA
                 INDONESIA
     -CONTROLLING FACTORS:
                 HIGH YEAR AROUND INSOLATION/PRECIPITATION RESULT OF ITCZ/DOLDRUMS
                 RISING AIR ALONG TRADE WIND COASTS
     -DISTINGUISHING CHARACTERISTICS:
                 CONSTANT HIGH TEMPERATURES
                 EQUAL LENGTH DAY AND NIGHT
                 LOWEST ANNUAL AVERAGE TEMP RANGES (2-3C/3-5F)
                         OCEAN ISLAND/CENTRAL PACIFIC HAS O DEGREE ANNUAL TEMPERATURE RANGE!
                 EVENLY DISTRIBUTED HVY ANNL PCPN (AVG 250CM/100"; EXTREME UP TO 500CM/250")
                 HIGH AMOUNT OF CLOUD COVER AND HUMIDITY YEAR AROUND

Aw: TROPICAL WET-DRY (LOW SUN DRY) - SAVANNA
     -ALL AVERAGE MONTHLY TEMPS GREATER THAN 18C/64.4F
     -MORE THAN 2 MONTHS HAVE LESS THAN 6CM/2.40" PRECIPITATION
                 DISTINCT DRY SEASON DURING LOW SUN SEASON (WINTER); DISTINCT WET  SEASON
                 HIGH SUN SEASON (SUMMER)
     -LOCATIONS:
                 GENERALLY POLEWARD OF Af CLIMATE AREAS
                 NORTHERN AND EASTERN INDIA
                 INTERIOR MYANMAR (BURMA)
                 INDO-CHINESE PENINSULA
                 NORTHERN AUSTRALIA
                 BORDERLANDS OF CONGO RIVER BASIN (AFRICA)
                 SOUTH CENTRAL AFRICA
                 WESTERN CENTRAL AMERICA
                 LLANOS OF VENEZUELA & CAMPOS OF BRAZIL (SAVANNA)
                 EXTREME SOUTHERN FLORIDA
                 CARIBBEAN ISLANDS
     -CONTROLLING FACTORS:
                 ALTERNATION BETWEEN HIGH SUN ITCZ/DOLDRUMS AND  LOW SUN SUBTROPICAL
                 HIGHS AND TRADES CAUSED BY  SHIFTING WINDS AND PRESSURE BELTS
     -DISTINGUISHING CHARACTERISTICS:
                 DISTINCT HIGH-SUN WET AND LOW-SUN DRY SEASONS
                 RAINFALL AVGS 75-130CM/30-70" (RANGES FROM 180CM/70" RAINFOREST MARGINS..
                                100CM/39" DRIER  MARGINS
                 HIGHEST TEMPERATURE RANGES OF "A" CLIMATE FAMILY

As: TROPICAL WET-DRY (HIGH SUN DRY) - SAVANNA
     -ALL AVERAGE MONTHLY TEMPS GREATER THAN 18C/64.4F
     -MORE THAN 2 MONTHS HAVE LESS THAN 6CM/2.40" PRECIPITATION
                  DISTINCT DRY SEASON DURING HIGH SUN SEASON (SUMMER) - VERY RARE CLIMATE
     -LOCATIONS:
                  EXTREME EASTERN TIP OF SOUTH AMERICA (BRAZIL)
     -CONTROLLING FACTORS:
                 OCEANIC INFLUENCE RESULTS IN THIS RARE CLIMATE TYPE
     -DISTINGUISHING CHARACTERISTICS:
                 DISTINCT HIGH SUN DRY AND LOW SUN WET SEASONS
                 RAINFALL AVGS 75-130CM/30-70" (RANGES FROM 180CM/70" RAINFOREST MARGINS..
                                100CM/39" DRIER  MARGINS
                 HIGHEST TEMPERATURE RANGES OF "A" CLIMATE FAMILY

Am: TROPICAL MONSOON      
     -ALL AVERAGE MONTHLY TEMPS GREATER THAN 18C/64.4F
     -ONE OR MORE MONTHS LESS THAN 6CM/2.40" PRECIPITATION
     -EXCESSIVELY WET DURING RAINY SEASON (VERY PRONOUNCED WET SEASON)
     -LOCATIONS:
                 COASTAL AREAS OF SOUTHWESTERN INDIA
                 SRI LANKA
                 BANGLADESH
                 MYANMAR (BURMA)
                 SOUTHWESTERN AFRICA
                 GUYANA
                 SURINAM
                 FRENCH GUIANA
                 PARTS OF NORTHEAST AND SOUTHEAST BRAZIL
     -CONTROLLING FACTORS:
                 SUMMER ONSHORE, WINTER OFFSHORE AIR MOVEMENT RELATED TO SHIFTING ITCZ
                               AND CHANGING PRESSURE CONDITIONS OVER LARGE  LANDMASSES
                 TRANSITIONAL BETWEEN Af AND Aw TO SOME DEGREE
     -DISTINGUISHING CHARACTERICS:
                 OUTSIDE OF HAWAII, HEAVIEST RAINFALL RECORDS IN WORLD  EXIST IN THIS CLIMATE
                               CHERRIPUNJI, INDIA - 476" RAIN IN YEAR (40 FEET OF RAIN!!)
                 HEAVY HIGH-SUN RAINFALL (ESPECIALLY W/OROGRAPHIC LIFT)
                 VERY SHORT LOW SUN (WINTER) DROUGHT
                 ANNUAL TEMPERATURE RANGE OF 2-6C/3-10F
                 HIGHEST TEMPERATURE ANNUALLY JUST PRIOR TO RAINY SEASON
                 PRECIPITATION WIDELY RANGES FROM BETWEEN 150-400CM/60-150" ANNUALLY
 

"B" CLIMATES  - ARID/SEMIARID

BWh: DRY/ARID (HOT) - LOW LATITUDE DESERTS
      -EVAPORATION EXCEEDS PRECIPITATION ON AVERAGE
                 PRECIPITATION IS LESS THAN HALF OF POTENTIAL EVAPORATION
      -USUALLY LOWER LATITUDE, HOT DESERT CLIMATE
      -MEAN AVERAGE TEMP IS OVER 18C/64.4F; FROST ABSENT OR INFREQUENT WINTER
      -LOCATIONS:
                 NORTHERN MEXICO/SOUTHWESTERN USA/BAJA CALIFORNIA
                 NORTHERN AFRICA/SAUDI ARABIA/IRAN/WESTERN INDIA
                 CENTRAL/WESTERN AUSTRALIA
                 SOUTHERN AND WESTERN AFRICA
      -DESERTS:
                 SAHARA DESERT
                 SONORIAN DESERT
                 ARABIAN DESERT
                 THAR DESERT (WESTERN INDIA & PAKISTAN)
                 AUSTRALIAN DESERT
                 KALAHARI DESERT

BWk: DRY/ARID (COOL) - MIDDLE LATITUDE DESERTS
      -EVAPORATION EXCEEDS PRECIPITATION ON AVERAGE
                PRECIPITATION IS LESS THAN HALF OF POTENTIAL EVAPORATION
      -USUALLY MID-LATITUDE, COOLER DESERT CLIMATE
      -MEAN AVERAGE TEMP IS BELOW 18C/64.4F; BELOW FREEZING TEMPS WINTER
      -LOCATIONS:
                CASPIAN SEA EASTWARD TO NORTHERN CHINA & MONGOLIA
                PORTIONS OF SOUTHERN SOUTH AMERICA
      -DESERTS:
                RUSSIAN TURKESTAN DESERT
                TAKLA MAKAN DESERT
                GOBI DESERT
                MOHAVE DESERT

APPLIES TO BOTH BWk & BWh:
      -CONTROLLING FACTORS:
                DESCENDING, DIVERGING CIRCULATION OF SUBTROPICAL HIGHS
                CONTINENTALITY OFTEN LINKED WITH RAIN SHADOW LOCATIONS
      -DISTINGUISHING CHARACTERISTICS:
                ARIDITY, LOW RELATIVE HUMIDITY
                IRREGULAR AND UNRELIABLE RAINFALL LESS THAN 25CM/10"..OFTEN MUCH LESS
                GREATEST PERCENTAGE OF SUNSHINE OF ALL CLIMATE TYPES
                HIGHEST DIURNAL (DAY TO NIGHT) TEMPERATURE RANGES OF ALL  CLIMATES
                HIGHEST DAILY MAXIMUM TEMPERATURES OF ALL CLIMATE TYPES
                WINDY & BREEZY CONDITIONS
 

BSh: SEMI-ARID, STEPPE  (HOT)
      -EVAPORATION EXCEEDS PRECIPITATION ON AVERAGE
                PRECIPITATION IS MORE THAN HALF BUT LESS THAN POTENTIAL EVAPORATION
      -STEPPE/GRASSLAND/BUNCH GRASSES (WEST TEXAS NORTHWARD)
      -MEAN AVERAGE TEMP IS OVER 18C/64.4F
      -LOCATIONS:
                APPROXIMATELY 13-15 DEGREES NORTH LATITUDE IN AFRICA - SOUTHERN BORDER OF ARID CLIMATE
                20 DEGREES SOUTH LATITUDE SOUTHERN AFRICA
                BORDERLANDS AUSTRALIAN DESERT
                PORTIONS OF SOUTHERN SOUTH AMERICA
                PORTIONS OF INDIA
                BORDERS BWh CLIMATES OF NORTHWESTERN AFRICA, SAUDI ARABIA, WESTERN INDIA

BSk: SEMI-ARID, STEPPE (COOL)      
       -EVAPORATION EXCEEDS PRECIPITATION ON AVERAGE
                PRECIPITATION IS MORE THAN HALF BUT LESS THAN  POTENTIAL EVAPORATION
       -USUALLY MID-LATITUDE, STEPPE/GRASSLAND/BUNCH GRASSES (MONTANA SOUTH)
       -MEAN AVERAGE TEMP IS BELOW 18C/64.4F
       -LOCATIONS:
                 WESTERN GREAT PLAINS OF USA & SOUTH CENTRAL CANADA
                 BORDERS BWh AREAS CASPIAN SEA EASTWARD TO CHINA/MONGOLIA

APPLIES TO BOTH BSh & BSk:
      -CONTROLLING FACTORS:
                 SAME AS DESERTS..USUALLY TRANSITIONAL BETWEEN DESERTS AND HUMID CLIMATES.
      -DISTINGUISHING CHARACTERISTICS:
                 SEMIARID CONDITIONS, ANNUAL RAINFALL DISTRIBUTION SIMILAR TO NEAREST HUMID
                            CLIMATE W/PRECIPITATION BETWEEN 25-50CM/10-20"
                 TEMPERATURES GREATLY VARY W/LATITUDE, ELEVATION & CONTINENTALITY
 

"C" CLIMATES - SUBTROPICAL

Cwa: HUMID SUBTROPICAL - WARM WITH DISTINCTLY DRY WINTER
       -AVERAGE TEMPERATURE OF WARMEST MONTH AVERAGES OVER 22C/72F
       -AVERAGE TEMPERATURE OF COLDEST MONTH IS UNDER 18C/64.4F AND ABOVE  -3C/26.6F
       -WINTER DROUGHT; AT LEAST 10 TIMES AS MUCH PRECIPITATION DURING WETTEST SUMMER
                    MONTH AS IN DRIEST WINTER MONTH.

Cfa: HUMID SUBTROPICAL - EAST COASTS
       -AVERAGE TEMPERATURE OF WARMEST MONTH AVERAGES OVER 22C/72F
       -AVERAGE TEMPERATURE OF COLDEST MONTH IS UNDER 18C/64.4F AND ABOVE  -3C/26.6F
       -YEAR AROUND RAINFALL DISTRIBUTION
 
APPLIES TO BOTH Cwa & Cfa:
      -CONTROLLING FACTORS:
                  EAST COASTAL LOCATIONS BETWEEN 20 & 40 DEGREES NORTH & SOUTH  LATITUDE
                  HUMID, ONSHORE AIR MOVEMENT IN SUMMER, CYCLONIC STORMS IN WINTER
      -LOCATIONS:
                  SOUTHEASTERN UNITED STATES (FLORIDA NORTHWARD TO NORTH CAROLINA AND
                             WESTWARD THROUGH ALL OF OKLAHOMA, EXCEPT PANHANDLE, AS WELL AS
                              CENTRAL AND EAST TEXAS)
                 SOUTHEASTERN SOUTH AMERICA
                 COASTAL SOUTHEASTERN SOUTH AFRICA
                 EASTERN AUSTRALIA
                 EASTERN ASIA (FROM NORTHERN INDIA THROUGH SOUTHERN CHINA TO  SOUTHERN JAPAN
                             WHICH IS Cwa - DRY/WET MONSOONAL)
      -DISTINGUISHING CHARACTERISTICS:
                HIGH HUMIDITY
                SUMMER ARE MUCH LIKE HUMID TROPICS
                FROST WITH POLAR AIR MASSES IN WINTER
                PRECIPITATION HIGHLY VARIABLE; 65-250CM/25-100" YEARLY..DECREASES INLAND
                MONSOONAL INFLUENCE (Cwa) ONLY FOUND IN ASIA
 

Csa: HUMID SUBTROPICAL (MEDITERRANEAN)
       -WARM WITH DISTINCTLY DRY HOT SUMMER W/STRONG CONTINENTAL INFLUENCE
       -AVERAGE TEMP OF COLDEST MONTH IS UNDER 18C/64.4F AND ABOVE -3C/26.6F
       -AT LEAST 3 TIMES AS MUCH PRECIPITATION DURING WETTEST WINTER MONTH AS IN DRIEST
                        SUMMER MONTH (PRECIPITATION IN DRIEST SUMMER MONTH LESS THAN 4CM/1.56")
       -WARMEST MONTH HAS AVERAGE TEMP OVER 22C/71.6F; AT LEAST 4 MONTHS  HAVE AVERAGE TEMPS OVER 10C/50F

Csb: HUMID SUBTROPICAL (MEDITERRANEAN)
       -COOL WITH DISTINCTLY DRY COOL SUMMER W/STRONG MARITIME INFLUENCE
       -AVERAGE TEMP OF COLDEST MONTH IS UNDER 18C/64.4F AND ABOVE -3C/26.6F
       -AT LEAST 3 TIMES AS MUCH PRECIPITATION DURING WETTEST WINTER MONTH AS IN DRIEST
                        SUMMER MONTH (PRECIPITATION IN DRIEST SUMMER MONTH LESS THAN 4CM/1.56")
       -NO MONTH WITH AVERAGE TEMP OVER 22C/71.6F; AT LEAST 4 MONTHS HAVE AVERAGE TEMPS OVER 10C/50F

APPLIES TO BOTH Csa & Csb:
       -LOCATIONS:
                        CENTRAL, COASTAL AREAS OF CALIFORNIA
                        CENTRAL, COASTAL CHILE
                        MEDITERRANEAN SEA BORDERLANDS
                        IRANIAN HIGHLANDS
                        CAPETOWN AREA OF SOUTH AFRICA
                        SOUTHERN AND SOUTHWESTERN AREAS OF AUSTRALIA
       -CONTROLLING FACTORS:
                        WEST COAST LOCATIONS BETWEEN 30 AND 40 N & S LATITUDES
                        ALTERNATION BETWEEN SUBTROPICAL HIGHS IN SUMMER  AND WESTERLIES IN WINTER
       -DISTINGUISHING CHARACTERISTICS:
                        MILD, MOIST WINTERS & HOT, DRY SUMMERS (INLAND AREAS) AND FOGGY, COOLER COASTS
                        HIGH PERCENTAGE OF SUNSHINE
                        HIGH SUMMER DIURNAL  RANGE (RANGE BETWEEN HIGH & LOW TEMPERATURES OF DAY)
                        FROST DANGER IN WINTER SEASON

 
Cfb: MARINE WEST COAST - MILD
      -AVERAGE TEMPERATURE OF ALL MONTHS IS BELOW 22C/71.6C
      -AT LEAST 4 MONTHS WITH AN AVERAGE TEMPERATURE ABOVE 10C/50F
      -AVERAGE TEMPERATURE OF COLDEST MONTH IS UNDER 18C/64.4F AND ABOVE -3C/26.6C
      -RAINFALL EQUALLY SPREAD THROUGHOUT YEAR

Cfc: MARINE WEST COAST - COOL
     -AVERAGE TEMPERATURE OF ALL MONTHS IS BELOW 22C/71.6C
     -1 TO 3 MONTHS WITH AN AVERAGE TEMPERATURE ABOVE 10C/50F
     -AVERAGE TEMPERATURE OF COLDEST MONTH IS UNDER 18C/64.4F AND ABOVE -3C/26.6F
     -RAINFALL EQUALLY SPREAD THROUGHOUT YEAR

APPLIES TO BOTH Cfb & Cfc:
      -CONTROLLING FACTORS:
      -WEST COAST LOCATION (AROUND YEAR INFLUENCE OF THE WESTERLIES)
      -WARM OCEAN CURRENTS ALONG MOST OF THE COASTS
      -LOCATIONS:
                   COASTAL OREGON, WASHINGTON, BRITISH COLUMB AND SOUTHERN ALASKA
                   NORTHWEST EUROPE
                   SOUTHERN CHILE
                   INTERIOR SOUTH AFRICA
                   SOUTHEAST AUSTRALIA AND NEW ZEALAND
      -DISTINGUISHING CHARACTERISTICS:
                   MILD WINTERS AND MILD SUMMERS WITH LOW ANNUAL TEMPERATURE RANGE
                   HEAVY CLOUD COVER
                   HIGH HUMIDITY
                   FREQUENT CYCLONIC STORMS WITH PROLONGED RAIN, DRIZZLE OR FOG
                   3 TO 4 MONTH FROST PERIOD DURING THE WINTER SEASON
 

"D" CLIMATES - TEMPERATE      

Dfa: HUMID CONTINENTAL HOT SUMMERS W/YEAR AROUND PRECIPITATION
      -AVERAGE TEMPERATURE OF COLDEST MONTH IS -3C/26.6F OR BELOW
      -AVERAGE TEMPERATURE OF WARMEST MONTH IS GREATER THAN 10C/50F
      -RAINFALL EQUALLY SPREAD THROUGHOUT YEAR

Dwa: HUMID CONTINENTAL HOT SUMMERS W/DRY WINTERS
      -AVERAGE TEMPERATURE OF COLDEST MONTH IS -3C/26.6F OR BELOW
      -AVERAGE TEMPERATURE OF WARMEST MONTH IS GREATER THAN 10C/50F
      -WINTERS DRY; AT LEAST TEN TIMES AS MUCH PRECIPITATION DURING THE  WETTEST SUMMER MONTH
                         AS IN THE DRIEST WINTER MONTH

APPLIES TO BOTH Dfa & Dwa:
      -CONTROLLING FACTORS:
                     LOCATION IN THE LOWER MIDDLE LATITUDES (35 TO 45 DEGREES)
                     CYCLONIC STORMS ALONG THE POLAR FRONT
                     PREVAILING WESTERLIES
                     CONTINENTALITY PREVAILS
                     POLAR ANTICYCLONE IN WINTER (RESULTS IN Dwa CLIMATE TYPE) - HIGH CONTINENTALITY
      -LOCATIONS:
                     EASTERN AND MIDWESTERN UNITED STATES (ATLANTIC COAST TO  THE 100TH  MERIDIAN
                                 POLEWARD OF THE "C" CLIMATE TYPE)
                     EAST CENTRAL EUROPE
                     NORTHERN CHINA, MANCHURIA, NORTHERN KOREA, AND HONSHU
      -DISTINGUISHING CHARACTERISTICS:
                     HOT, OFTEN HUMID SUMMERS; OCCASIONAL WINTER COLD WAVES
                     RATHER LARGE ANNUAL TEMPERATURE RANGES
                     GREAT WEATHER VARIABILITY ON ESPECIALLY YEARLY BASIS
                     PRECIPITATION 50-115CM/20-45" ANNUALLY DECREASING INLAND AND POLEWARD
                     AN APPROXIMATE 140-200 DAY GROWING SEASON
 

Dfb: HUMID CONTINENTAL MILD SUMMER WITH YEAR AROUND RAINFALL
      -AVERAGE TEMPERATURE OF COLDEST MONTH IS -3C/26.6F OR BELOW
      -AVERAGE TEMPERATURE OF WARMEST MONTH IS GREATER THAN 10C/50F
      -NO MONTH WITH AVERAGE TEMPERATURE OVER 22C/71.6F
      -RAINFALL EQUALLY SPREAD THROUGHOUT YEAR

Dwb: HUMID CONTINENTAL MILD SUMMER WITH DRY WINTERS
      -AVERAGE TEMPERATURE OF COLDEST MONTH IS -3C/26.6F OR BELOW
      -AVERAGE TEMPERATURE OF WARMEST MONTH IS GREATER THAN 10C/50F
      -NO MONTH WITH AVERAGE TEMPERATURE OVER 22C/71.6F
      -AT LEAST 10 TIMES AS MUCH PRECIPITATION IS THE WETTEST SUMMER MONTH AS IN DRIEST WINTER MONTH

APPLIES TO BOTH Dfb & Dwb:
      -CONTROLLING FACTORS:
                   LOCATIONS IN THE MID-LATITUDES (45 TO 55 DEGREES)
                   CYCLONIC STORMS ALONG THE POLAR FRONT
                   PREVAILING WESTERLIES
                   CONTINENTALITY PREVAILS
                   POLAR ANTICYCLONE IN WINTER (RESULTS IN Dwb CLIMATE TYPE)
      -LOCATIONS:
                   NEW ENGLAND, THE GREAT LAKES REGION, AND SOUTH CENTRAL CANADA
                   SOUTHEASTERN SCANDINAVIA
                   EASTERN EUROPE
                   WEST CENTRAL ASIA
                   EASTERN MANCHURIA & ASIA
                   HOKKAIDO
      -DISTINGUISHING CHARACTERISTICS:
                  MODERATE SUMMERS
                  LONG WINTERS WITH FREQUENT SPELLS OF CLEAR, COLD WEATHER
                  LARGE ANNUAL TEMPERATURE RANGES
                  VARIABLE WEATHER W/ LESS TOTAL PPRECIPITATION THAN AREAS SOUTH
                  AN APPROXIMATE 90-130 DAY GROWING SEASON
 

Dfc: SUBARCTIC WITH COOL SUMMERS AND YEAR AROUND RAINFALL
      -AVERAGE TEMPERATURE OF COLDEST MONTH IS -3C/26.6F OR BELOW
      -AVERAGE TEMPERATURE OF WARMEST MONTH IS GREATER THAN 10C/50F
      -1 TO 3 MONTHS WITH AVERAGE TEMPERATURES ABOVE 10C/50F
      -RAINFALL EQUALLY SPREAD THROUGHOUT YEAR

Dfd: SUBARCTIC WITH COLD WINTERS AND YEAR AROUND RAINFALL
      -COLDEST MONTH HAS AVERAGE TEMPERATURE OF -38C/-36.4F OR BELOW
      -AVERAGE TEMPERATURE OF WARMEST MONTH IS GREATER THAN 10C/50F
      -RAINFALL EQUALLY SPREAD THROUGHOUT YEAR

Dwc: SUBARCTIC WITH COOL SUMMERS AND DRY WINTERS
      -AVERAGE TEMPERATURE OF COLDEST MONTH OF -3C/26.6F OR BELOW
      -AVERAGE TEMPERATURE OF WARMEST MONTH IS GREATER THAN 10C/50F
      -1 TO 3 MONTHS WITH AVERAGE TEMPERATURES ABOVE 10C/50F
      -AT LEAST 10 TIMES AS MUCH PRECIPITATION IN THE WETTEST SUMMER MONTH AS IN DRIEST WINTER MONTH

Dwd: SUBARCTIC WITH COLD WINTERS AND DRY WINTERS
      -COLDEST MONTH HAS AVERAGE TEMPERATURE OF -38C/-36.4F OR BELOW
      -AVERAGE TEMPERATURE OF WARMEST MONTH IS GREATER THAN 10C/50F
      -AT LEAST 10 TIMES AS MUCH PRECIPITATION IN THE WETTEST SUMMER MONTH AS IN DRIEST WINTER MONTH

APPLIES TO Dfc, Dwc, Dfd & Dwd:
      -CONTROLLING FACTORS:
                  LOCATION IN THE HIGHER MIDDLE LATITUDE (50 TO 70 DEGREES)
                  WESTERLIES IN SUMMER
                  STRONG POLAR ANTICYCLONE IN WINTER (CREATES Dwc & Dwd CLIMATE TYPES)
                  OCCASIONAL CYCLONIC STORMS
                  EXTREME CONTINENTALITY
      -LOCATIONS:
                  NORTHERN NORTH AMERICA (FROM NEWFOUNDLAND TO ALASKA)
                  NORTHERN EURASIA (FROM SCANDINAVIA THROUGH SIBERIA TO THE  BERING SEA AND THE SEA OF OKHOTSK)
      -DISTINGUISHING CHARACTERISTICS:
                  BRIEF, COOL SUMMERS AND LONG, BITTERLY COLD WINTERS
                  LARGEST ANNUAL TEMPERATURE RANGES
                  LOWEST TEMPERATURES OUTSIDE OF ANTARCTICA
                  LOW PRECIPITATION OF 25-50CM/10-20" ANNUALLY
                  UNRELIABLE 50-80 DAY GROWING SEASON
                  PERMAFROST COMMON
 
 
 

"E" CLIMATES - POLAR

ET: TUNDRA CLIMATE
      -AVERAGE TEMP OF WARMEST MONTH IS BELOW 10C/50F BUT IS GREATER THAN  0C/32F
      -PRECIPITATION EXCEEDS POTENTIAL EVAPORATION
      -LOCATIONS:
                    ARCTIC OCEAN BORDERLANDS OF NORTH AMERICA, GREENLAND AND EURASIA
                    ANTARCTIC PENINSULA
                    SOME POLAR ISLANDS
     -CONTROLLING FACTORS:
                    LOCATION IN HIGH LATITUDES
                    SUBSIDENCE AND DIVERGENCE OF THE POLAR ANTICYCLONE
                    PROXIMITY TO COASTS
     -DISTINGUISHING CHARACTERISTICS:
                    SUMMERLESS, AT LEAST 9 MONTHS AVERAGE BELOW FREEZING
                    VERY LOW EVAPORATION
                    PRECIPITATION USUALLY BELOW 25.5CM/10"
                    COASTAL FOG
                    STRONG WINDS

EF: ICECAP CLIMATE
       -AVERAGE TEMP OF WARMEST MONTH IS 0C/32F OR BELOW
       -PRECIPITATION EXCEEDS POTENTIAL EVAPORATION
       -LOCATIONS:
                    INTERIOR GREENLAND
                    MOST OF ANTARCTICA (EXCEPT ANTARCTIC PENINSULA)
                    PERMANENTLY FROZEN PORTIONS OF THE ARCTIC OCEAN AND
                    ASSOCIATED ISLANDS
      -CONTROLLING FACTORS:
                    LOCATIONS IN HIGH LATITUDES AND INTERIORS OF LANDMASSES
                    YEAR-AROUND INFLUENCE OF THE POLAR ANTICYCLONE
                    ICE COVER
                    ELEVATION OF ICE DOME
     -DISTINGUISHING CHARACTERISTICS:
                    SUMMERLESS, ALL MONTHS AVERAGE BELOW FREEZING
                    WORLD'S COLDEST TEMPERATURES
                    EXTREMELY MEAGER PRECIPITATION IN FORM OF SNOW, EVAPORATION EVEN LESS
 
 

"H" CLIMATES - HIGHLAND AREAS

H: HIGHLAND CLIMATE
      -DUE TO MOUNTAINOUS AREAS, CAN ENCOMPASS ANY OF THE ABOVE CLIMATE  CLASSIFICATIONS
      -VERY COMPLEX AND TIGHT KNIT CLIMATIC ZONE.
      -TEMPERATURE DECREASE WITH INCREASING ALTITUDE = AVG 3.6F/1000FT
      -ZONES OF CLIMATE IN HIGHLAND REGIONS BASED ON CHANGES IN TEMPERATURE WITH ELEVATION THAT
                       ROUGHLY COORESPOND TO KOPPENS CLIMATIC ZONES BASED ON THE CHANGE IN TEMPERATURE
                       WITH LATITUDE...WITH ONE IMPORTANT  EXCEPTION...SEASONS ONLY EXIST IN HIGHLANDS IF THEY
                       ALSO EXIST IN THE  NEARBY LOWLAND REGIONS. (EXAMPLE: ALTHOUGH ZONES OF INCREASINGLY
                       COOLER TEMPERATURES OCCUR AT PROGRESSIVELY HIGHER ELEVATIONS IN THE TROPICAL
                       REGIONS ("A" CLIMATES), THE SEASONAL CHANGES OF KOPPENS "C", "D" AND "E" CLIMATES
                       ARE NOT PRESENT.
      -CONTROLLING FACTORS:
                       ELEVATION
                       EXPOSURE
 
 
 

TMK
03JUL00