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Koppen Classification System
Name the 5 categories in the 
Koppen Classification System.
Citation 
Pidwirny, M. (2011). 
Köppen Climate 
Classification System. 
Retrieved from 
http://www.eoearth.org/vi 
ew/article/162263 
• 1. Humid, Tropical Climate 2. Dry Climate 3. Humid Mid Latitude Climate 4. Polar climate 5. Highlands Climate
Humid Tropical Climate 
http://sos.noaa.gov/Datasets/dataset.p 
hp?id=418#
Humid Tropical Climate 
• Three characteristics 
• 1. SE coasts of continents 
• 2. temp 50 to 95 
• 3. 48 inches of rainfall annually
Within the Köppen Climate Classification System, tropical moist climates extend 
northward and southward from the equator to about 15 to 25° of latitude. In these 
climates, all months have average temperatures greater than 18° Celsius (64° 
Fahrenheit). Annual precipitation is often greater than 1500 mm (59 in.). 
Citation 
Pidwirny, M. (2011). Tropical Moist Climates - A Climate Type. Retrieved from 
http://www.eoearth.org/view/article/162264
Dry Climate
Dry Climate 
• Three characteristics 
• 1. Temp freezing to hot 
• 2. covers 12% of Earth 
• 3. less than 20 inches annual rainfall
These Köppen climate types extend from 20 to 35° North and 
South of the equator and in large continental regions of the 
mid-latitudes often surrounded by mountains. 
http://sos.noaa.gov/Datasets/dataset.php?id=418#
Humid Mid Latitude
Humid Mid Latitude 
• Three characteristics 
• 1. Heavy rain during mild winters 
• 2. 30 to 50 degrees latitude 
• 3. hot muggy summers
Locations: Southeastern United States, northern 
Argentina, Uruguay, southern Brazil, southern 
Japan, and southern China. 
http://sos.noaa.gov/Datasets/d 
ataset.php?id=418#
Polar
Polar 
• Three characteristics 
• 1. temps not over 50 
• 2. northern land masses 
• 3. lichens and scrubby vegetation
Polar climates are found on the northern coastal 
areas of North America, Europe, Asia, and on the 
landmasses of Greenland and Antarctica.
Highlands
Highland 
• Three characteristics 
• 1. temps not above 50 
• 2. high mountain locations 
• 3. locations has snow-capped peaks most of the year
Highland (H) climates are defined by the effect 
altitude has on a location’s climate. As such, these 
climates are located from the tropics to the poles. 
• Rocky Mountains, USA Peru Nepal 
• The most obvious climate characteristic that is altered in these climates is 
temperature. Annual and monthly temperatures are lower because of 
adiabatic cooling, and due to the fact that the atmosphere at high altitudes 
contains less moisture. 
• Citation 
• Pidwirny, M. (2011). Highland Climates - H Climate Type. Retrieved from http://www.eoearth.org/view/article/162312
References 
• Aguado, E. and James E. Burt. 2010. Understanding Weather and Climate. Fifth Edition. 
Prentice Hall, Upper Saddle River, New Jersey. 
• Ahrens, C. D. 2006. Meteorology Today. An Introduction to Weather, Climate, and the 
Environment. Eighth Edition. Thompson, Brooks/Cole. USA. 
• Lutgens, F.K. and E.J. Tarbuck. 2004. The Atmosphere: An Introduction to Meteorology. 
Ninth Edition. Prentice Hall, Upper Saddle River, New Jersey. 
• Lydolph, P.E. 1985. The Climate of the Earth. Rowman and Allanheld Publishers, Totowa, 
New Jersey. 
• NOAA. Climate, JetStream - Online School for Weather, National Weather Service. 
• NOAA. Climate Classification. 
• Oliver, J.E. and J.J. Hidore. 2002. Climatology: An Atmospheric Science. Second Edition. 
Prentice Hall, Upper Saddle River, New Jersey. 
• Peel, Murray C. 2011. Updated Köppen-Geiger Climate Map of the World. 
http://people.eng.unimelb.edu.au/mpeel/koppen.html

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Koppen classification system

  • 2. Name the 5 categories in the Koppen Classification System.
  • 3. Citation Pidwirny, M. (2011). Köppen Climate Classification System. Retrieved from http://www.eoearth.org/vi ew/article/162263 • 1. Humid, Tropical Climate 2. Dry Climate 3. Humid Mid Latitude Climate 4. Polar climate 5. Highlands Climate
  • 4. Humid Tropical Climate http://sos.noaa.gov/Datasets/dataset.p hp?id=418#
  • 5. Humid Tropical Climate • Three characteristics • 1. SE coasts of continents • 2. temp 50 to 95 • 3. 48 inches of rainfall annually
  • 6. Within the Köppen Climate Classification System, tropical moist climates extend northward and southward from the equator to about 15 to 25° of latitude. In these climates, all months have average temperatures greater than 18° Celsius (64° Fahrenheit). Annual precipitation is often greater than 1500 mm (59 in.). Citation Pidwirny, M. (2011). Tropical Moist Climates - A Climate Type. Retrieved from http://www.eoearth.org/view/article/162264
  • 8. Dry Climate • Three characteristics • 1. Temp freezing to hot • 2. covers 12% of Earth • 3. less than 20 inches annual rainfall
  • 9. These Köppen climate types extend from 20 to 35° North and South of the equator and in large continental regions of the mid-latitudes often surrounded by mountains. http://sos.noaa.gov/Datasets/dataset.php?id=418#
  • 11. Humid Mid Latitude • Three characteristics • 1. Heavy rain during mild winters • 2. 30 to 50 degrees latitude • 3. hot muggy summers
  • 12. Locations: Southeastern United States, northern Argentina, Uruguay, southern Brazil, southern Japan, and southern China. http://sos.noaa.gov/Datasets/d ataset.php?id=418#
  • 13. Polar
  • 14. Polar • Three characteristics • 1. temps not over 50 • 2. northern land masses • 3. lichens and scrubby vegetation
  • 15. Polar climates are found on the northern coastal areas of North America, Europe, Asia, and on the landmasses of Greenland and Antarctica.
  • 17. Highland • Three characteristics • 1. temps not above 50 • 2. high mountain locations • 3. locations has snow-capped peaks most of the year
  • 18. Highland (H) climates are defined by the effect altitude has on a location’s climate. As such, these climates are located from the tropics to the poles. • Rocky Mountains, USA Peru Nepal • The most obvious climate characteristic that is altered in these climates is temperature. Annual and monthly temperatures are lower because of adiabatic cooling, and due to the fact that the atmosphere at high altitudes contains less moisture. • Citation • Pidwirny, M. (2011). Highland Climates - H Climate Type. Retrieved from http://www.eoearth.org/view/article/162312
  • 19. References • Aguado, E. and James E. Burt. 2010. Understanding Weather and Climate. Fifth Edition. Prentice Hall, Upper Saddle River, New Jersey. • Ahrens, C. D. 2006. Meteorology Today. An Introduction to Weather, Climate, and the Environment. Eighth Edition. Thompson, Brooks/Cole. USA. • Lutgens, F.K. and E.J. Tarbuck. 2004. The Atmosphere: An Introduction to Meteorology. Ninth Edition. Prentice Hall, Upper Saddle River, New Jersey. • Lydolph, P.E. 1985. The Climate of the Earth. Rowman and Allanheld Publishers, Totowa, New Jersey. • NOAA. Climate, JetStream - Online School for Weather, National Weather Service. • NOAA. Climate Classification. • Oliver, J.E. and J.J. Hidore. 2002. Climatology: An Atmospheric Science. Second Edition. Prentice Hall, Upper Saddle River, New Jersey. • Peel, Murray C. 2011. Updated Köppen-Geiger Climate Map of the World. http://people.eng.unimelb.edu.au/mpeel/koppen.html

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