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Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.

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Early Greek View of Earth’s Climate
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Page 1: Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.

Early GreekView of Earth’s Climate

Page 2: Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.

Köppen climate classification

--average monthly temp.

Page 3: Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.

Chart for DeterminingKöppen classification

Page 4: Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.

The Köppen system uses a series of letters to designate climate:

Page 5: Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.
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Koppen 2nd and 3rd letter designations

m – short dry season (monsoon)

s – dry summer (rare)

A climates

“Night is winter in the tropics”—

Page 12: Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.

CLIMATE CLASSIFICATION

“Genetic” Classification Köppen symbol

--warm, humid year-round--controls: ITCZ

mT air masses

--warm, humid year-round; short dry season--Controls: ITCZ, on-shore winds in rainy season

Page 13: Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.

--longer dry season than monsoon--Controls: ITCZ in rainy season (“summer”)STH in dry season (“winter”)

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Main control on A climates:

Page 21: Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.

B climates S– potential evapotranspiration exceeds precipitation W– potential evapotranspiration is 2x precipitation

Page 22: Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.

--hot, dry year round--Controls: STH

cT air masses

--not as dry as #4--Controls: same as #4

-- seasonal rainfall due to either ITCZ or Mid-latitude

cyclones

Page 23: Early Greek View of Earth’s Climate. Köppen climate classification --average monthly temp.

--Controls --cold ocean currents--e.g. Atacama Desert, Chile

--colder than #5 due to higher latitude

--Controls: long distance to moisture source; rainshadows

--similar to #7, but with more summer convective rainfall

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