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Published byWinfred Stokes Modified over 9 years ago
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Climate Classifications October 28, 2014
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Weather vs. Climate Weather – state of the atmosphere at a specific place and time on Earth’s surface. Climate – average values of weather elements, such as temp and precipitation, over an extended period of time “Climate is what you expect, weather is what you get.” –Mark Twain
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Variables that Influence Climate Latitude – intensity of radiation, length of day Seasonality – annual variation of sun angle Air Circulation – predictable – weather systems Maritime/Continental – proximity to water can increase precip. and reduce temp range Topography – local topography can impact climate, e.g. windward vs. leeward side of mts.
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Köppen Climate Classification System Describes world climates based on: – Avg monthly temp – Avg monthly precip – Total annual precip 6 major climate groups based on latitude: A-E & H Further subdivided by temp and precip.
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Primary Letter – based on latitude – Exceptions: B and H climate types Secondary letter – based on seasonal changes in precipitation Tertiary letter – based on seasonal changes in temperature – Exceptions: A and E climate types have no tertiary letter Köppen Climate Classification System
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Köppen’s Climate Classifications Tropical Climates (A) – Average temp of every month > 18ºC Mesothermal Climates (C) – Coldest month average temperature -3ºC – At least 1 month average temperature > 10ºC Microthermal Climates (D) – Average temperature of warmest month >10ºC – Average temperature of coldest month < -3ºC Primary Letters
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Köppen’s Climate Classifications Polar Climates (E) – Average temperature of all months < 10ºC Dry Arid and Semiarid Climates (B) – Evaporation > precipitation Highland (H) Primary Letters
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Köppen’s Climate Classifications Secondary Letters These letters are based primarily on seasonal precipitation: –f = adequate rainfall all through the year, no distinct dry season –w = winter dry (keep in mind the hemisphere), if 70% or more of annual rainfall occurs in summer –s = summer dry, if 70% or more of annual rainfall occurs in winter –m = extremely wet summer = monsoon. A climate only.
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Köppen’s Climate Classifications Secondary Letters For B climate only: –S = semiarid = steppe –W = arid = desert –which results in either BS or BW. For E climate only: –T = tundra –F = perpetual frost = permanent ice –which results in either ET or EF.
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Köppen’s Climate Classifications Tertiary Letters The third letters in the system are based exclusively on seasonal and annual temperature: –a = hot summer, warmest month > 22°C; C and D only –b = warm summer, warmest month < 22°C; C and D only –c = cool summer, < 4 months over 10°C; C and D only –d = very cold winter, coldest month < -38°C; D only –h = dry-hot, annual temperature > 18°C; B only –k = dry-cold, annual temperature < 18°C; B only
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Köppen’s Climate Classifications Examples of Combinations Af = Tropical Rainforest climate type Am = Tropical Monsoon climate type BWh = Low-Latitude Hot Desert climate type Cfa = Humid Subtropical climate type Csa = Mediterranean climate type Dfb = Humid Continental climate type ET = Tundra climate type
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Tropical Climates (A) Straddle Equator from 25º N to 25º S Avg. Monthly temp. exceeds 18ºC (64ºF) Subdivided by precipitation: Af – tropical rainforest – wettest Am – tropical monsoon Aw – tropical savanna - drier
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AfAf
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Hawaii Tropical Rainforest - Af Northern Australia Tropical Savanna - Aw India Tropical Savanna - Am
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Arid/Semi-Arid Climates (B) Poleward of A climates on all continents Subsiding air from STHs - Moister on fringes Subdivided by temp & moisture: – BWh – 15-30º N & S – hot - little precip – BWk - <15 cm precip/yr – high temp range – BSh – more temp range & precip than BWh – BSk – rainshadow – convectional precip – high temp range
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Arid Climates (BWh)
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Semiarid Climates (BWk)
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BWh
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BWk
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Semiarid Climates (BS)
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BSh
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BSk
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Jordan – Hot, Low-latitude Desert - BWh Northcentral China – Cold, mid latitude Desert - BWk Eastern Colorado, USA Cold, mid latitude Steppe - BSk California, USA - Hot, low latitude Steppe - BSh
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Mesothermal Climates (C) 20º- 60º N & S – where most people live A warm and a cool season Cfa, Cwa – Humid Subtropical - hot, humid summer – east side of continents – 20-35º N & S Csa, Csb – Maritime - near 35º N & S – winter wet season, dry summer Cfb, Cfc – Mediterranean - west coast of continents – 35-60º N & S – mP air & orographic processes
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Humid Subtropical
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Cfa
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Maritime
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Mediterranean
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Csa
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Southern California – Mediterranean Dry-Summer Climate - Csa Western Washington – Marine West-Coast Climate - Cfc
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Microthermal Climates (D) Poleward of C climates, 35º- 60º N & S Long winters, limited summer warmth, continental climates Dfa, Dwa – large annual temp range – jet stream & cyclonic precip, most in summer Dfb, Dwb – very large annual temp range – mild summer, harsh, dry winter Dfc, Dwc, Dwd – long, bitter winters - short, cool summers – little precip – highest annual temp range on Earth
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Microthermal Climates (D)
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Dfa
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Dwa
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Eastern US – Humid Continental Hot-Summer Climate - Dfa Northern Michigan – Humid Continental Mild-Summer Climate - Dfb Central Canada - Subarctic Climate – Dfc
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Polar Climates (E) Latitudes >70º N & S Long, cold winters w/little precip. 2 Subcategories: – ET – temp moderated by ocean – precip mostly June-Oct.- polar high dominates – EF – interior Greenland and Antarctica – always brutally cold – polar desert
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Polar Climates (E)
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ET
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EF
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Highland Climates (H) Associated with large mtn ranges, e.g. Andes, Rockies, Alps, etc. Cooler/colder than surrounding lowlands, even in tropical or equatorial regions Often wetter than surroundings due to orographic precip.
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North American Climates
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