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Global Climate Chapter 17 Chapter 17 April 23, 2009

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Page 1: Global Climate - Web.nmsu.edu

Global Climate

Chapter 17Chapter 17April 23, 2009

Page 2: Global Climate - Web.nmsu.edu

Climatic Controls• Climate controls

Climatic Controls

– Latitude– Land and waterLand and water– Ocean currents

P ili i d– Prevailing winds– Pressure cells– Mountain

barriers– Altitude

This shows average annual sea-level temperatures in oF

Page 3: Global Climate - Web.nmsu.edu

Regions of Rising & Sinking AirRegions of Rising & Sinking Air

Global patterns of temperature and precipitation areprecipitation are affected by global cells ofglobal cells of rising and sinking air, which run meridionally north to southnorth to south

Page 4: Global Climate - Web.nmsu.edu

Observed Precipitationp

N th t th tt f i i d i ki i h l t di tNorth-to-south patterns of rising and sinking air help to predict precipitation, but zonal variation in land masses and ocean currents create deviations from these predictions.

Page 5: Global Climate - Web.nmsu.edu
Page 6: Global Climate - Web.nmsu.edu

Topographic Controls on ClimateTopographic Controls on Climate

Westerly winds blowing moist air from the Pacific Ocean encounter several mountain ranges that create patterns of rising air and precipitation followed by sinking air and warm dry rain shadows.

Page 7: Global Climate - Web.nmsu.edu

Climate ClassificationsClimate ClassificationsTh A i t G k• The Ancient Greeks– Tropical, temperate, and polar zone– Not enough zones to describe climate

• The Köppen System– Waldimir Köppen– Related vegetation and climate in order to predict g p

climate types in areas without climate data• The Thornthwaite Systemy

– P/E ratio, P/E Index– Potential Evapotranspirationp p

Page 8: Global Climate - Web.nmsu.edu

Köppen Climate Classification GroupsKöppen Climate Classification Groups

• A = Topical Moist: no winterB D P t ti l t i ti• B = Dry; Potential evapotranspiration > precipitation

• C = Moist Mid-Latitude with mild winterD M i t Mid L tit d ith i t• D = Moist Mid Latitude with severe winter

• E = Polar: cold, T<10°C,• H = Highland

Page 9: Global Climate - Web.nmsu.edu

More ClassificationsMore ClassificationsAf Tropical rain forest Dfa humid continental long hot Af Tropical rain forestAm Tropical monsoonAw Tropical wet and dry

Dfa humid continental long hot summer

Dfb humid continental long cool Aw Tropical wet and dryBW Arid desertBS Semi-arid

gsummer

Dfc subpolar cool short summerBS Semi aridCfa Humid subtropicalCfb Cfc Marine

Dw Dry winterET polar tundraCfb Cfc Marine

Cs Mediterranean dry summer

EF Polar ice capH Highlandsummer

Cw Dry winter

g

Page 10: Global Climate - Web.nmsu.edu
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AfAfIquitos Peru

Tropical wet

Iquitos, Peru

wet climate

Page 12: Global Climate - Web.nmsu.edu

AwAwTimbo, Guinea

Tropical wet and dry climate

Page 13: Global Climate - Web.nmsu.edu

BWhBWh

Arid desertArid desert climate

Phoenix, AZ

Page 14: Global Climate - Web.nmsu.edu

BWh

Arid desertArid desert climate

6

8

ion (in

)

4

thly Precupitat

2

Anv

erage Mon

t

Average annual precipitation 10.6 cm (4.19 inches)

0

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec

A

Page 15: Global Climate - Web.nmsu.edu

BSkBSk

Dry, semi-id l

Denver, COarid, cool climate

Page 16: Global Climate - Web.nmsu.edu

CfaCfa

Humid sub- Mobile, ALtropical climate

Page 17: Global Climate - Web.nmsu.edu

CfbCfb

Humid marine Port Hardy, climate Canada

Page 18: Global Climate - Web.nmsu.edu

Csb Csa

Coastal Mediterranean Interior Mediterranean

Page 19: Global Climate - Web.nmsu.edu

DfcDfc

Moist C ti t Fairbanks AKContinental Sub polar

Fairbanks, AK

polar

Page 20: Global Climate - Web.nmsu.edu

ETET

Polar tundraPolar tundra

Barrow, AKBarrow, AK

Page 21: Global Climate - Web.nmsu.edu

Elevation Controls on ClimateElevation Controls on Climate

Ascending a mountain brings changes in temperature and precipitation, and so to will bring changes in vegetation types and micro-climates, as illustrated i thi k t h th t f l d t t d d i h tin this sketch that moves from grassland to tundra and icecap across a short distance of 180 km, and up a steep elevation of 4 km.

Page 22: Global Climate - Web.nmsu.edu

Extremes from last 30 yearsExtremes from last 30 years

http://www.ncdc.noaa.gov/oa/climate/research/2007/dec/extreme-cities.html

Page 23: Global Climate - Web.nmsu.edu

Extremes from last 30 yearsExtremes from last 30 years

Page 24: Global Climate - Web.nmsu.edu

Climate Anomalies 2008Climate Anomalies 2008

From NCDChttp://www.ncdc.noaa.gov/img/climate/research/2008/ann/significant-extremes2008.gif

Page 25: Global Climate - Web.nmsu.edu

Daily Climate SummaryDaily Climate SummaryThis is the climate summary for WednesdayReport published Thursday

Climate database

p p y

Indicates normal temperatures and precipitation and records

Page 26: Global Climate - Web.nmsu.edu

Annual Precipitation 2008Annual Precipitation 2008

Total Precipitation map from:

Jan to Dec 2008 Precipitation % of Normal map:http://www.ncdc.noaa.gov/img/climate/research/2008/dec/precip.dfn.ytd-cont-200812.gif

Total Precipitation map from:http://www.cpc.noaa.gov/products/analysis_monitoring/regional_monitoring/us_12-month_precip.shtml

Page 27: Global Climate - Web.nmsu.edu

Drought TrackingDrought Tracking

Page 28: Global Climate - Web.nmsu.edu

Cloud ClimatologyCloud Climatology

• International Satellite Cloud Climatology Projectj

Page 29: Global Climate - Web.nmsu.edu

Average January Cloud Coverg y

Based on 2002-2006 MODIS Aqua daytime imagery