Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science...

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Chapter 25.2 Chapter 25.2 Climate Zones Climate Zones Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith

Transcript of Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science...

Page 1: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.

Chapter 25.2Chapter 25.2““Climate ZonesClimate Zones””

Modified from many sources & Prentice Hall & Holt CA Earth Scienceby L. Smith

Page 2: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.

Remember:Remember:

CLIMATE = WEATHER

CLIMATE = The AVERAGE weather conditions over a LONG period of time

Page 3: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.

Remember:Remember:CLIMATE = most often described by:

AVERAGE TEMPERATUREand

ANNUAL PRECIPITATION

Page 4: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.

Latitude influences angle of sunlight and therefore the temperature of an area.

Page 5: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.
Page 6: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.

This also influences the global wind

patterns and therefore precipitation.

Page 7: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.
Page 8: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.

Climate Zones

http://www.webquest.hawaii.edu/kahihi/sciencedictionary/images/degreemap.jpg

Page 9: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.

http://home.comcast.net/~rhaberlin/images/emclim.gif

Page 10: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.

Tropical Zone

The tropical zone is between 23.5o north (the tropic of Cancer) and 23.5o south (the tropic of Capricorn) of the equator.

The sun’s rays are most intense and the temperatures are always warm.

http://www.touristmaker.com/images/tropical/wet-tropical-climate.jpg

http://blogs.nature.com/climatefeedback/files/rainforest2.jpg

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Temperate Zone

The temperate zones are between 23.5o and 66.5o north and between 23.5o and 66.5o south of the equator.

The sun’s rays strike Earth at a smaller angle than near the equator.

http://www.meteorologyclimate.com/temperate-ireland.jpg

http://www.touristmaker.com/images/temperate/autumn-temperate-climate-zone-new-zealand.jpg

Page 12: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.

Polar Zone

Polar zones are between 66.5o and 90o north and south latitudes and the poles.

The sun’s rays strike Earth at a very small angle in the polar zones.

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Köppen Climate Classification System

The most widely used for classifying the world's climates.

Köppen divided the Earth's surface into climatic regions that generally coincided with world patterns of vegetation and soils.

The Köppen system recognizes five major climate types based on the annual and monthly averages of temperature and precipitation. Each type is designated by a capital letter.

Page 14: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.
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Further subgroups are designated by a second, lower case letter which distinguish specific seasonal characteristics of temperature and precipitation.

To further denote variations in climate, a third letter was added to the code

These letters usually correspond to information about certain months or about max and min temperature or rainfall.

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Page 17: Chapter 25.2 “Climate Zones” Modified from many sources & Prentice Hall & Holt CA Earth Science by L. Smith.

Local ClimatesThe climate of a small area is called the microclimate.

Density of vegetation, elevation and proximity to large bodies of water greatly influence the local microclimate.

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ElevationHigher elevations tend to have lower temperatures.

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Precipitation amounts are also influenced by the rain shadow effect.

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Large Bodies of WaterWater absorbs and release heat slower than land does—moderating temperature variation.

Large bodies of water also typically lead to increased precipitation for a region.