global distribution OF EXTREME ENVIRONMENTS

 

DESCRIBING DISTRIBUTION

Global Subregions (UN)

Global Subregions (UN)

Distribution refers to the way something is spread out or arranged over a geographic area. Describing distribution is an important skill for IB Geography. Referring to global subregions in your answer is a useful way to gain extra marks.

 

TASK 1: Study the maps below and write a description of the distribution using the key words below to help.

north/south/east/west                          named continents/regions                         coastal/inland                     highest/lowest                                         hemisphere                            tropics/mid latitude/polar    

In coastal areas. Highest in south west coast. Lowest north east coast and interior.

In coastal areas. Highest in south west coast. Lowest north east coast and interior.

Found in all regions of the world. Highest concentrations in northern hemisphere. Lowest in central Asia, northern North America.

Found in all regions of the world. Highest concentrations in northern hemisphere. Lowest in central Asia, northern North America.

Highest densities in south. Mainly extreme south and south west borders. Very low densities in north.

Highest densities in south. Mainly extreme south and south west borders. Very low densities in north.

 

GLOBAL DISTRIBUTION OF COLD & HIGH ALTITUDE ENVIRONMENTS

In the Köppen climate system, polar climates are defined as the warmest temperature of any month being below 10 °C (50 °F). Polar climates are further divided into two types, tundra climates and icecap climates (Source).

 

GLOBAL DISTRIBUTION OF HOT, ARID ENVIRONMENTS

Hot, arid climates are characterised by the amount of annual precipitation less than a threshold value that approximates the potential loss of moisture by evapotranspiration. (Source)

 

TASK 2: DISTRIBUTION AND CHARACTERISTICS OF EXTREME ENVIRONMENTS

  1. Research and present an overview of the distribution and characteristics of each of the following climate zones:

 
 

REASONS FOR COLD TEMPERATURES

Why polar regions are colder

 

REASONS FOR ARIDITY

Hadley cells and climate

Hadley cells and climate

Rain shadow effect

Rain shadow effect

 
 

REVIEW

Form pairs with person A unable to see the diagrams. Person B describes the picture for A to draw.

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