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World Geography 3202 Unit 2 Climate Patterns

World Geography 3202

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World Geography 3202. Unit 2 Climate Patterns. Introduction. In this unit, we will examine some of the basic forces that produce our weather and climate, how they produce climate patterns on the earth’s surface, and relate to human activity. - PowerPoint PPT Presentation

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Page 1: World Geography 3202

World Geography 3202

Unit 2Climate Patterns

Page 2: World Geography 3202

Introduction

In this unit, we will examine some of the basic forces that produce our weather and climate, how they produce climate patterns on the earth’s surface, and relate to human activity.

These patterns are strongly affected by the distribution of landforms and water forms.

Page 3: World Geography 3202

Weather and Climate: The earth, itself

The earth’s movement in space causes the occurrence of day and night.

It also causes the conditions related to the seasons.

When we refer to the rotation of the earth, we are referring to the 24 hour period it takes the earth to complete one full “spin” in orbit around the sun. – It is this 24 hour “spin” that causes the periods of day

and night, as the sun shines only on the half of the earth that is pointed toward the sun.

Page 4: World Geography 3202

Weather and Climate: The earth, itself

When we refer to the earth’s revolution, we are referring to the approximately 365 days that it takes the earth to revolve on it’s orbit around the sun.– This revolution is responsible for the seasons,

as the portions of the earth that are more directly or less directly exposed to the sun’s rays will correspondingly experience different seasons.

Page 5: World Geography 3202

Weather and Climate: The earth, itself

Equinox: Refers to the period in the year when day and night are equal (12 hours long). This occurs twice a year, in March and September. Solstice: Refers to the period in the year when daylight is longest (or daylight is shortest) depending on the hemisphere: This occurs twice a year, in June and December

Page 6: World Geography 3202

Solar Intensity

The diagram above attempts to illustrate how the sun’s rays are dispersed as they strike the earth. The more direct the rays are, the more intense, and hence, more heat they give off.

Where are temperatures generally going to be the warmest on the earth? Why?

Page 7: World Geography 3202

Solar Intensity

temperatures tend to decrease from low to high latitudes.

Where might there be an exception to this rule at the equator (ie: There Are places at the equator that are extremely cold).

Page 8: World Geography 3202

Solar inputs and outputs

How cloud cover influences the range of temperatures from day to night. How the greenhouse effect moderates climates.

Page 9: World Geography 3202

The cause of winds andhow winds affect climate

Wind is the result of air movement over the Earth. Air moves as a result of pressure systems from

areas of high pressure to areas of low pressure.

Page 10: World Geography 3202

Reasons for Pressure Variance 1) The Earth rotates. As it rotates, it drags the atmosphere around with it

causing the air to mix with the higher level atmosphere resulting in turbulence and pressure systems.

2) The sun heats. The heating of air around the Earth varies by latitude and time of day. – At the equator, for instance, large amounts of sun warm the air causing it to rise. – Conversely, the more acute angles of sunlight over the polar regions spread the

rays over a greater area resulting in less warming of the air. – The resulting effect is that the air over the poles is more dense than the air over

the equator.