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1 Global Climate Systems I. Earth’s Climate A. Present Climate and Classification 1. Climate components 2. Classification 3. Köppen Climate Classification III. Global Climate Change A. Global Warming I. Earth’s Climate Climate is weather over time Climatology is the study of climate Climatic regions are areas with weather statistics that are similar over time

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Page 1: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Global Climate SystemsI. Earth’s Climate

A. Present Climate and Classification1. Climate components

2. Classification

3. Köppen Climate Classification

III. Global Climate Change

A. Global Warming

I. Earth’s Climate

Climate is weather over time

Climatology is the study of climate

Climatic regions are areas with weather statistics that are similar over time

Page 2: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Earth’s Present Climate A. Climate Components

Page 3: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Types of Climate Classification:

Earth’s Present Climate 2. Classification of Climatic Regions

Types of Climate Classification:

Genetic classification: Classification based on causative factors (things like air masses and global circulation)

Empirical classification: Classification based on temperature and precipitation data.temperature and precipitation data.

Page 4: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Earth’s Present Climate3. Köppen Climate Classification System

Weather data used to create the Köppen Climate ppMaps:

Average monthly temperatures

Average monthly precipitation

Total annual precipitation

Köppen Generalized Climates

Page 5: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Tropical Climates (A) – equatorial regions, humid, warm

Tropical Climates (A) – equatorial regions, humid, warm

Page 6: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Dry Arid and Semiarid Climates (B) - deserts and steppes; arid and semiarid regions

Page 7: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Earth’s Present Climate 3. Köppen Climate Classification System

Mesothermal Climates (C) – humid subtropical, Mediterranean, and marine west coast regions

Earth’s Present Climate3. Köppen Climate Classification System

Mediterranean Climates (Cs)

Page 8: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Earth’s Present Climate 3. Köppen Climate Classification System

Microthermal Climates (D) – humid continental, subarctic regions

Earth’s Present Climate 3. Köppen Climate Classification System

Polar Climates (E) - polar regions

Page 9: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Earth’s Present Climate 3. Köppen Climate Classification System

Highland Climates (H) – Found in areas with moderate to high temps., but temperatures here are low due to elevation.

Global Climate Change

A.Global Warming

R f h i i l b lRefers to short-term increases in global temperatures caused by human actions.

Forced fluctuations in climate change are due to human activities.

Unforced fluctuations are natural changes in l b l liglobal climate.

IPCC states that global warming can be attributed to human activities (forced fluctuations).

Page 10: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Global Climate ChangeA. Global Warming

Global Climate ChangeA. Global Warming

Radiatively active gases that influence global iwarming:

Carbon dioxide (CO2)

Methane (CH4)

Nitrous oxide (N20)

Chloroflourocarbons (CFCs)( )

Water vapor

Page 11: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Global Climate ChangeA. Global Warming

Impact of Global Warming:Impact of Global Warming:

World food supply changes

Natural ecosystems changes

Melting glaciers

Increase in sea level

Page 12: Global Climate Systems - California State University, Northridgesd1229/101/Section2/Chpt7.pdfMicrosoft PowerPoint - Chpt7.pptx Author Shawna Created Date 10/13/2009 9:24:47 PM

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Global Climate ChangeA. Global Warming

A i I Di i i

Figure 10.32

Antarctic Ice Disintegration

Global Climate ChangeA. Global Warming

Political Actions:D l t f th K t P t l i 1997Development of the Kyoto Protocol in 1997.Forces more developed countries to reduce greenhouse gas emissions collectively by 5.3%United States goal of 7.0% will not be met because President Bush has abandoned the Kyoto Protocol under concerns for theKyoto Protocol under concerns for the economic cost of the emissions reduction.