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Dynamic Climate An overview of Climate Oscillations

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Dynamic Climate. An overview of Climate Oscillations. WHAT is a Climate Oscillation?. Climates are long-term weather patterns. Climates are a product of Latitude, Altitude, Proximity to Water, Location and distribution of nearby Highlands, and Nearby Ocean Currents. - PowerPoint PPT Presentation

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Page 1: Dynamic Climate

Dynamic Climate

An overview of Climate Oscillations

Page 2: Dynamic Climate

WHAT is a Climate Oscillation?

• Climates are long-term weather patterns.• Climates are a product of

– Latitude, – Altitude, – Proximity to Water, – Location and distribution of nearby Highlands, and – Nearby Ocean Currents.

• Which of these are static? • Which of these are dynamic?

Page 3: Dynamic Climate

Thermohaline Circulation: The Global Conveyor Belt

Page 4: Dynamic Climate

How thermohaline circulation runs

Page 5: Dynamic Climate

How Thermohaline Circulation works

Page 6: Dynamic Climate

How the Thermohaline affects the atmosphere.

Page 7: Dynamic Climate

Thermohaline Circulation, as viewed from the North Pole

Page 8: Dynamic Climate

What happens in the Antarctic

Page 10: Dynamic Climate

What can happen? (cont.)

The global conveyor belt thermohaline circulation is driven primarily by the formation and sinking of deep water.

When the strength of the haline forcing increases due to excess precipitation, runoff, or ice melt the conveyor belt will weaken or even shut down.

The variability in the strength of the conveyor belt will lead to climate change in Europe and it could also influence other areas of the global ocean.

Page 11: Dynamic Climate

So how does it affect climate?

• http://www.pik-potsdam.de/~stefan/thc_fact_sheet.html

Page 12: Dynamic Climate

So what present Climate Oscillations have been noted?

• El Niño Southern Oscillation (ENSO)

• North Atlantic Oscillation (NAO)

• Arctic Oscillation (AO)

• Pacific Decadal Oscillation (PDO)

Page 13: Dynamic Climate

El Niño Southern Oscillation (ENSO)

During El Niño, sea-surface temperatures in the eastern equatorial Pacific are warmer than usual (top), while during La Niña the same region is cooler.

Page 14: Dynamic Climate

El Niño Southern Oscillation (ENSO)

• http://www.pmel.noaa.gov/tao/elnino/el-nino-story.html

Page 15: Dynamic Climate

What results…

Page 16: Dynamic Climate

What results…

Page 17: Dynamic Climate

North Atlantic Oscillation (NAO)

Page 18: Dynamic Climate

What results…

Page 19: Dynamic Climate

Arctic Oscillation (AO)

Page 20: Dynamic Climate

Pacific Decadal Oscillation (PDO)