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10/1/09 1 DARGAN M. W. FRIERSON UNIVERSITY OF WASHINGTON, DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 1: 10-1-09 Climate Dynamics (PCC 587): An Introduction to the Course Susan Solomon Talk Today! Discovered ozone hole link with CFCs Chair of IPCC Working Group 1 3:30 PM, Johnson 102 “A Tale for Our Times: Climate Change and Irreversibility”

Climate Dynamics (PCC 587): An Introduction to the Coursecourses.washington.edu › pcc587 › notes › 587_1.pdf · 2009-10-01 · 10/1/09 1 DARGAN M. W. FRIERSON UNIVERSITY OF

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Page 1: Climate Dynamics (PCC 587): An Introduction to the Coursecourses.washington.edu › pcc587 › notes › 587_1.pdf · 2009-10-01 · 10/1/09 1 DARGAN M. W. FRIERSON UNIVERSITY OF

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D A R G A N M . W . F R I E R S O N

U N I V E R S I T Y O F W A S H I N G T O N , D E P A R T M E N T O F A T M O S P H E R I C S C I E N C E S

D A Y 1 : 1 0 - 1 - 0 9

Climate Dynamics (PCC 587): An Introduction to the Course

Susan Solomon Talk Today!

 Discovered ozone hole link with CFCs

  Chair of IPCC Working Group 1

  3:30 PM, Johnson 102

  “A Tale for Our Times: Climate Change and Irreversibility”

Page 2: Climate Dynamics (PCC 587): An Introduction to the Coursecourses.washington.edu › pcc587 › notes › 587_1.pdf · 2009-10-01 · 10/1/09 1 DARGAN M. W. FRIERSON UNIVERSITY OF

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Climate Dynamics

 Questions like:   What determines the current climate mean state?

  Mean precipitation distribution:

TRMM Climatology (1998-2008)

Questions like…

 Why are the rainforests and deserts of the world at similar latitudes?

Page 3: Climate Dynamics (PCC 587): An Introduction to the Coursecourses.washington.edu › pcc587 › notes › 587_1.pdf · 2009-10-01 · 10/1/09 1 DARGAN M. W. FRIERSON UNIVERSITY OF

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Current Climate

Natural Climate Variability: El Niño

Page 4: Climate Dynamics (PCC 587): An Introduction to the Coursecourses.washington.edu › pcc587 › notes › 587_1.pdf · 2009-10-01 · 10/1/09 1 DARGAN M. W. FRIERSON UNIVERSITY OF

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El Niño/Southern Oscillation

La Niña conditions

Winds keep warm water to the west during La Niña

El Niño/Southern Oscillation

El Niño conditions

Page 5: Climate Dynamics (PCC 587): An Introduction to the Coursecourses.washington.edu › pcc587 › notes › 587_1.pdf · 2009-10-01 · 10/1/09 1 DARGAN M. W. FRIERSON UNIVERSITY OF

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El Niño/Southern Oscillation

El Niño/Southern Oscillation

  Impacts are global:

Page 6: Climate Dynamics (PCC 587): An Introduction to the Coursecourses.washington.edu › pcc587 › notes › 587_1.pdf · 2009-10-01 · 10/1/09 1 DARGAN M. W. FRIERSON UNIVERSITY OF

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North Atlantic Oscillation

  Shifts of storm tracks in the Atlantic

+ -

Arctic Oscillation: a similar phenomenon all the way around the N. Hemisphere

Pacific Decadal Oscillation

Warm PDO: left Cold PDO: right

Page 7: Climate Dynamics (PCC 587): An Introduction to the Coursecourses.washington.edu › pcc587 › notes › 587_1.pdf · 2009-10-01 · 10/1/09 1 DARGAN M. W. FRIERSON UNIVERSITY OF

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  PDO impacts on salmon catches ->

  PDO tells you whether they’re biting in Alaska or Washington

From Mantua et al (1997)

PDO Impacts .

Climate Change

 We’re modifying the atmospheric composition and climate at a rapid rate

 How much warming?   Depends on feedbacks:

 Water vapor

  Ice-albedo (melting ice

reflects less solar radiation)

 Clouds

 We’ll discuss a framework for feedback analysis, and these individual processes

Page 8: Climate Dynamics (PCC 587): An Introduction to the Coursecourses.washington.edu › pcc587 › notes › 587_1.pdf · 2009-10-01 · 10/1/09 1 DARGAN M. W. FRIERSON UNIVERSITY OF

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Climate Change

 What to expect?   Rainy gets rainier, dry gets drier

From Lu et al 2006

Paleoclimate

  Ice Age cycles   Last Glacial Maximum (21,000 years ago)

  Extreme climates of long ago?   “Snowball Earth”