California
State University Long Beach
GEOL 300i; Earth Systems
and Global Change
Lecture 21b
Dr.
Rick Behl
Complexity of modern climatic change
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Global warming / global cooling
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When we look closely:
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Does anything change globally?
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Do all changes have a global effect?
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The truth is that any change may weave
a complex web
El Niño
/ Southern Oscillation (ENSO)
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Irregular multi-year (3-7?) cycle of oceanographic
& climatic change
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Typically last 14-22 months, but quite variable
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Centered in Pacific, but global effects
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Web of triggering events (El Niño)
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Westward shift of atmospheric high pressure
cells
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Weakened trade winds
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Slowed westward flow of equatorial surface
water
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Warm pool relaxes back to the east
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Storms and rain shift from Indonesia eastward
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Normal years referred to as "La Niña"
Climatic & ecologic repercussions
in the Pacific
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Decreased upwelling off Peru
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Catastrophic reduced fisheries
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Torrential rains along west coast of North
& South America (California)
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Floods, mudslides, crop damage
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Drought and fires in Australia, Indonesia,
Micronesia
Teleconnections (somewhat predictable)
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Equatorial air temperature and pressure disrupts
the jet stream
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Simultaneous warm pool shift in Indian Ocean
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Drought in India, Australia, central North
America, Caribbean, & Africa
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Recent El Niño episodes
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1977-1978, 1982-83, 1986-87, 1991-92,
1993-94 Mississippi floods), 1994-1996 (some consider 1990-1996 the longest
single El Niño
-
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1982-1983: the worst El Niño of
the century
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Encephalitis along the east coast (mosquitoes)
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Bubonic plague in New Mexico (fleas)
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Shark attacks off Oregon (warm water)
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Drought in Spain & N. Africa
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Changing frequency of El Niños
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During the Little Ice Age
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This century
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Past 20 years
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Why?
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For any questions or problems with these pages contact>
John Francis
Email: jfrancis@csulb.edu
Phone: 562-985-4928
written by R. Behl.
Last changes: 24 Oct. 1997