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Published byMeredith Parsons Modified over 6 years ago
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Abrupt climate change
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Abrupt climate change events during last glacial period (20-60kyr BP)
Dansgaard-Oeschger events (ice cores) Heinrich events (ocean sediments) Younger Dryas event
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Ice cores: a record of past climate history
Snow turns into ice under pressure Ice core drilling in EPICA, Antarctica: 800,000 yr of climate history
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Dansgaard-Oeschger events
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Global warming vs abrupt past climate change: D/O & Heinrich events
Amplitude 0.6C 10C Duration of change 100 years 20 years
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Heinrich events
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Collecting the data: Deep sea cores CSS Hudson; gravity piston core
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Cores stored in lab and retrieving a10m long gravity piston core
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Deep Sea Drilling Named for the Captain James Cook‘s HMS Resolution, 200 yrs ago. a derrick 61.5 m (202 ft) above water line; 143 m (469 ft) long; 21 m (68.9 ft) wide. Rig can suspend 9,150 m (30,020 ft) of drill pipe to ocean depth 8,235 m Resolution Drill Ship, originally an oil exploration ship operations days: 6,591 n. miles traveled 355,781 # of sites visited: 669 # of holes drilled: 1797 # recovered cores : 35,772
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Micrograph of sand-size fraction in core HU87033-009.
Henrich’s 1988 cores from Dreizack seamounts: chain of extinct underwater volcanoes; 1000m above the sea floor; eastern North Atlantic, west of portugal Micrograph of sand-size fraction in core HU sand-size fraction from the same core at cm depth, within H-2.
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Color and X-ray of lithic-rich sediments.
Heinrich (1988) discovered unexpectedly abrupt transitions between foraminifera & lithic sediments. Lithic sediments found at six depths. Changes are visible in color and X-rays: between dark-colored (foraminifera) & light-colored (lithic) segments.
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Heinrich events (fraction of lithic material as function of time)
How did these continental sand/ rocks get to the middle of the ocean??
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Spatial extent of Heinrich layers
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Source of lithic sediments: icebergs released from land ice
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Source of ice rafted debri: “Dirty ice”
East Greenland: We seldom think of icebergs as dirty, and with good reason: only some icebergs contain debris, and even then, only in a 1-2m layer like that which is plainly visible in this iceberg.
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Heinrich “teleconnections”
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Mechanism of Heinrich events: The Binge/ Purge Oscillator:
The mechanism of periodic ice discharges from Laurentide ice sheet (Doug MacAyeal 1993):
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Which is what? Dansgaard/ Oeschger (DO) events: abrupt warming events seen in Greenland ice cores every ~1,500 years. Warming occurs within 20 years, and lasts years. Heinrich events are massive releases of icebergs into North Atlantic ocean from Laurentide ice sheet and possibly others. Occurs every ~7,000-10,000 years Are they linked?
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Climate effects of Heinrich events; Possible link between Heinrich and D/O events:
Some of the larger D/O warming events seem to follow and perhaps result from Heinrich events:
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Connection between D/O and Heinrich events: the “bond cycle”
No satisfactory explanation currently exists for this cycle…
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Mechanism of D/O warming events in Greenland ice cores
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Two alternative explanations to observed abrupt warmings: 1: Thermohaline circulation
Density=-Temperature+Salinity; THC: driven by temperature gradients due to atmc heating & cooling. braked by salinity gradients due to evaporation & precipitation. Transport = 20Sv (world rivers combined = 1Sv =10^6m^3/sec) Large heat transport from equator to poles.
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Two alternative explanations to observed abrupt warmings: 2: sea ice
Sea ice albedo: Sea LGM: Sea ice pancakes:
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Younger Dryas Abrupt return to glacial conditions in the northern north Atlantic at around 12,900 – 11,500 yr BP; some related climate signals in many areas around globe Due to weakening of thermohaline circulation and expansion of sea ice?
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Finally, the good(?) news about D/O events
Some scientists suggested that global warming may result in an unstable climate, as during the last glacial maximum: However, this is not likely if D/O events were caused by sea ice changes around Greenland. Sea ice is expected to melt even in the arctic within years Is this good news…?
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Sea ice and global warming
Arctic sea ice animation from satellite data: winter: smallest sea ice recovery on record Arctic sea ice area shrinking by some 25% from 1979 to 2005
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