Definitions
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Etymologies
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Examples
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These temperature increases occurred during glacial terminations and at the onset of D-O interstadials.
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These oscillations correlate with the D-O cycles, showing a close relationship between the deep-ocean circulation and the abrupt climatic changes during the last glaciation.
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A study of the ice-rafted material suggests that, coincident with the D-O cooling, ice within the Icelandic ice caps and within or near the Gulf of Saint Lawrence underwent nearly synchronous increases in rates of calving.
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Ice core records of the last 740,000 years leave little doubt regarding the role of CO2 and CH4 during the glacial-interglacial Milankovic cycles and Dansgaard-Oeschger (D-O) ~1470 years-long cycles (Ganopolski and Rahmstorf, 2001) during the last ice age.
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It is increasingly apparent that large, globally linked environmental feedbacks were involved in the generation of the large, rapid temperature increases that occurred during glacial termination and the onset of D-O events.
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The duration of these ice-rafting cycles varies between 2000 and 3000 years and they closely coincide with the D-O events.
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Oxygen isotope measurements from Greenland ice cores demonstrate that a series of rapid warm and cold oscillations, called Dansgaard – Oeschger (D-O) events, punctuated the last glaciation, often taking Greenland and northwestern Europe from a full-glacial climate to conditions about as warm as at present (Fig. 2.15).
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According to Lang et al. [42], associated temperature changes may have been as great as 16 ºC. The D-O oscillations are correlated with sea surface temperature variations derived from several North Atlantic deep-sea cores [43].
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Dr. Joshua Wurman, part of the D-O - W team -- Doppler on Wheels.
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No one knows why D-O events happen, but happen they do.
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