Dansgaard-Oeschger oscillations, Heinrich Events, Bond Events

Dansgaard-Oeschger oscillations
While most people's attention has been spent watching people with a vested interest in promoting anthropogenic climate change do so, there are a few people being true scientists. Instead of spreading opinions, they are continuing to do research for other explanations.

In the graphic at the top, we are seeing evidence of the Dansgaard-Oeschger oscillations commonly abbreviated as D-O. The D-O occur roughly every 1500 years. They have an upward temperature spike of 3-5 degrees (Greenland Ice Core samples) (but could be as high as 8 degrees) in a 40-year timeframe.

Heinrich Events are a cold phase that coincides with D-O Oscillations with a 6000-year periodicity and lasting for about 500 years.

List of Supposed Bond Events

Dansgaard-Oeschger oscillations are represented by a sudden rise in temperature every 1500 years followed by an almost as precipitous drop in temperatures described as Bond Events. Once the temperatures rise, the Polar Ice Sheet starts to calve icebergs that carry and deposit sediment on the ocean floor. This earmarks the Bond Events (arguable an aspect of D-O).

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