
Sediment cores were obtained from Lake Kråkenes in western Norway and from the Nordic seas in order to document the last part of the ice age.
A group of scientists at the Bjerknes Centre for Climate Research and the University of Bergen in Norway, together with colleagues at ETH, Zürich, combined terrestrial and marine proxy palaeo-data covering the latest part of the ice age to improve our understanding of the mechanisms leading to rapid climatic changes.
The Younger Dryas event, which began approximately 12,900 years ago, was a period of rapid cooling in the Northern Hemisphere, driven by large-scale reorganizations of patterns of atmospheric and oceanic circulation. Environmental changes during this period have been documented by both proxy-based reconstructions from sediment archives and model simulations, but there is currently no consensus on the exact mechanisms of onset, stabilization, or termination of the Younger Dryas. In contrast to existing knowledge, the Nature article shows that the climate shifted repeatedly from cold and dry to wet and less cold, from decade to decade, before interglacial conditions were finally reached and the climate system became more stable.
Comment: According to the late Rhodes Fairbridge, the alignment of the Jupiter and Saturn, along with the minor planets, control the climate on Earth. And according Richard Mackey, writing in the Journal of Coastal Research (Special Issue 50, 2007): Not only has Ulysses found that the sun has reduced its output of solar wind to the lowest levels since accurate readings became available, but it's magnetic field has dropped by 20%. At the same time, the solar system appears to be passing through a galactic dust storm. Indeed.
And we also know that during the previous ice age the depositional flux of cosmic dust was much higher than during the Holocene.
Gabrielli's paper shows that it was not the sun alone that caused the last ice age:
It bears repeating astronomer Victor Clube's comment: