Travel just few miles west of bustling Cheyenne, Wyoming, a you’ll find yourself in big-sky country. Tall-grass plains line the highway, snow-packed peaks pierce the sky, and round-edged granite formations jut out of the ground. But in this bucolic scene sits an alien building: a blocky, almost pre-fab structure with a white rotunda, speckled with dozens of windows that look out onto the grounds. Inside, it’s home to two supercomputers that focus on the vast landscape above.

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The climate of the Earth follows a complex interplay of cause-and-effect chains. A change in precipitation at one location may be caused by changes on the other side of the planet. A better understanding of these “teleconnections” – the linkages between remote places – may help to better understand local impacts of future climate change. A look into the climate of the past helps to investigate the teleconnections. An international team of Japanese, British, Australian, and German scientists, with the participation of the GFZ German Research Centre for Geosciences, now investigated Japanese lake sediments to decipher the interplay between local climate changes on the northern hemisphere about 12.000 years ago. Their results, now published as Nature Scientific Report, show that a regional warming in Europe caused a cooling and an increase in snowfall in East Asia.

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When spring arrives in the Arctic, both snow and sea ice melt, forming melt ponds on the surface of the sea ice. Every year, as global warming increases, there are more and larger melt ponds.

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