The summer rains that fall on the Western Himalaya—rains that feed glaciers, rivers, and hundreds of millions of people downstream—appear to be partly controlled by events unfolding more than 8,000 kilometers away, on the sea ice of the Greenland Sea and in the shifting pressure patterns of the Arctic. That is the central finding of […]
This story is only covered by news sources that have yet to be evaluated by the independent media monitoring agencies we use to assess the quality and reliability of news outlets on our platform. Learn more here.