and sediment input to the deep Atlantic Ocean during the onset of glaciation on the Barents Sea margin. The new paleoenvironmental reconstruction spans from the Pliocene-Pleistocene transition to the mid-Pleistocene transition and contributes to the overall understanding of the evolution of the Arctic c...
Droughts can cover anywhere from a few square kilometers to large sections of continents, and they can last from a few weeks to decades [32]. Droughts often have a slow, creeping onset, with incremental long-term impacts. This slow start may delay initial responses, which leads to situations...