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The amount of fresh water flowing through the Arctic as snow or rainfall, in rivers and other cycles is increasing, in agreement with model projections under a warming climate, according to a new study by University of Massachusetts Amherst hydrologist Michael Rawlins and colleagues from 18 other institutions in the United States, Norway and Finland.

The multi-year, multi-investigator synthesis of available data caps a five-year effort known as the Freshwater Integration study (FWI), funded by the National Science Foundation, which sought to answer fundamental questions about the Arctic system, foremost of which: Is the Arctic freshwater cycle accelerating or intensifying? Findings appear in the current, online issue of the Journal of Climate.

As Rawlins, manager of the Climate System Research Center at UMass Amherst explains, “The balance of evidence suggests that Arctic freshwater cycle intensification is occurring across the terrestrial Arctic. These observations are consistent with what models have suggested should occur with climatic warming.” Intensification is related to the atmosphere’s ability to hold more moisture as it warms.

Graphic of Arctic hydrologic system (photo credit Arctic-CHAMP / ARCUS) ..MORE...


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