Trajectory Shifts in the Arctic and Subarctic Freshwater Cycle

• Published in: Science (American Association for the Advancement of Science) 2006-08, Vol.313 (5790), p.1061-1066
• Main Authors: Peterson, Bruce J., McClelland, James, Curry, Ruth, Holmes, Robert M., Walsh, John E., Aagaard, Knut
• Format: Article
• Language: English
• Subjects: Atmospheric moisture; Brackish; Changes; Earth sciences; Earth, ocean, space; Exact sciences and technology; External geophysics; Fresh water; Freshwater; Freshwater resources; Glacial melting; Glaciers; Hydrology; Hydrology. Hydrogeology; Ice sheets; Marine; Meteorology; Oceans; Physics of the oceans; Review; River basins; Salinity; Sea ice; Seas; Thermohaline structure and circulation. Turbulence and diffusion; Water; Water in the atmosphere (humidity, clouds, evaporation, precipitation)
• ISSN: 0036-8075; 1095-9203
• DOI: 10.1126/science.1122593

Manifold changes in the freshwater cycle of high-latitude lands and oceans have been reported in the past few years. A synthesis of these changes in freshwater sources and in ocean freshwater storage illustrates the complementary and synoptic temporal pattern and magnitude of these changes over the past 50 years. Increasing river discharge anomalies and excess net precipitation on the ocean contributed ~20,000 cubic kilometers of fresh water to the Arctic and high-latitude North Atlantic oceans from lows in the 1960s to highs in the 1990s. Sea ice attrition provided another ~ 15,000 cubic kilometers, and glacial melt added ~2000 cubic kilometers. The sum of anomalous inputs from these freshwater sources matched the amount and rate at which fresh water accumulated in the North Atlantic during much of the period from 1965 through 1995. The changes in freshwater inputs and ocean storage occurred in conjunction with the amplifying North Atlantic Oscillation and rising air temperatures. Fresh water may now be accumulating in the Arctic Ocean and will likely be exported southward if and when the North Atlantic Oscillation enters into a new high phase.