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Decreasing river discharge in northern Canada -: art. no. L10401

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GEOPHYSICAL RESEARCH LETTERS
卷 32, 期 10, 页码 -

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AMER GEOPHYSICAL UNION
DOI: 10.1029/2005GL022845

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Freshwater discharge to high-latitude oceans in 64 Canadian rivers is investigated. The mean annual discharge rate attains 1252 km(3) yr(-1) for an area of 5.6 x 10(6) km(2), equating to a sink of 225 mm yr(-1) in the surface water budget of northern Canada (excluding the Arctic Archipelago where insufficient data exist). Application of the Mann-Kendall test to the data reveals a 10% decrease (-125 km(3) yr(-1) or -22 mm yr(-1)) in the total annual river discharge to the Arctic and North Atlantic Oceans from 1964 to 2003. This trend in river runoff is consistent with a 21 mm yr(-1) decline in observed precipitation over northern Canada between 1964 and 2000. We find evidence of statistically-significant links between the Arctic Oscillation, El Nino/ Southern Oscillation, and the Pacific Decadal Oscillation to the total annual freshwater discharge in northern Canada's rivers at interannual- to-decadal timescales.

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