Abstract
By most estimates, runoff from the land surface represents the single largest input of freshwater to the Arctic Ocean. Alekseev and Buzuev [1] estimated the total freshwater input to the Arctic Ocean to be between 4300 and 6475 km3/year based on ice formation data. Treshnikov [2] (reported in [3]) estimated the total freshwater flux from gauged land surface areas to be 3300 km3/yr, or 51 to 77 percent of the total from [1]. Grabs et al. [4] report that the accumulated sum of mean annual flow from the 35 largest gauged Arctic basins is approximately 202 mm/yr (2603 km3). When extrapolated to the entire land area draining to the Arctic (approximately 19,300,000 km2), this yields a total annual freshwater flux from the land surface of approximately 4000 km3, or between 62 and 93% of the total freshwater input as estimated from [1]. Another estimate of total freshwater flux from land areas into the Arctic Ocean is 4269 km3/year, with 17 and 24% attributed to ungauged discharge from islands and mainland, respectively [5].
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Bowling, L.C., Lettenmaier, D.P., Matheussen, B.V. (2000). Hydroclimatology of the Arctic Drainage Basin. In: Lewis, E.L., Jones, E.P., Lemke, P., Prowse, T.D., Wadhams, P. (eds) The Freshwater Budget of the Arctic Ocean. NATO Science Series, vol 70. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-4132-1_4
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