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- W2016778864 abstract "The Arctic hydrological cycle throughout the Holocene is analyzed based on the results of transient simulations with the coupled atmosphere-ocean circulation model ECHO-G. The results suggest a ~ 2% increase of mid-Holocene to preindustrial Arctic river discharges for the Eurasian continent. However, rivers of the North America Arctic realm show a moderate runoff decline of approximately 4 to 5% for the same period. The total river discharge into the Arctic Ocean has remained at an approximately constant preindustrial level since the mid-Holocene. The positive discharge trend within Eurasia is caused by a more rapid decrease in local net evaporation compared to a smaller decline in advected moisture and hence precipitation. This effect is neither recognized within the North American Arctic domain nor in the far eastern part of the Eurasian Arctic realm. A detailed comparison of these model findings with a variety of proxy studies is conducted. The collected proxy records show trends of continental surface temperatures and precipitation rates that are consistent with the simulations. A continuation of the transient Holocene runs for the 19th and 20th century with increased greenhouse gasses indicates an increase of the total river influx into the Arctic Ocean of up to 7.6%. The Eurasian river discharges increase by 7.5%, the North American discharges by up to 8.4%. The most rapid increases have been detected since the beginning of the 20th century. These results are corroborated by the observed rising of Arctic river discharges during the last century which is attributed to anthropogenic warming. The acceleration of the Arctic hydrological cycle in the 20th century is without precedence in the Holocene." @default.
- W2016778864 created "2016-06-24" @default.
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- W2016778864 date "2011-10-01" @default.
- W2016778864 modified "2023-10-17" @default.
- W2016778864 title "Arctic river discharge trends since 7ka BP" @default.
- W2016778864 cites W1586067135 @default.
- W2016778864 cites W1600846377 @default.
- W2016778864 cites W1966244027 @default.
- W2016778864 cites W1969679649 @default.
- W2016778864 cites W1971142106 @default.
- W2016778864 cites W1973478069 @default.
- W2016778864 cites W1975697763 @default.
- W2016778864 cites W1980124673 @default.
- W2016778864 cites W1984909502 @default.
- W2016778864 cites W1989617382 @default.
- W2016778864 cites W1989757627 @default.
- W2016778864 cites W1991209386 @default.
- W2016778864 cites W1996875821 @default.
- W2016778864 cites W1998638908 @default.
- W2016778864 cites W2000444336 @default.
- W2016778864 cites W2001936277 @default.
- W2016778864 cites W2003270447 @default.
- W2016778864 cites W2019299358 @default.
- W2016778864 cites W2026795246 @default.
- W2016778864 cites W2027125083 @default.
- W2016778864 cites W2027929232 @default.
- W2016778864 cites W2028522241 @default.
- W2016778864 cites W2032326491 @default.
- W2016778864 cites W2032882676 @default.
- W2016778864 cites W2035587516 @default.
- W2016778864 cites W2036179143 @default.
- W2016778864 cites W2036409439 @default.
- W2016778864 cites W2038658935 @default.
- W2016778864 cites W2049775661 @default.
- W2016778864 cites W2050492015 @default.
- W2016778864 cites W2053327069 @default.
- W2016778864 cites W2053693705 @default.
- W2016778864 cites W2054878306 @default.
- W2016778864 cites W2058801094 @default.
- W2016778864 cites W2067145150 @default.
- W2016778864 cites W2071630498 @default.
- W2016778864 cites W2075793519 @default.
- W2016778864 cites W2078942759 @default.
- W2016778864 cites W2079891510 @default.
- W2016778864 cites W2080199880 @default.
- W2016778864 cites W2083641421 @default.
- W2016778864 cites W2085729535 @default.
- W2016778864 cites W2086481263 @default.
- W2016778864 cites W2089187669 @default.
- W2016778864 cites W2090761054 @default.
- W2016778864 cites W2091996742 @default.
- W2016778864 cites W2093043845 @default.
- W2016778864 cites W2094344136 @default.
- W2016778864 cites W2096830549 @default.
- W2016778864 cites W2098000364 @default.
- W2016778864 cites W2101000561 @default.
- W2016778864 cites W2103425624 @default.
- W2016778864 cites W2104040517 @default.
- W2016778864 cites W2108379304 @default.
- W2016778864 cites W2115371293 @default.
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- W2016778864 cites W2118955746 @default.
- W2016778864 cites W2121120729 @default.
- W2016778864 cites W2125600063 @default.
- W2016778864 cites W2126580316 @default.
- W2016778864 cites W2133609473 @default.
- W2016778864 cites W2136337495 @default.
- W2016778864 cites W2136736328 @default.
- W2016778864 cites W2137847923 @default.
- W2016778864 cites W2141389112 @default.
- W2016778864 cites W2145162552 @default.
- W2016778864 cites W2146079950 @default.
- W2016778864 cites W2152208495 @default.
- W2016778864 cites W2154306139 @default.
- W2016778864 cites W2155069722 @default.
- W2016778864 cites W2157962338 @default.
- W2016778864 cites W2166324565 @default.
- W2016778864 cites W2166469879 @default.
- W2016778864 cites W2168769901 @default.
- W2016778864 cites W2179158456 @default.
- W2016778864 cites W2180241847 @default.
- W2016778864 cites W2181284422 @default.
- W2016778864 cites W2301651007 @default.
- W2016778864 cites W90352741 @default.
- W2016778864 cites W99768300 @default.
- W2016778864 doi "https://doi.org/10.1016/j.gloplacha.2011.07.006" @default.
- W2016778864 hasPublicationYear "2011" @default.
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