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100			_aSmith, Stephen G _952099
245			_a 4000-year record of hydrologic variability from the Olympic Mountains, Washington, USA/
260			_bSage, _c2019.
300			_aVol 29, issue 8, 2019 : (1273-1291p.).
520			_a Sedimentological and geochemical analyses of gravity and piston cores retrieved from Lake Quinault, Washington, reveal an ~4000-year flood-dominated depositional record. Individual flood event layers are identified by combining core stratigraphy, sedimentology, and the ratio of incoherent to coherently scattered x-ray radiation (inc/coh) from µXRF (x-ray fluorescence) core scans. The inc/coh time series is used as a proxy for sediment grain size and, in combination with radiocarbon-anchored core age–depth models, enables the reconstruction of late-Holocene hydrologic variability for the Quinault River catchment. Decadal to centennial variability in inc/coh is interpreted to reflect trends in ocean-atmosphere teleconnections favorable for the formation of land-falling atmospheric rivers along the Pacific Ocean flank of the Olympic Mountains. Such processes likely modulate the rate of flooding and may explain notable increases in the frequency of flood event layers observed during the periods 2350–2450 cal. yr BP and the most recent century (AD 1910–2010). Understanding past hydrologic variability has important implications for the landscape and ecosystem response of Olympic Mountain catchments to future climate warming.
650			_aHolocene, _950806
650			_a lacustrine sediments, _952100
650			_aOlympic Peninsula, _952101
650			_apaleoflood reconstructions, _952102
650			_a μXRF core scanning _952103
700			_aWegmann, Karl W _952104
700			_aLeithold, Elana L _952105
700			_aBohnenstieh, Delwayne R l _952106
773	0		_012756 _916504 _dLondon: Sage Publication Ltd, 2019. _tHolocene/ _x09596836
856			_uhttps://doi.org/10.1177/0959683619846975
942			_2ddc _cART
999			_c12846 _d12846