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dc.contributor.authorDemaria, Eleonora M. C.
dc.contributor.authorRoundy, Joshua K.
dc.contributor.authorWi, Sungwook
dc.contributor.authorPalmer, Richard N.
dc.date.accessioned2017-12-07T22:16:38Z
dc.date.available2017-12-07T22:16:38Z
dc.date.issued2016-08-26
dc.identifier.citationDemaria, E. M., Roundy, J. K., Wi, S., & Palmer, R. N. (2016). The Effects of climate change on seasonal snowpack and the hydrology of the Northeastern and Upper Midwest United States. Journal of Climate, 29(18), 6527-6541.en_US
dc.identifier.urihttp://hdl.handle.net/1808/25613
dc.descriptionPermission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. All AMS journals and monograph publications are registered with the Copyright Clearance Center (http://www.copyright.com). Questions about permission to use materials for which AMS holds the copyright can also be directed to the AMS Permissions Officer at permissions@ametsoc.org. Additional details are provided in the AMS Copyright Policy statement, available on the AMS website (http://www.ametsoc.org/CopyrightInformation).en_US
dc.description.abstractThe potential effects of climate change on the snowpack of the northeastern and upper Midwest United States are assessed using statistically downscaled climate projections from an ensemble of 10 climate models and a macroscale hydrological model. Climate simulations for the region indicate warmer-than-normal temperatures and wetter conditions for the snow season (November–April) during the twenty-first century. However, despite projected increases in seasonal precipitation, statistically significant negative trends in snow water equivalent (SWE) are found for the region. Snow cover is likely to migrate northward in the future as a result of warmer-than-present air temperatures, with higher loss rates in northern latitudes and at high elevation. Decreases in future (2041–95) snow cover in early spring will likely affect the timing of maximum spring peak streamflow, with earlier peaks predicted in more than 80% of the 124 basins studied.en_US
dc.publisherAmerican Meteorological Societyen_US
dc.rights© Copyright 26/08/2016 American Meteorological Society (AMS).en_US
dc.subjectPhysical Meteorology and Climatologyen_US
dc.subjectClimate changeen_US
dc.subjectHydrologic cycleen_US
dc.subjectHydrologyen_US
dc.subjectSnow coveren_US
dc.subjectModels and modelingen_US
dc.subjectHydrologic modelsen_US
dc.titleThe Effects of Climate Change on Seasonal Snowpack and the Hydrology of the Northeastern and Upper Midwest United Statesen_US
dc.typeArticleen_US
kusw.kuauthorRoundy, Joshua K.
kusw.kudepartmentCivil, Environmental & Architectural Engineeringen_US
dc.identifier.doi10.1175/JCLI-D-15-0632.1en_US
kusw.oaversionScholarly/refereed, publisher versionen_US
kusw.oapolicyThis item meets KU Open Access policy criteria.en_US
dc.rights.accessrightsopenAccessen_US


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