Winter runoff events pose an unquantified continental-scale risk of high wintertime nutrient export

Winters in snow-covered regions have warmed, likely shifting the timing and magnitude of nutrient export, leading to unquantified changes in water quality. Intermittent, seasonal, and permanent snow covers more than half of the global land surface. Warming has reduced the cold conditions that limit...

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Main Authors: Erin C Seybold, Ravindra Dwivedi, Keith N Musselman, Dustin W Kincaid, Andrew W Schroth, Aimee T Classen, Julia N Perdrial, E Carol Adair
Format: Article
Language:English
Published: IOP Publishing 2022-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/ac8be5
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author Erin C Seybold
Ravindra Dwivedi
Keith N Musselman
Dustin W Kincaid
Andrew W Schroth
Aimee T Classen
Julia N Perdrial
E Carol Adair
author_facet Erin C Seybold
Ravindra Dwivedi
Keith N Musselman
Dustin W Kincaid
Andrew W Schroth
Aimee T Classen
Julia N Perdrial
E Carol Adair
author_sort Erin C Seybold
collection DOAJ
description Winters in snow-covered regions have warmed, likely shifting the timing and magnitude of nutrient export, leading to unquantified changes in water quality. Intermittent, seasonal, and permanent snow covers more than half of the global land surface. Warming has reduced the cold conditions that limit winter runoff and nutrient transport, while cold season snowmelt, the amount of winter precipitation falling as rain, and rain-on-snow have increased. We used existing geospatial datasets (rain-on-snow frequency overlain on nitrogen and phosphorous inventories) to identify areas of the contiguous United States (US) where water quality could be threatened by this change. Next, to illustrate the potential export impacts of these events, we examined flow and turbidity data from a large regional rain-on-snow event in the United States’ largest river basin, the Mississippi River Basin. We show that rain-on-snow, a major flood-generating mechanism for large areas of the globe (Berghuijs et al 2019 Water Resour. Res. 55 4582–93; Berghuijs et al 2016 Geophys. Res. Lett. 43 4382–90), affects 53% of the contiguous US and puts 50% of US nitrogen and phosphorus pools (43% of the contiguous US) at risk of export to groundwater and surface water. Further, the 2019 rain-on-snow event in the Mississippi River Basin demonstrates that these events could have large, cascading impacts on winter nutrient transport. We suggest that the assumption of low wintertime discharge and nutrient transport in historically snow-covered regions no longer holds. Critically, however, we lack sufficient data to accurately measure and predict these episodic and potentially large wintertime nutrient export events at regional to continental scales.
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spelling doaj.art-a195fb1c19c644968b49de12c1d0dc312023-08-09T15:15:32ZengIOP PublishingEnvironmental Research Letters1748-93262022-01-01171010404410.1088/1748-9326/ac8be5Winter runoff events pose an unquantified continental-scale risk of high wintertime nutrient exportErin C Seybold0https://orcid.org/0000-0002-0365-2333Ravindra Dwivedi1https://orcid.org/0000-0001-9369-132XKeith N Musselman2https://orcid.org/0000-0001-8394-491XDustin W Kincaid3https://orcid.org/0000-0003-1640-685XAndrew W Schroth4https://orcid.org/0000-0001-5553-3208Aimee T Classen5https://orcid.org/0000-0002-6741-3470Julia N Perdrial6https://orcid.org/0000-0002-2581-9341E Carol Adair7https://orcid.org/0000-0002-8567-9045Kansas Geological Survey, University of Kansas , Lawrence, KS, United States of America; Vermont EPSCoR, University of Vermont , Burlington, VT, United States of AmericaVermont EPSCoR, University of Vermont , Burlington, VT, United States of America; USDA-ARS Southwest Watershed Research Center , Tucson, AZ, United States of AmericaInstitute of Arctic and Alpine Research, University of Colorado Boulder , Boulder, CO, United States of AmericaVermont EPSCoR, University of Vermont , Burlington, VT, United States of America; The Gund Institute for Environment, University of Vermont , Burlington, VT, United States of AmericaVermont EPSCoR, University of Vermont , Burlington, VT, United States of America; Department of Geology, University of Vermont , Burlington, VT, United States of AmericaThe Gund Institute for Environment, University of Vermont , Burlington, VT, United States of America; Department of Ecology & Evolutionary Biology, University of Michigan , Ann Arbor, MI, United States of America; Rubenstein School of Environment & Natural Resources, University of Vermont , Burlington, VT, United States of AmericaVermont EPSCoR, University of Vermont , Burlington, VT, United States of America; The Gund Institute for Environment, University of Vermont , Burlington, VT, United States of America; Department of Geology, University of Vermont , Burlington, VT, United States of AmericaVermont EPSCoR, University of Vermont , Burlington, VT, United States of America; The Gund Institute for Environment, University of Vermont , Burlington, VT, United States of America; Rubenstein School of Environment & Natural Resources, University of Vermont , Burlington, VT, United States of AmericaWinters in snow-covered regions have warmed, likely shifting the timing and magnitude of nutrient export, leading to unquantified changes in water quality. Intermittent, seasonal, and permanent snow covers more than half of the global land surface. Warming has reduced the cold conditions that limit winter runoff and nutrient transport, while cold season snowmelt, the amount of winter precipitation falling as rain, and rain-on-snow have increased. We used existing geospatial datasets (rain-on-snow frequency overlain on nitrogen and phosphorous inventories) to identify areas of the contiguous United States (US) where water quality could be threatened by this change. Next, to illustrate the potential export impacts of these events, we examined flow and turbidity data from a large regional rain-on-snow event in the United States’ largest river basin, the Mississippi River Basin. We show that rain-on-snow, a major flood-generating mechanism for large areas of the globe (Berghuijs et al 2019 Water Resour. Res. 55 4582–93; Berghuijs et al 2016 Geophys. Res. Lett. 43 4382–90), affects 53% of the contiguous US and puts 50% of US nitrogen and phosphorus pools (43% of the contiguous US) at risk of export to groundwater and surface water. Further, the 2019 rain-on-snow event in the Mississippi River Basin demonstrates that these events could have large, cascading impacts on winter nutrient transport. We suggest that the assumption of low wintertime discharge and nutrient transport in historically snow-covered regions no longer holds. Critically, however, we lack sufficient data to accurately measure and predict these episodic and potentially large wintertime nutrient export events at regional to continental scales.https://doi.org/10.1088/1748-9326/ac8be5rain on snowwater qualityclimate changewinternutrient transportwatershed
spellingShingle Erin C Seybold
Ravindra Dwivedi
Keith N Musselman
Dustin W Kincaid
Andrew W Schroth
Aimee T Classen
Julia N Perdrial
E Carol Adair
Winter runoff events pose an unquantified continental-scale risk of high wintertime nutrient export
Environmental Research Letters
rain on snow
water quality
climate change
winter
nutrient transport
watershed
title Winter runoff events pose an unquantified continental-scale risk of high wintertime nutrient export
title_full Winter runoff events pose an unquantified continental-scale risk of high wintertime nutrient export
title_fullStr Winter runoff events pose an unquantified continental-scale risk of high wintertime nutrient export
title_full_unstemmed Winter runoff events pose an unquantified continental-scale risk of high wintertime nutrient export
title_short Winter runoff events pose an unquantified continental-scale risk of high wintertime nutrient export
title_sort winter runoff events pose an unquantified continental scale risk of high wintertime nutrient export
topic rain on snow
water quality
climate change
winter
nutrient transport
watershed
url https://doi.org/10.1088/1748-9326/ac8be5
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