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Tracking the subsurface signal of decadal climate warming to quantify vertical groundwater flow rates

dc.contributor.authorBense, Victor F.
dc.contributor.authorKurylyk, Barret L.
dc.date.accessioned2018-01-23T15:47:10Z
dc.date.available2018-01-23T15:47:10Z
dc.date.issued2017-12-28
dc.identifier.citationBense, V. F., & Kurylyk, B. L. (2017). Tracking the subsurface signal of decadal climate warming to quantify vertical groundwater flow rates. Geophysical Research Letters, 44, 12,244–12,253. https://doi.org/10.1002/2017GL076015en_US
dc.identifier.urihttp://hdl.handle.net/10222/73576
dc.language.isoenen_US
dc.publisherWiley (AGU publications)en_US
dc.relation.ispartofGeophysical Research Lettersen_US
dc.subjectgroundwater temperature, climate change, heat as a tracer, geotherms, geothermics, advectionen_US
dc.titleTracking the subsurface signal of decadal climate warming to quantify vertical groundwater flow ratesen_US
dc.typeTexten_US

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