Strontium isotope dynamics reveal streamflow contributions from shallow flow paths during snowmelt in a montane watershed, Provo River, Utah, USA-Reference-Cited by-同舟云学术

Strontium isotope dynamics reveal streamflow contributions from shallow flow paths during snowmelt in a montane watershed, Provo River, Utah, USA

Published:2022-01 Issue:1 Volume:36 Page:
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Hale Colin A.¹,Carling Gregory T.¹^ORCID,Nelson Stephen T.¹,Fernandez Diego P.²,Brooks Paul D.²,Rey Kevin A.¹^ORCID,Tingey David G.¹,Packer Brian N.¹,Aanderud Zachary T.³

Affiliation:

1. Department of Geological Sciences Brigham Young University Provo Utah USA

2. Department of Geology & Geophysics University of Utah Salt Lake City Utah USA

3. Department of Plant & Wildlife Sciences Brigham Young University Provo Utah USA

Funder

Division of Earth Sciences

Office of Experimental Program to Stimulate Competitive Research

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14458

Reference46 articles.

1. Resolving the Double Paradox of rapidly mobilized old water with highly variable responses in runoff chemistry

2. Increasing Ca2+ deposition in the western US: The role of mineral aerosols

3. Annual maxima in Zn concentrations during spring snowmelt in streams impacted by mine drainage

4. Quantifying contributions to storm runoff through end-member mixing analysis and hydrologic measurements at the Panola Mountain Research Watershed (Georgia, USA)

5. Dust-mediated loading of trace and major elements to Wasatch Mountain snowpack

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