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1000 Titel
  • Elevational control of isotopic composition and application in understanding hydrologic processes in the mid Merced River catchment, Sierra Nevada, California, USA
1000 Autor/in
  1. Liu, Fengjing |
  2. Conklin, Martha |
  3. Shaw, Glenn D. |
1000 Verlag Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-05-28
1000 Erschienen in
1000 Quellenangabe
  • 28(10):2239-2258
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/hess-28-2239-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. Mountain snowpack has been declining and more precipitation has fallen as rainfall than snowfall, particularly in the western US. Isotopic composition in stream water, springs, groundwater, and precipitation was examined to understand the impact of declining snowpack on hydrologic processes in the mid Merced River catchment (1873 km2), Sierra Nevada, California. Mean isotopic values in small tributaries (catchment area &lt; 122 km2), rock glacier outflows, and groundwater from 2005 to 2008 were strongly correlated with mean catchment elevation (R2= 0.96 for δ2H, n= 16, p &lt; 0.001), with an average isotopic lapse rate of −1.9 ‰ per 100 m for δ2H and −0.22 ‰ per 100 m for δ18O in meteoric water. The lapse rate did not change much over the seasons and was not strongly affected by isotopic fractionation. A catchment-characteristic isotopic value, representing the catchment arithmetic mean isotopic signature in meteoric water, was thus established for each sub-catchment based on the lapse rate to elucidate hydrometeorologic and hydrologic processes such as the duration and the magnitude of snowmelt events and elevational water sources of streamflow and groundwater for ungauged catchments. Compared to Tenaya Creek without water falls, the flow and flow duration of Yosemite Creek appear to be much more sensitive to seasonal temperature increases during the baseflow period due to a strong evaporation effect caused by waterfalls, suggesting a possible prolonged dry-up period of Yosemite Falls in the future. Groundwater in Yosemite Valley (∼ 900–1200 m) was recharged primarily from the upper snow–rain transition zone (2000–2500 m), suggesting its strong vulnerability to shifts in the snow–rain ratio. The information gained from this study helps advance our understanding of hydrologic responses to climate change in snowmelt-fed river systems. </jats:p>
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1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/TGl1LCBGZW5namluZw==|https://orcid.org/0000-0002-9627-2427|https://frl.publisso.de/adhoc/uri/U2hhdywgR2xlbm4gRC4=
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1000 Förderer
  1. California Energy Commission |
  2. Michigan Technological University |
  3. Directorate for Geosciences |
  4. National Institute of Food and Agriculture |
1000 Fördernummer
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1000 Förderprogramm
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1000 Dateien
1000 Förderung
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    1000 Förderer California Energy Commission |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer Michigan Technological University |
    1000 Förderprogramm -
    1000 Fördernummer -
  3. 1000 joinedFunding-child
    1000 Förderer Directorate for Geosciences |
    1000 Förderprogramm -
    1000 Fördernummer -
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    1000 Förderer National Institute of Food and Agriculture |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 @id frl:6485874.rdf
1000 Erstellt am 2024-10-02T22:47:43.928+0200
1000 Erstellt von 322
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1000 Zuletzt bearbeitet 2025-08-13T16:34:48.543+0200
1000 Objekt bearb. Wed Aug 13 16:34:48 CEST 2025
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