Vegetation water sources in California's Sierra Nevada ( USA ) are young and change over time, a multi‐isotope ( δ 18 O , δ 2 H , 3 H ) tracer approach.-Reference-Cited by-同舟云学术

Vegetation water sources in California's Sierra Nevada ( USA ) are young and change over time, a multi‐isotope ( δ 18 O , δ 2 H , 3 H ) tracer approach.

Published:2021-06 Issue:6 Volume:35 Page:
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Thaw Melissa¹²^ORCID,Visser Ate²^ORCID,Bibby Richard²,Deinhart Amanda²,Oerter Erik²,Conklin Martha¹

Affiliation:

1. School of Engineering University of California Merced California USA

2. Lawrence Livermore National Laboratory Livermore California USA

Funder

Lawrence Livermore National Laboratory

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14249

Reference57 articles.

1. Seasonal origins of soil water used by trees

2. Mechanisms controlling the impact of multi-year drought on mountain hydrology

3. Soil Moisture Response to Snowmelt and Rainfall in a Sierra Nevada Mixed‐Conifer Forest

4. Unexplained hydrogen isotope offsets complicate the identification and quantification of tree water sources in a riparian forest

5. Effects of climatic seasonality on the isotopic composition of evaporating soil waters

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