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Old groundwater buffers the effects of a major drought in groundwater-dependent ecosystems of the eastern Sierra Nevada (CA)

Bibliographic Data

ID15550737
AuthorsZachary P Meyers (0000-0003-4946-7720, Purdue University West Lafayette, corresponding author), Marty D Frisbee (0000-0002-9928-7149, Purdue University West Lafayette), Laura K Rademacher (0000-0002-5277-9656, University of the Pacific), Noah Stewart‐Maddox (Purdue University West Lafayette), Noah S Stewart-Maddox
Year2021
Volume16
Issue4
Pages044044-044044
Publication date2021-04-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/abde5f
OpenAlexW3139996024
LanguageEN
Citations received1
References cited65

Global groundwater resources are stressed and the effects of climate change are projected to further disrupt recharge processes. Therefore, we must identify the buffers to climate change in hydrogeologic systems in order to understand which groundwater resources will be disproportionally affected by these changes. Here, we utilize a novel combination of remote sensing (e.g. Landsat) and groundwater residence time data ( 3 H, 36 Cl) to identify the factors controlling the hydrogeologic stability of aridland mountain-front springs in response to a major climate event, the 2011–2017 California drought. Desert springs within Owens Valley (CA) support unique ecosystems that are surrounded by lush, green vegetation sustained only by discharging groundwater and are not reliant on localized precipitation. Therefore, the health or ecological response of this vegetation is a direct reflection of the hydrogeologic stability of the mountain-block groundwater system since water is the limiting resource for riparian plant growth in arid regions. We compared spring water residence times to vegetation health metrics computed from Landsat imagery leading up to and during the drought interval. We observe that the vegetation surrounding springs discharging a high fraction of modern and bomb-pulse groundwater ( 100 years) showed little response thereby supporting the conceptual model where old groundwater, i.e. a distribution of deep and stable groundwater flowpaths, buffers short- to long-term climate perturbations and may provide hydrogeologic resistance to future effects from climate change

Aquifer · Arid · Climate change · Ecosystem · Geography · Groundwater · Groundwater recharge · Hydrogeology · Hydrology (agriculture · Precipitation · Vegetation (pathology · Environmental Science · Hydrology and Drought Analysis · Hydrology and Watershed Management Studies · Plant Water Relations and Carbon Dynamics · Ecology · Geology

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Unique citing works1
Citations per year1
Citation span2025 - 2025 (1)
Citation velocityrecent
Highly citedNo
Citation typesNeutral: 1

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