Evaluating mountain meadow groundwater response to Pinyon-Juniper and temperature in a great basin watershed
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Authors
Carroll, Rosemary W. H.
Huntington, Justin L.
Snyder, Keirith A.
Niswonger, Richard G.
Morton, Charles
Stringham, Tamzen K.
Issue Date
2017
Type
Article
Language
en_US
Keywords
climate , Great Basin , groundwater dependent ecosystems , integrated hydrologic model , Landsat , PinyonâJuniper
Alternative Title
Abstract
This research highlights development and application of an integrated hydrologic model (GSFLOW) to a semiarid, snow-dominated watershed in the Great Basin to evaluate Pinyon-Juniper (PJ) and temperature controls on mountain meadow shallow groundwater. The work used Google Earth Engine Landsat satellite and gridded climate archives for model evaluation. Model simulations across three decades indicated that the watershed operates on a threshold response to precipitation (P) >400mm/y to produce a positive yield (P-ET
9%) resulting in stream discharge and a rebound in meadow groundwater levels during these wetter years. Observed and simulated meadow groundwater response to large P correlates with above average predicted soil moisture and with a normalized difference vegetation index threshold value >0.3. A return to assumed pre-expansion PJ conditions or an increase in temperature to mid-21st century shifts yielded by only +/- 1% during the multi-decade simulation period
but changes of approximately +/- 4% occurred during wet years. Changes in annual yield were largely dampened by the spatial and temporal redistribution of evapotranspiration across the watershed: Yet the influence of this redistribution and vegetation structural controls on snowmelt altered recharge to control water table depth in the meadow. Even a small-scale removal of PJ (0.5km(2)) proximal to the meadow will promote a stable, shallow groundwater system resilient to droughts, while modest increases in temperature will produce a meadow susceptible to declining water levels and a community structure likely to move toward dry and degraded conditions.
9%) resulting in stream discharge and a rebound in meadow groundwater levels during these wetter years. Observed and simulated meadow groundwater response to large P correlates with above average predicted soil moisture and with a normalized difference vegetation index threshold value >0.3. A return to assumed pre-expansion PJ conditions or an increase in temperature to mid-21st century shifts yielded by only +/- 1% during the multi-decade simulation period
but changes of approximately +/- 4% occurred during wet years. Changes in annual yield were largely dampened by the spatial and temporal redistribution of evapotranspiration across the watershed: Yet the influence of this redistribution and vegetation structural controls on snowmelt altered recharge to control water table depth in the meadow. Even a small-scale removal of PJ (0.5km(2)) proximal to the meadow will promote a stable, shallow groundwater system resilient to droughts, while modest increases in temperature will produce a meadow susceptible to declining water levels and a community structure likely to move toward dry and degraded conditions.
Description
Citation
Carroll, R. W. H., Huntington, J. L., Snyder, K. A., Niswonger, R. G., Morton, C., & Stringham, T. K. (2016). Evaluating mountain meadow groundwater response to PinyonâJuniper and temperature in a great basin watershed. Ecohydrology, 10(1), e1792. doi:10.1002/eco.1792
Publisher
Ecohydrology
License
Journal
Volume
Issue
PubMed ID
DOI
ISSN
1936-0584