Publication Search
Pérez‐Ruiz, E. R., Vivoni, E. R., Sala, O. E.
Journal: Ecosphere, Volume 13 (7): (2022), ISBN . DOI: http://doi.org/10.1002/ecs2.4189 Sites: US-Jo2
Schreiner-McGraw, A. P., Vivoni, E. R., Ajami, H., Sala, O. E., Throop, H. L., Peters, D. P.
Journal: Scientific Reports, Volume 10 (1): (2020), ISBN . DOI: https://doi.org/10.1038/s41598-020-65094-x Sites: US-Jo2
Schreiner‐McGraw, A. P., Vivoni, E. R.
Channel transmission losses alter the streamflow response of arid and semiarid watersheds and promote focused groundwater recharge. This process has been primarily studied in dryland channels draining large areas that are displaced away from hillslope runoff generation. In contrast, small watersheds on arid piedmont slopes allow …
Journal: Water Resources Research, Volume 54 (7): 4498-4518 (2018), ISBN . DOI: https://doi.org/10.1029/2018WR022842 Sites: US-Jo2
Biederman, J. A., Scott, R. L., Arnone III, J. A., Jasoni, R. L., Litvak, M. E., Moreo, M. T., Papuga, S. A., Ponce-Campos, G. E., Schreiner-McGraw, A. P., Vivoni, E. R.
Journal: Agricultural And Forest Meteorology, Volume 249: 407-419 (2018), ISBN . DOI: https://doi.org/10.1016/j.agrformet.2017.11.005 Sites: US-Jo2
Schreiner-McGraw, A. P., Vivoni, E. R.
A critical hydrologic process in arid and semiarid regions is the interaction between ephemeral channels and groundwater aquifers. Generally, it has been found that ephemeral channels contribute to groundwater recharge when streamflow infiltrates into the sandy bottoms of channels. This process has traditionally been studied in channels …
Journal: Ecosphere, Volume 8 (11): e02000 (2017), ISBN . DOI: https://doi.org/10.1002/ecs2.2000 Sites: US-Jo2
Anderson, C. A., Vivoni, E. R.
Land surface states play important roles in the turbulent exchanges between ecosystems and their overlying atmosphere. Field methods to estimate turbulent fluxes have time‐variable source areas, while land surface observations are typically obtained at single plots with a smaller measurement scale. In this study, we characterize …
Journal: Water Resources Research, Volume 52 (6): 4785-4800 (2016), ISBN . DOI: https://doi.org/10.1002/2015WR018016 Sites: US-Jo2
Schreiner-McGraw, A. P., Vivoni, E. R., Mascaro, G., Franz, T. E.
Soil moisture dynamics reflect the complex interactions of meteorological conditions with soil, vegetation and terrain properties. In this study, intermediate-scale soil moisture estimates from the cosmic-ray neutron sensing (CRNS) method are evaluated for two semiarid ecosystems in the southwestern United States: a mesquite savanna …
Journal: Hydrology And Earth System Sciences, Volume 20 (1): 329-345 (2016), ISBN . DOI: https://doi.org/10.5194/hess-20-329-2016 Sites: US-Jo2
Mascaro, G., Vivoni, E. R.
The spatiotemporal variability of soil moisture (θ) has rarely been studied at the field scale across different seasons and sites. Here, we utilized 9 months of θ data in two semiarid ecosystems of North America to investigate the key relationship between the spatial mean (〈θ〉) and standard deviation (σ θ ) at the field-scale …
Journal: Environmental Research Letters, Volume 11 (8): 084008 (2016), ISBN . DOI: https://doi.org/10.1088/1748-9326/11/8/084008 Sites: US-Jo2, US-SRS
Templeton, R. C., Vivoni, E. R., Méndez-Barroso, L. A., Pierini, N. A., Anderson, C. A., Rango, A., Laliberte, A. S., Scott, R. L.
The North American monsoon (NAM) contributes roughly half of the annual precipitation in the Chihuahuan Desert from July to September. Relatively frequent, intense storms increase soil moisture and lead to ephemeral runoff. Quantifying these processes, however, is difficult due to the sparse nature of existing observations. This …
Journal: Journal Of Hydrology, Volume 509: 306-319 (2014), ISBN . DOI: https://doi.org/10.1016/j.jhydrol.2013.11.047 Sites: US-Jo2