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ARS Home » Plains Area » Las Cruces, New Mexico » Range Management Research » Research » Publications at this Location » Publication #366272
Research Project: Science and Technologies for the Sustainable Management of Western Rangeland Systems

Location: Range Management Research

Title: Extreme weather events and transmission losses in arid streams

Author
item SCHREINER-MCGRAW, ADAM - University Of California
item AJAMI, HOORI - Arizona State University
item VIVONI, ENRIQUE - Arizona State University

Submitted to: Environmental Research Letters
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: 6/12/2019
Publication Date: 7/22/2019
Citation: Schreiner-McGraw, A., Ajami, H., Vivoni, E. 2019. Extreme weather events and transmission losses in arid streams. Environmental Research Letters. 14(8):084002. https://doi.org/10.1088/1748-9326/ab2949.
DOI: https://doi.org/10.1088/1748-9326/ab2949

Interpretive Summary: Using a process-based hydrologic model, we investigate how potential changes to precipitation intensity and temperature will affect the water balance of a typical first-order, arid watershed located in the Chihuahuan Desert. Across many simulations, the average daily storm size is the primary factor that controls transmission losses with larger precipitation amounts increasing channel infiltration while simultaneously decreasing land surface evapotranspiration. As a result, climatic changes leading to larger, less frequent storms will result in higher channel transmission losses in arid regions.

Technical Abstract: Alimited understanding of how extreme weather events affect groundwater hinders our ability to predict climate change impacts in drylands, where channel transmission losses are often the primary recharge mechanism. In this study, we investigate how potential changes to precipitation intensity and temperature will affect the water balance of a typical first-order, arid watershed located in the Chihuahuan Desert.Weutilize a process-based hydrologic model driven by stochastically-downscaled simulations from a set of climate models, emissions scenarios, and future periods. Across many simulations, the average daily storm size is the primary factor that controls transmission losses with larger precipitation amounts increasing channel infiltration while simultaneously decreasing land surface evapotranspiration. Extreme events (>25mmd-1) that account for less than 30% of the annual precipitation, contribute almost 50% of the focused recharge. As a result, climatic changes leading to larger, less frequent storms will result in higher channel transmission losses in arid regions.