H186-04
A Global Analysis of Streamflow in a Changing World

Tuesday, 15 December 2020: 17:42
Virtual
Brian Brown1, Benjamin W Abbott1, Aimee H Fullerton2, Christopher James Sergeant3, Flavia Tromboni4, Arial Shogren5, J Angus Webb6, Daniel Allen7, Jay P Zarnetske5, Lenka Kuglerová8, Claire Marie Ruffing-Cathcart9, Darin Kopp7, Eric Sokol10, Matthew Heaton11 and Jeremy Jones12, (1)Brigham Young University, Provo, UT, United States, (2)NOAA Fisheries, Northwest Fisheries Science Center, Seattle, WA, United States, (3)University of Alaska Fairbanks, College of Fisheries and Ocean Sciences, Fairbanks, AK, United States, (4)University of Nevada Reno, Biology, Reno, United States, (5)Michigan State University, Department of Earth and Environmental Sciences, East Lansing, MI, United States, (6)University of Melbourne, Department of Infrastructure Engineering, Parkville, Australia, (7)University of Oklahoma Norman Campus, Biology, Norman, OK, United States, (8)SLU Swedish University of Agricultural Sciences Umea, Umea, Sweden, (9)University of British Columbia, Vancouver, BC, Canada, (10)Institute of Arctic and Alpine Research, Boulder, CO, United States, (11)Brigham Young University, Statistics, Provo, UT, United States, (12)University of Alaska Fairbanks, Fairbanks, AK, United States
Abstract:
Streamflow regime influences human societies, aquatic ecosystems, and biogeochemical cycles. Despite its importance, a unified method for describing streamflow has not emerged; several hundred metrics of flow have been proposed, and their usefulness is still debated by the community. Here we show that a single frequency decomposition can capture most of the information present in currently used flow metrics. We also show that PCA dimensionality reduction can be used to further simplify the continuous output from a frequency decomposition into a few axes that describe fundamental combinations of frequencies commonly observed throughout the world. This same technique can be applied to raw hydrographs to condense non-frequency characteristics of streamflow into a few additional axes describing magnitude and seasonality. We found little evidence of clustering, instead observing continuous variation in flow regime associated with several ecological gradients, especially stream order (i.e. watershed size) and human influence. We also applied these descriptors to quantify global alterations in streamflow during the last ~30 years. Finally, we found that a transposed PCA dimensionality reduction effectively described the autocorrelation between days in the hydrological year, demonstrating that global day-to-day alterations in magnitude can be described by a handful of variables. We conclude that these continuous descriptions of streamflow regime provide a unified, global framework for characterizing flow regime, complementing and potentially subsuming the information described by previously proposed metrics.