Abstract

We compared modeled and observed streamflow trends from 1984 to 2016 using five statistical transfer models and one deterministic, distributed-parameter, process-based model, for 26 flow metrics at 502 basins in the United States that are minimally influenced by development. We also looked at a measure of overall model fit and average bias. A higher percentage of basins, for all models, had relatively low trend differences between modeled and observed mean/median flows than for very high or low flows such as the annual 1-day high and 7-day low flows. Mean-flow metrics also had the largest percentage of basins with relatively good overall model fit and low bias. The five statistical transfer models performed better at more basins than the process-based model. The overall model fit for all models, for mean and/or high flows, was correlated with one or more measures of basin precipitation or aridity. Our study and previous studies generally observed good model performance for high flows up to 90th or 95th percentile flows. However, we found model performance was substantially worse for more extreme flows, including 99th percentile and annual 1-day high flows, indicating the importance of including more extreme high flows in analyses of model performance.

Highlights

  • Streamflow records are important for effective management of water resources for rivers, streams, and reservoirs [1]

  • Overall differences in trends were based on results from hundreds of diverse but minimally altered basins across the conterminous U.S Trends were compared between metrics (13 annual-flow metrics, a measure of snowmelt-related streamflow timing, and monthly mean flows) and between six models

  • In addition to trend comparisons, we compared modeled and observed streamflow metrics using a measure of model fit, volumetric efficiency, and with a measure of bias

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Summary

Introduction

Streamflow records are important for effective management of water resources for rivers, streams, and reservoirs [1]. 7-day low flows (e.g., U.S Environmental Protection Agency [3]) can be determined from the daily values. Changing flows over time are important to water management, as climatic changes and basin development can increase or decrease flows (e.g., Hodgkins et al, Dudley et al, Vincente-Serrano [4,5,6]). There have been increases in peak flows for many basins in the Northeast and Midwest and many decreases in the West and South [4]. There have been many increases in the Northeast and Midwest and many decreases in the Southeast [5]

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