Regional Analysis of the Dependence of Peak-Flow Quantiles on Climate with Application to Adjustment to Climate Trends

Standard flood-frequency analysis methods rely on an assumption of stationarity, but because of growing understanding of climatic persistence and concern regarding the effects of climate change, the need for methods to detect and model nonstationary flood frequency has become widely recognized. In t...

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Main Authors: Thomas Over, Mackenzie Marti, Hannah Podzorski
Format: Article
Language:English
Published: MDPI AG 2025-05-01
Series:Hydrology
Subjects:
Online Access:https://www.mdpi.com/2306-5338/12/5/119
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author Thomas Over
Mackenzie Marti
Hannah Podzorski
author_facet Thomas Over
Mackenzie Marti
Hannah Podzorski
author_sort Thomas Over
collection DOAJ
description Standard flood-frequency analysis methods rely on an assumption of stationarity, but because of growing understanding of climatic persistence and concern regarding the effects of climate change, the need for methods to detect and model nonstationary flood frequency has become widely recognized. In this study, a regional statistical method for estimating the effects of climate variations on annual maximum (peak) flows that allows for the effect to vary by quantile is presented and applied. The method uses a panel–quantile regression framework based on a location-scale model with two fixed effects per basin. The model was fitted to 330 selected gauged basins in the midwestern United States, filtered to remove basins affected by reservoir regulation and urbanization. Precipitation and discharge simulated using a water-balance model at daily and annual time scales were tested as climate variables. Annual maximum daily discharge was found to be the best predictor of peak flows, and the quantile regression coefficients were found to depend monotonically on annual exceedance probability. Application of the models to gauged basins is demonstrated by estimating the peak-flow distributions at the end of the study period (2018) and, using the panel model, to the study basins as-if-ungauged by using leave-one-out cross validation, estimating the fixed effects using static basin characteristics, and parameterizing the water-balance model discharge using median parameters. The errors of the quantiles predicted as-if-ungauged approximately doubled compared to the errors of the fitted panel model.
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spelling doaj-art-775665c2e2184694a829fd2a6d3e019e2025-08-20T03:47:54ZengMDPI AGHydrology2306-53382025-05-0112511910.3390/hydrology12050119Regional Analysis of the Dependence of Peak-Flow Quantiles on Climate with Application to Adjustment to Climate TrendsThomas Over0Mackenzie Marti1Hannah Podzorski2Central Midwest Water Science Center, U.S. Geological Survey, Urbana, IL 61801, USACentral Midwest Water Science Center, U.S. Geological Survey, Urbana, IL 61801, USACentral Midwest Water Science Center, U.S. Geological Survey, Iowa City, IA 52240, USAStandard flood-frequency analysis methods rely on an assumption of stationarity, but because of growing understanding of climatic persistence and concern regarding the effects of climate change, the need for methods to detect and model nonstationary flood frequency has become widely recognized. In this study, a regional statistical method for estimating the effects of climate variations on annual maximum (peak) flows that allows for the effect to vary by quantile is presented and applied. The method uses a panel–quantile regression framework based on a location-scale model with two fixed effects per basin. The model was fitted to 330 selected gauged basins in the midwestern United States, filtered to remove basins affected by reservoir regulation and urbanization. Precipitation and discharge simulated using a water-balance model at daily and annual time scales were tested as climate variables. Annual maximum daily discharge was found to be the best predictor of peak flows, and the quantile regression coefficients were found to depend monotonically on annual exceedance probability. Application of the models to gauged basins is demonstrated by estimating the peak-flow distributions at the end of the study period (2018) and, using the panel model, to the study basins as-if-ungauged by using leave-one-out cross validation, estimating the fixed effects using static basin characteristics, and parameterizing the water-balance model discharge using median parameters. The errors of the quantiles predicted as-if-ungauged approximately doubled compared to the errors of the fitted panel model.https://www.mdpi.com/2306-5338/12/5/119flood frequencynonstationarityclimate variationregressionwater balancemidwestern United States
spellingShingle Thomas Over
Mackenzie Marti
Hannah Podzorski
Regional Analysis of the Dependence of Peak-Flow Quantiles on Climate with Application to Adjustment to Climate Trends
Hydrology
flood frequency
nonstationarity
climate variation
regression
water balance
midwestern United States
title Regional Analysis of the Dependence of Peak-Flow Quantiles on Climate with Application to Adjustment to Climate Trends
title_full Regional Analysis of the Dependence of Peak-Flow Quantiles on Climate with Application to Adjustment to Climate Trends
title_fullStr Regional Analysis of the Dependence of Peak-Flow Quantiles on Climate with Application to Adjustment to Climate Trends
title_full_unstemmed Regional Analysis of the Dependence of Peak-Flow Quantiles on Climate with Application to Adjustment to Climate Trends
title_short Regional Analysis of the Dependence of Peak-Flow Quantiles on Climate with Application to Adjustment to Climate Trends
title_sort regional analysis of the dependence of peak flow quantiles on climate with application to adjustment to climate trends
topic flood frequency
nonstationarity
climate variation
regression
water balance
midwestern United States
url https://www.mdpi.com/2306-5338/12/5/119
work_keys_str_mv AT thomasover regionalanalysisofthedependenceofpeakflowquantilesonclimatewithapplicationtoadjustmenttoclimatetrends
AT mackenziemarti regionalanalysisofthedependenceofpeakflowquantilesonclimatewithapplicationtoadjustmenttoclimatetrends
AT hannahpodzorski regionalanalysisofthedependenceofpeakflowquantilesonclimatewithapplicationtoadjustmenttoclimatetrends