Period of Project: 2021 -
Study Area: Midwest
Cooperating Agency: Transportation Pooled Fund
Executive Summary (or Background):
The U.S. Geological Survey (USGS), in cooperation with the following State agencies:
- Illinois Department of Transportation,
- Iowa Department of Transportation,
- Minnesota Department of Transportation,
- Missouri Department of Transportation,
- North Dakota State Water Commission,
- South Dakota Department of Transportation, and
- Wisconsin Department of Transportation,
has undertaken a multi-year study to research methods for detecting and addressing potential trends in flood frequency distributions because of changes in climate, land use, and other potential drivers of change. This multi-state region represents complex variability in topography, ecoregions, land use, land cover, and climate. The region is characterized by abrupt transitions among high-relief, semi-mountainous areas, well-drained moderate-elevation plains, poorly drained low-elevation glaciated prairies, and other complex geologic and hydrologic features. The land use is mainly pasture and small grains to the west. The Corn Belt covers much of the center and eastern portion of the region and has recently expanded to the west and north. The region also contains major urban-suburban areas, centered on Chicago, Minneapolis-St. Paul, and St. Louis, which have expanded substantially during the proposed study period and thus are another source of non-stationarity.
Peak-flow frequency analysis is essential for flood insurance studies, floodplain management, and the design of transportation infrastructure. In recent decades, better understanding of long-term hydroclimatic persistence, as well as concerns about potential climate change and land-use change have caused the stationarity assumption, underpinning for flood-frequency analysis, to be reexamined. Although many important water-management activities are independently conducted within the sociopolitical state boundaries, regional hydrologic complexities transcend the state boundaries and are more efficiently handled from a regional perspective. This investigation will be conducted in collaboration with a national study funded by the Federal Highway Administration and will focus on specific issues that have the most impact on flood-frequency analysis within the multi-state region.
Objectives:
The overall goal of this study is to evaluate the combined effects of multidecadal climatic persistence (including hydroclimatic shifts), gradual climate change, and some aspects of land-use change on peak-flow frequency analyses in the multi-state region. This study is intended to provide a framework for addressing potential non-stationarity issues in statewide flood-frequency updates that commonly are conducted by the USGS in cooperation with state DOTs throughout the nation on an ongoing basis. This will be achieved through the following primary objectives:
- Define spatial and temporal characteristics of climatic persistence/change affecting annual peak flows in the multi-state region.
- Develop and apply a statistical methodology for estimating changes in peak-flow frequency distributions in the multi-state region in relation to climatic persistence/change and urbanization; the effects of rural and land-use change will only be investigated in an exploratory manner.
- Investigate methods for addressing regional climatic persistence/change and land-use change in peak-flow frequency analysis. To the extent possible, estimates of trend-adjusted flood magnitudes for various exceedance levels (such as the 10-percent or 1-percent annual exceedance probability) will be provided for comparison to previously published estimates.
Tasks:
The results of the proposed investigation will be presented in several peer-reviewed USGS Data Releases, Scientific Investigations Reports (SIR; online only), and journal articles and a USGS Fact Sheet or Story Map. Tasks include efforts to:
- Publicly release watershed-based climate data (metrics of precipitation and temperature) on a monthly time scale and summed to annual seasonal and annual total values. These data will also contain trend results for trends in climate metrics in annual peak streamflow and climate variables.
- Characterize the effects of natural hydroclimatic shifts and potential climate change on annual peak flows in Midwest: Illinois, Iowa, Minnesota, Missouri, North Dakota, South Dakota and Wisconsin.
- Analyze the seasonality of flood peaks in the region and their trends and implications for trend attribution.
- Evaluate the effect of urbanization on flood-peaks in major metropolitan areas in the study region.
- Analyze, compile, and publish regional tile drainage data for study reproducibility and documentation
- Publicly release data that compares adjustment methods at individual sites, such as multiple flood-frequency analysis results.
- Summarize methods for addressing regional hydroclimatic shifts, climate change, and land-use change in peak-flow frequency analyses in the Midwest.
- Succinctly summarize the above work in a short fact sheet that provides links to project products to make it easy to find data and results which can be handed out at future meetings, sent to managers for an overview, etc.
- Receive science communication training from the Alda Center for Communicating Science (funded by USGS Midcontinent Region as an extension to this project).
Below are publications associated with this project or past related projects.
Flood-frequency estimation for very low annual exceedance probabilities using historical, paleoflood, and regional information with consideration of nonstationarity
Causal effect of impervious cover on annual flood magnitude for the United States
Change points in annual peak streamflows: Method comparisons and historical change points in the United States
Techniques for estimating the magnitude and frequency of peak flows on small streams in the binational U.S. and Canadian Lake of the Woods–Rainy River Basin upstream from Kenora, Ontario, Canada, based on data through water year 2013
The U.S. Geological Survey Peak-Flow File Data Verification Project, 2008–16
2011 Souris River flood—Will it happen again?
Adjusting annual maximum peak discharges at selected stations in northeastern Illinois for changes in land-use conditions
Estimation of peak discharge quantiles for selected annual exceedance probabilities in northeastern Illinois
Tree-ring-based estimates of long-term seasonal precipitation in the Souris River Region of Saskatchewan, North Dakota and Manitoba
Stochastic model for simulating Souris River Basin precipitation, evapotranspiration, and natural streamflow
Changes in seasonality and timing of peak streamflow in snow and semi-arid climates of the north-central United States, 1910–2012
Trends in annual, seasonal, and monthly streamflow characteristics at 227 streamgages in the Missouri River watershed, water years 1960-2011
- Overview
Period of Project: 2021 -
Study Area: Midwest
Cooperating Agency: Transportation Pooled Fund
Executive Summary (or Background):
The U.S. Geological Survey (USGS), in cooperation with the following State agencies:
- Illinois Department of Transportation,
- Iowa Department of Transportation,
- Minnesota Department of Transportation,
- Missouri Department of Transportation,
- North Dakota State Water Commission,
- South Dakota Department of Transportation, and
- Wisconsin Department of Transportation,
has undertaken a multi-year study to research methods for detecting and addressing potential trends in flood frequency distributions because of changes in climate, land use, and other potential drivers of change. This multi-state region represents complex variability in topography, ecoregions, land use, land cover, and climate. The region is characterized by abrupt transitions among high-relief, semi-mountainous areas, well-drained moderate-elevation plains, poorly drained low-elevation glaciated prairies, and other complex geologic and hydrologic features. The land use is mainly pasture and small grains to the west. The Corn Belt covers much of the center and eastern portion of the region and has recently expanded to the west and north. The region also contains major urban-suburban areas, centered on Chicago, Minneapolis-St. Paul, and St. Louis, which have expanded substantially during the proposed study period and thus are another source of non-stationarity.
Peak-flow frequency analysis is essential for flood insurance studies, floodplain management, and the design of transportation infrastructure. In recent decades, better understanding of long-term hydroclimatic persistence, as well as concerns about potential climate change and land-use change have caused the stationarity assumption, underpinning for flood-frequency analysis, to be reexamined. Although many important water-management activities are independently conducted within the sociopolitical state boundaries, regional hydrologic complexities transcend the state boundaries and are more efficiently handled from a regional perspective. This investigation will be conducted in collaboration with a national study funded by the Federal Highway Administration and will focus on specific issues that have the most impact on flood-frequency analysis within the multi-state region.
USGS responds to spring flooding in North Dakota. (Credit: Ernie McCoy, USGS. Public domain.) Objectives:
The overall goal of this study is to evaluate the combined effects of multidecadal climatic persistence (including hydroclimatic shifts), gradual climate change, and some aspects of land-use change on peak-flow frequency analyses in the multi-state region. This study is intended to provide a framework for addressing potential non-stationarity issues in statewide flood-frequency updates that commonly are conducted by the USGS in cooperation with state DOTs throughout the nation on an ongoing basis. This will be achieved through the following primary objectives:
- Define spatial and temporal characteristics of climatic persistence/change affecting annual peak flows in the multi-state region.
- Develop and apply a statistical methodology for estimating changes in peak-flow frequency distributions in the multi-state region in relation to climatic persistence/change and urbanization; the effects of rural and land-use change will only be investigated in an exploratory manner.
- Investigate methods for addressing regional climatic persistence/change and land-use change in peak-flow frequency analysis. To the extent possible, estimates of trend-adjusted flood magnitudes for various exceedance levels (such as the 10-percent or 1-percent annual exceedance probability) will be provided for comparison to previously published estimates.
Verification of high water mark on Whitewood Creek above Whitewood, SD. (Credit: Wyatt Tatge. Public domain.) Tasks:
The results of the proposed investigation will be presented in several peer-reviewed USGS Data Releases, Scientific Investigations Reports (SIR; online only), and journal articles and a USGS Fact Sheet or Story Map. Tasks include efforts to:
- Publicly release watershed-based climate data (metrics of precipitation and temperature) on a monthly time scale and summed to annual seasonal and annual total values. These data will also contain trend results for trends in climate metrics in annual peak streamflow and climate variables.
- Characterize the effects of natural hydroclimatic shifts and potential climate change on annual peak flows in Midwest: Illinois, Iowa, Minnesota, Missouri, North Dakota, South Dakota and Wisconsin.
- Analyze the seasonality of flood peaks in the region and their trends and implications for trend attribution.
- Evaluate the effect of urbanization on flood-peaks in major metropolitan areas in the study region.
- Analyze, compile, and publish regional tile drainage data for study reproducibility and documentation
- Publicly release data that compares adjustment methods at individual sites, such as multiple flood-frequency analysis results.
- Summarize methods for addressing regional hydroclimatic shifts, climate change, and land-use change in peak-flow frequency analyses in the Midwest.
- Succinctly summarize the above work in a short fact sheet that provides links to project products to make it easy to find data and results which can be handed out at future meetings, sent to managers for an overview, etc.
- Receive science communication training from the Alda Center for Communicating Science (funded by USGS Midcontinent Region as an extension to this project).
USGS hydrologist Rod Caldwell observed by cows at O'Fallon Creek near Mildred, Montana. (Credit: Todd Preston, USGS contractor. Public domain.) Sheyenne River at Baldhill Dam north of Valley City, North Dakota. Streamflow was approximately 6,500 cubic feet per second. (Credit: Kathleen M. Rowland, U.S. Geological Survey. Public domain.) - Publications
Below are publications associated with this project or past related projects.
Filter Total Items: 39Flood-frequency estimation for very low annual exceedance probabilities using historical, paleoflood, and regional information with consideration of nonstationarity
Streamflow estimates for floods with an annual exceedance probability of 0.001 or lower are needed to accurately portray risks to critical infrastructure, such as nuclear powerplants and large dams. However, extrapolating flood-frequency curves developed from at-site systematic streamflow records to very low annual exceedance probabilities (less than 0.001) results in large uncertainties in the stCausal effect of impervious cover on annual flood magnitude for the United States
Despite consensus that impervious surfaces increase flooding, the magnitude of the increase remains uncertain. This uncertainty largely stems from the challenge of isolating the effect of changes in impervious cover separate from other factors that also affect flooding. To control for these factors, prior study designs rely on either temporal or spatial variation in impervious cover. We leverage bChange points in annual peak streamflows: Method comparisons and historical change points in the United States
Change-point, or step-trend, detection is an active area of research in statistics and an area of great interest in hydrology because change points may be evidence of natural or anthropogenic changes in climatic, hydrologic, or landscape processes. A common change-point technique is the Pettitt test; however, many change-point methods are now available and testing of methods has been limited. ThisTechniques for estimating the magnitude and frequency of peak flows on small streams in the binational U.S. and Canadian Lake of the Woods–Rainy River Basin upstream from Kenora, Ontario, Canada, based on data through water year 2013
A binational study was initiated to update statistical equations that are used to estimate the magnitude and frequency of peak flows on streams in Manitoba and Ontario, Canada, and Minnesota that are contained within the binational Lake of the Woods–Rainy River Basin upstream from Kenora, Ontario, Canada. Hydraulic engineers use peak streamflow data to inform designs of bridges, culverts, and damsThe U.S. Geological Survey Peak-Flow File Data Verification Project, 2008–16
Annual peak streamflow (peak flow) at a streamgage is defined as the maximum instantaneous flow in a water year. A water year begins on October 1 and continues through September 30 of the following year; for example, water year 2015 extends from October 1, 2014, through September 30, 2015. The accuracy, characterization, and completeness of the peak streamflow data are critical in determining floo2011 Souris River flood—Will it happen again?
The Souris River Basin is a 61,000 square kilometer basin in the provinces of Saskatchewan and Manitoba and the state of North Dakota. Record setting rains in May and June of 2011 led to record flooding with peak annual streamflow values (762 cubic meters per second [m3/s]) more than twice that of any previously recorded peak streamflow and more than five times the estimated 100 year postregulatioAdjusting annual maximum peak discharges at selected stations in northeastern Illinois for changes in land-use conditions
The effects of urbanization on annual maximum peak discharges in northeastern Illinois and nearby areas from 1945 to 2009 were analyzed with a two-step longitudinal-quantile linear regression approach. The peak discharges were then adjusted to 2010 land-use conditions. The explanatory variables used were daily precipitation at the time of the peak discharge event and a housing density-based measurEstimation of peak discharge quantiles for selected annual exceedance probabilities in northeastern Illinois
This report provides two sets of equations for estimating peak discharge quantiles at annual exceedance probabilities (AEPs) of 0.50, 0.20, 0.10, 0.04, 0.02, 0.01, 0.005, and 0.002 (recurrence intervals of 2, 5, 10, 25, 50, 100, 200, and 500 years, respectively) for watersheds in Illinois based on annual maximum peak discharge data from 117 watersheds in and near northeastern Illinois. One set ofTree-ring-based estimates of long-term seasonal precipitation in the Souris River Region of Saskatchewan, North Dakota and Manitoba
Historically unprecedented flooding occurred in the Souris River Basin of Saskatchewan, North Dakota and Manitoba in 2011, during a longer term period of wet conditions in the basin. In order to develop a model of future flows, there is a need to evaluate effects of past multidecadal climate variability and/or possible climate change on precipitation. In this study, tree-ring chronologies and histStochastic model for simulating Souris River Basin precipitation, evapotranspiration, and natural streamflow
The Souris River Basin is a 61,000-square-kilometer basin in the Provinces of Saskatchewan and Manitoba and the State of North Dakota. In May and June of 2011, record-setting rains were seen in the headwater areas of the basin. Emergency spillways of major reservoirs were discharging at full or nearly full capacity, and extensive flooding was seen in numerous downstream communities. To determine tChanges in seasonality and timing of peak streamflow in snow and semi-arid climates of the north-central United States, 1910–2012
Changes in the seasonality and timing of annual peak streamflow in the north-central USA are likely because of changes in precipitation and temperature regimes. A source of long-term information about flood events across the study area is the U.S. Geological Survey peak streamflow database. However, one challenge of answering climate-related questions with this dataset is that even in snowmelt-domTrends in annual, seasonal, and monthly streamflow characteristics at 227 streamgages in the Missouri River watershed, water years 1960-2011
The Missouri River and its tributaries are an important resource that serve multiple uses including agriculture, energy, recreation, and municipal water supply. Understanding historical streamflow characteristics provides relevant guidance to adaptive management of these water resources. Streamflow records in the Missouri River watershed were examined for trends in time series of annual, seasonal, - Partners