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Base Terrain and Bathymetry for the Middle Mississippi River

Dates

Publication Date
Start Date
1936-01-01
End Date
2015-12-31

Citation

Bulliner, E.A., Lindner, G.A., Remo, J., Jacobson, R.B., and Paukert, C.P., 2020, Science to inform management of floodplain conservation lands on the Middle Mississippi River: U.S. Geological Survey data release, https://doi.org/10.5066/P9AQ364R.

Summary

Within large-river ecosystems, floodplains serve a variety of important ecological functions. A recent survey of 80 managers of floodplain conservation lands along the Upper and Middle Mississippi and Lower Missouri Rivers in the central United States found that the most critical information needed to improve floodplain management centered on metrics for characterizing depth, extent, frequency, duration, and timing of inundation. These metrics can be delivered to managers efficiently through cloud-based interactive maps. To calculate these metrics, we interpolated an existing one-dimensional HEC-RAS hydraulic model for the Middle Mississippi River, which simulated water surface elevations at cross sections spaced (<1 kilometer) to [...]

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Attached Files

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Extension: BaseTerrainAndBathymetry.zip
BaseTerrainAndBathymetry.tif 11.61 MB
BaseTerrainAndBathymetry.tif-ColorRamp.SLD 2.09 KB

Purpose

This dataset was developed to quantify timing, extent, depth, and duration of inundation for floodplains on the Middle Mississippi River, and to assess relative potential for ecological restoration with a variety of biological endpoints. We developed a suite of metrics which characterize inundation timing and extent that will be useful to floodplain managers in for planning restoration efforts. We developed this layer to provide a base elevation from which to calculate inundation depths. This dataset is derived from multiple LIDAR and bathymetric surveys from a variety of state and federal agencies across several states.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9AQ364R

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