Remote Sensing to Characterize River Floodplain Structure and Function

Advancing understanding of the complexities and expansive spatial scales of river ecology can be enhanced through the application of remote sensing. We obtained satellite (Quickbird) and airborne (LIDAR, hyperspectral, multispectral, and thermal) imagery data of an alluvial gravel-bed river floodpla...

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Main Authors: F. Richard Hauer, Mark S. Lorang, Tom Gonser
Format: Article
Language:English
Published: MDPI AG 2022-02-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/14/5/1132
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author F. Richard Hauer
Mark S. Lorang
Tom Gonser
author_facet F. Richard Hauer
Mark S. Lorang
Tom Gonser
author_sort F. Richard Hauer
collection DOAJ
description Advancing understanding of the complexities and expansive spatial scales of river ecology can be enhanced through the application of remote sensing. We obtained satellite (Quickbird) and airborne (LIDAR, hyperspectral, multispectral, and thermal) imagery data of an alluvial gravel-bed river floodplain in western Montana to quantify both riparian and aquatic habitats and processes. LIDAR data provided a detailed bare earth DEM and vegetation canopy DEM. We classified river hydraulics and aquatic habitats using a combination of the satellite multispectral, airborne hyperspectral, and LIDAR data coupled with spatially-explicit acoustic Doppler velocity profile data of water depth and velocity. Velocity, depth, and Froude classifications were aggregated into similar hydraulic zones of river habitat classes. Thermal imagery data were coupled with field measurements of temperature and radon gas tracer to identify patterns of water exchange between the alluvial aquifer and the surface. We found a high complexity of aquatic surface temperatures and radon tracer linked to groundwater discharge from the alluvial aquifer. Airborne hyperspectral data were used to identify “hot spots” of periphyton production, which coincided with the complex nature of groundwater–surface water exchange. Airborne hyperspectral data provided differentiation of vegetation patches by dominant species. When the hyperspectral data were coupled to LIDAR first return metrics, we were able to determine vegetation canopy height and relative vegetation patch age classes. The integration of these various remote sensing sources allowed us to characterize the distribution and abundance of floodplain aquatic and riparian species and model processes of change through space and time.
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spelling doaj.art-03a3f14d868d4fd7b0e0fe8188574d9e2023-11-23T23:41:58ZengMDPI AGRemote Sensing2072-42922022-02-01145113210.3390/rs14051132Remote Sensing to Characterize River Floodplain Structure and FunctionF. Richard Hauer0Mark S. Lorang1Tom Gonser2Flathead Lake Biological Station, University of Montana, Polson, MT 59864, USAFlathead Lake Biological Station, University of Montana, Polson, MT 59864, USACenter for Ecology, Evolution and Biogeochemistry (CEEB), Department of Aquatic Ecology, EAWAG, 6047 Kastanienbaum, SwitzerlandAdvancing understanding of the complexities and expansive spatial scales of river ecology can be enhanced through the application of remote sensing. We obtained satellite (Quickbird) and airborne (LIDAR, hyperspectral, multispectral, and thermal) imagery data of an alluvial gravel-bed river floodplain in western Montana to quantify both riparian and aquatic habitats and processes. LIDAR data provided a detailed bare earth DEM and vegetation canopy DEM. We classified river hydraulics and aquatic habitats using a combination of the satellite multispectral, airborne hyperspectral, and LIDAR data coupled with spatially-explicit acoustic Doppler velocity profile data of water depth and velocity. Velocity, depth, and Froude classifications were aggregated into similar hydraulic zones of river habitat classes. Thermal imagery data were coupled with field measurements of temperature and radon gas tracer to identify patterns of water exchange between the alluvial aquifer and the surface. We found a high complexity of aquatic surface temperatures and radon tracer linked to groundwater discharge from the alluvial aquifer. Airborne hyperspectral data were used to identify “hot spots” of periphyton production, which coincided with the complex nature of groundwater–surface water exchange. Airborne hyperspectral data provided differentiation of vegetation patches by dominant species. When the hyperspectral data were coupled to LIDAR first return metrics, we were able to determine vegetation canopy height and relative vegetation patch age classes. The integration of these various remote sensing sources allowed us to characterize the distribution and abundance of floodplain aquatic and riparian species and model processes of change through space and time.https://www.mdpi.com/2072-4292/14/5/1132riverfloodplainsatellite imageryairborne imagerythermal imageryLIDAR
spellingShingle F. Richard Hauer
Mark S. Lorang
Tom Gonser
Remote Sensing to Characterize River Floodplain Structure and Function
Remote Sensing
river
floodplain
satellite imagery
airborne imagery
thermal imagery
LIDAR
title Remote Sensing to Characterize River Floodplain Structure and Function
title_full Remote Sensing to Characterize River Floodplain Structure and Function
title_fullStr Remote Sensing to Characterize River Floodplain Structure and Function
title_full_unstemmed Remote Sensing to Characterize River Floodplain Structure and Function
title_short Remote Sensing to Characterize River Floodplain Structure and Function
title_sort remote sensing to characterize river floodplain structure and function
topic river
floodplain
satellite imagery
airborne imagery
thermal imagery
LIDAR
url https://www.mdpi.com/2072-4292/14/5/1132
work_keys_str_mv AT frichardhauer remotesensingtocharacterizeriverfloodplainstructureandfunction
AT markslorang remotesensingtocharacterizeriverfloodplainstructureandfunction
AT tomgonser remotesensingtocharacterizeriverfloodplainstructureandfunction