Investigating the Influence of Variable Freshwater Ice Types on Passive and Active Microwave Observations

Dual-polarized airborne passive microwave (PM) brightness temperatures (Tb) at 6.9 GHz H/V, 19 GHz H/V and 37 GHz H/V and spaceborne active microwave (AM) X-band (9.65 GHz VV, VH) backscatter (σ0) are observed coincident to in situ snow and lake-ice measurements collected over two lakes near Inuvik,...

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Main Authors: Grant E. Gunn, Claude R. Duguay, Chris Derksen, David A. Clausi, Peter Toose
Format: Article
Language:English
Published: MDPI AG 2017-12-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/9/12/1242
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author Grant E. Gunn
Claude R. Duguay
Chris Derksen
David A. Clausi
Peter Toose
author_facet Grant E. Gunn
Claude R. Duguay
Chris Derksen
David A. Clausi
Peter Toose
author_sort Grant E. Gunn
collection DOAJ
description Dual-polarized airborne passive microwave (PM) brightness temperatures (Tb) at 6.9 GHz H/V, 19 GHz H/V and 37 GHz H/V and spaceborne active microwave (AM) X-band (9.65 GHz VV, VH) backscatter (σ0) are observed coincident to in situ snow and lake-ice measurements collected over two lakes near Inuvik, Canada. Lake-ice thickness is found to be positively correlated with 19 GHz V emission (R = 0.67) and negatively with 19 GHz H emission (R = −0.79), indicating surface ice conditions influence microwave interaction. Lake ice types are delineated from TerraSAR-X synthetic aperture radar (SAR) images using the iterative region growing with semantics (IRGS) segmentation algorithm implemented in the MAGIC (MAp Guided Ice Classification) system. The spatial extent of derived ice type classes correspond well to in situ observations. The overall magnitude of emission at 19 GHz H and X-band VH σ0 increase with the scattering potential of associated ice types (grey/rafted ice). Transects of 6.9 GHz PM and 19 GHz PM exhibit positive relationships with VH σ0 over freshwater lake ice, with the greatest R coefficients at H-pol (R = 0.64, 0.46). Conversely, 6.9 GHz Tb and 19 GHz Tb exhibit negative R coefficients in regions of brackish water due to tubular bubble and brine inclusions in the ice. This study identifies congruency between PM and AM scattering mechanisms over lake ice for the purpose of identifying the influence of ice types on overall microwave interaction within the lake-ice system.
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spelling doaj.art-b8b582516ab64df2810b4932fc66f3802022-12-21T19:41:49ZengMDPI AGRemote Sensing2072-42922017-12-01912124210.3390/rs9121242rs9121242Investigating the Influence of Variable Freshwater Ice Types on Passive and Active Microwave ObservationsGrant E. Gunn0Claude R. Duguay1Chris Derksen2David A. Clausi3Peter Toose4Department of Geography, Environment and Spatial Sciences, Michigan State University, East Lansing, MI 48824, USADepartment of Geography and Environmental Management, and the Interdisciplinary Centre on Climate Change, University of Waterloo, Waterloo, ON N2L 3G1, CanadaClimate Research Division, Environment and Climate Change Canada, Toronto, ON M3H 5T4, CanadaDepartment of Systems Design Engineering and Vision and Image Processing (VIP) Research Group, University of Waterloo, Waterloo, ON N2L 3G1, CanadaClimate Research Division, Environment and Climate Change Canada, Toronto, ON M3H 5T4, CanadaDual-polarized airborne passive microwave (PM) brightness temperatures (Tb) at 6.9 GHz H/V, 19 GHz H/V and 37 GHz H/V and spaceborne active microwave (AM) X-band (9.65 GHz VV, VH) backscatter (σ0) are observed coincident to in situ snow and lake-ice measurements collected over two lakes near Inuvik, Canada. Lake-ice thickness is found to be positively correlated with 19 GHz V emission (R = 0.67) and negatively with 19 GHz H emission (R = −0.79), indicating surface ice conditions influence microwave interaction. Lake ice types are delineated from TerraSAR-X synthetic aperture radar (SAR) images using the iterative region growing with semantics (IRGS) segmentation algorithm implemented in the MAGIC (MAp Guided Ice Classification) system. The spatial extent of derived ice type classes correspond well to in situ observations. The overall magnitude of emission at 19 GHz H and X-band VH σ0 increase with the scattering potential of associated ice types (grey/rafted ice). Transects of 6.9 GHz PM and 19 GHz PM exhibit positive relationships with VH σ0 over freshwater lake ice, with the greatest R coefficients at H-pol (R = 0.64, 0.46). Conversely, 6.9 GHz Tb and 19 GHz Tb exhibit negative R coefficients in regions of brackish water due to tubular bubble and brine inclusions in the ice. This study identifies congruency between PM and AM scattering mechanisms over lake ice for the purpose of identifying the influence of ice types on overall microwave interaction within the lake-ice system.https://www.mdpi.com/2072-4292/9/12/1242active microwavepassive microwavesynthetic aperture radarlake iceice typesX-bandgrey icerafted iceTerraSAR-X
spellingShingle Grant E. Gunn
Claude R. Duguay
Chris Derksen
David A. Clausi
Peter Toose
Investigating the Influence of Variable Freshwater Ice Types on Passive and Active Microwave Observations
Remote Sensing
active microwave
passive microwave
synthetic aperture radar
lake ice
ice types
X-band
grey ice
rafted ice
TerraSAR-X
title Investigating the Influence of Variable Freshwater Ice Types on Passive and Active Microwave Observations
title_full Investigating the Influence of Variable Freshwater Ice Types on Passive and Active Microwave Observations
title_fullStr Investigating the Influence of Variable Freshwater Ice Types on Passive and Active Microwave Observations
title_full_unstemmed Investigating the Influence of Variable Freshwater Ice Types on Passive and Active Microwave Observations
title_short Investigating the Influence of Variable Freshwater Ice Types on Passive and Active Microwave Observations
title_sort investigating the influence of variable freshwater ice types on passive and active microwave observations
topic active microwave
passive microwave
synthetic aperture radar
lake ice
ice types
X-band
grey ice
rafted ice
TerraSAR-X
url https://www.mdpi.com/2072-4292/9/12/1242
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