Variations of Microwave Scattering Properties by Seasonal Freeze/Thaw Transition in the Permafrost Active Layer Observed by ALOS PALSAR Polarimetric Data

Radar backscattering properties can be extremely sensitive to the freeze/thaw states of the ground surface. This study aims to evaluate the changes of L-band microwave scattering characteristics between thawed and frozen conditions by using polarimetric scattering mechanism indicators. ALOS PALSAR p...

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Published in:Remote Sensing
Main Author: Sang-Eun Park
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2015
Subjects:
Online Access:https://doi.org/10.3390/rs71215874
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author Sang-Eun Park
author_facet Sang-Eun Park
author_sort Sang-Eun Park
collection MDPI Open Access Publishing
container_issue 12
container_start_page 17135
container_title Remote Sensing
container_volume 7
description Radar backscattering properties can be extremely sensitive to the freeze/thaw states of the ground surface. This study aims to evaluate the changes of L-band microwave scattering characteristics between thawed and frozen conditions by using polarimetric scattering mechanism indicators. ALOS PALSAR polarimetric mode data acquired in winter and spring seasons over Eastern Siberia are used in this study. Experimental results show that the actual scattering mechanisms and their seasonal variations over various forested and non-forested permafrost ecosystems can be successfully characterized by the polarimetric target decomposition parameters and the polarimetric coherences. In addition, fully polarimetric radar observations exhibit great potential for mapping land cover types and surficial features in the permafrost active layer. Particularly, the co-polarization coherences on the HV-polarization basis and circular-polarization basis were found to be very useful for discriminating different surficial geocryological characteristics in recently burnt forests and thermokarst regions.
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Thermokarst
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spelling ftmdpi:oai:mdpi.com:/2072-4292/7/12/15874/ 2025-01-17T00:14:23+00:00 Variations of Microwave Scattering Properties by Seasonal Freeze/Thaw Transition in the Permafrost Active Layer Observed by ALOS PALSAR Polarimetric Data Sang-Eun Park agris 2015-12-18 application/pdf https://doi.org/10.3390/rs71215874 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/rs71215874 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 7; Issue 12; Pages: 17135-17148 synthetic aperture radar (SAR) radar polarimetry microwave scattering mechanism permafrost active layer freeze/thaw ALOS PALSAR Text 2015 ftmdpi https://doi.org/10.3390/rs71215874 2023-07-31T20:48:55Z Radar backscattering properties can be extremely sensitive to the freeze/thaw states of the ground surface. This study aims to evaluate the changes of L-band microwave scattering characteristics between thawed and frozen conditions by using polarimetric scattering mechanism indicators. ALOS PALSAR polarimetric mode data acquired in winter and spring seasons over Eastern Siberia are used in this study. Experimental results show that the actual scattering mechanisms and their seasonal variations over various forested and non-forested permafrost ecosystems can be successfully characterized by the polarimetric target decomposition parameters and the polarimetric coherences. In addition, fully polarimetric radar observations exhibit great potential for mapping land cover types and surficial features in the permafrost active layer. Particularly, the co-polarization coherences on the HV-polarization basis and circular-polarization basis were found to be very useful for discriminating different surficial geocryological characteristics in recently burnt forests and thermokarst regions. Text permafrost Thermokarst Siberia MDPI Open Access Publishing Remote Sensing 7 12 17135 17148
spellingShingle synthetic aperture radar (SAR)
radar polarimetry
microwave scattering mechanism
permafrost active layer
freeze/thaw
ALOS PALSAR
Sang-Eun Park
Variations of Microwave Scattering Properties by Seasonal Freeze/Thaw Transition in the Permafrost Active Layer Observed by ALOS PALSAR Polarimetric Data
title Variations of Microwave Scattering Properties by Seasonal Freeze/Thaw Transition in the Permafrost Active Layer Observed by ALOS PALSAR Polarimetric Data
title_full Variations of Microwave Scattering Properties by Seasonal Freeze/Thaw Transition in the Permafrost Active Layer Observed by ALOS PALSAR Polarimetric Data
title_fullStr Variations of Microwave Scattering Properties by Seasonal Freeze/Thaw Transition in the Permafrost Active Layer Observed by ALOS PALSAR Polarimetric Data
title_full_unstemmed Variations of Microwave Scattering Properties by Seasonal Freeze/Thaw Transition in the Permafrost Active Layer Observed by ALOS PALSAR Polarimetric Data
title_short Variations of Microwave Scattering Properties by Seasonal Freeze/Thaw Transition in the Permafrost Active Layer Observed by ALOS PALSAR Polarimetric Data
title_sort variations of microwave scattering properties by seasonal freeze/thaw transition in the permafrost active layer observed by alos palsar polarimetric data
topic synthetic aperture radar (SAR)
radar polarimetry
microwave scattering mechanism
permafrost active layer
freeze/thaw
ALOS PALSAR
topic_facet synthetic aperture radar (SAR)
radar polarimetry
microwave scattering mechanism
permafrost active layer
freeze/thaw
ALOS PALSAR
url https://doi.org/10.3390/rs71215874