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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Main Author: Sang-Eun Park
Format: Article
Language:English
Published: MDPI AG 2015-12-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/7/12/15874
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spelling doaj-aa6e5b37f6514679b7940655dc305a032020-11-24T22:52:05ZengMDPI AGRemote Sensing2072-42922015-12-01712171351714810.3390/rs71215874rs71215874Variations of Microwave Scattering Properties by Seasonal Freeze/Thaw Transition in the Permafrost Active Layer Observed by ALOS PALSAR Polarimetric DataSang-Eun Park0Department of Geoinformation Engineering, Sejong University, 209 Neungdong-ro, Gwangjin-gu, Seoul 143-747, KoreaRadar 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.http://www.mdpi.com/2072-4292/7/12/15874synthetic aperture radar (SAR)radar polarimetrymicrowave scattering mechanismpermafrost active layerfreeze/thawALOS PALSAR
collection DOAJ
language English
format Article
sources DOAJ
author Sang-Eun Park
spellingShingle Sang-Eun Park
Variations of Microwave Scattering Properties by Seasonal Freeze/Thaw Transition in the Permafrost Active Layer Observed by ALOS PALSAR Polarimetric Data
Remote Sensing
synthetic aperture radar (SAR)
radar polarimetry
microwave scattering mechanism
permafrost active layer
freeze/thaw
ALOS PALSAR
author_facet Sang-Eun Park
author_sort Sang-Eun Park
title 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_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_sort variations of microwave scattering properties by seasonal freeze/thaw transition in the permafrost active layer observed by alos palsar polarimetric data
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2015-12-01
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.
topic synthetic aperture radar (SAR)
radar polarimetry
microwave scattering mechanism
permafrost active layer
freeze/thaw
ALOS PALSAR
url http://www.mdpi.com/2072-4292/7/12/15874
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