First-year sea ice melt pond fraction estimation from dual-polarisation C-band SAR – Part 2: Scaling in situ to Radarsat-2

Sea ice melt pond fraction ( f p ), linked with lower sea ice surface albedo and increased light transmittance to the ocean, is inadequately parameterised in sea ice models due to a lack of observations. In this paper, results from a multi-scale remote-sensing program dedicated to the retrieval of l...

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Published in:The Cryosphere
Main Authors: R. K. Scharien, K. Hochheim, J. Landy, D. G. Barber
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2014
Subjects:
Online Access:https://doi.org/10.5194/tc-8-2163-2014
https://doaj.org/article/fbd2d1fa445a47f0ae2c463f6b799eda
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spelling ftdoajarticles:oai:doaj.org/article:fbd2d1fa445a47f0ae2c463f6b799eda 2023-05-15T18:17:16+02:00 First-year sea ice melt pond fraction estimation from dual-polarisation C-band SAR – Part 2: Scaling in situ to Radarsat-2 R. K. Scharien K. Hochheim J. Landy D. G. Barber 2014-11-01T00:00:00Z https://doi.org/10.5194/tc-8-2163-2014 https://doaj.org/article/fbd2d1fa445a47f0ae2c463f6b799eda EN eng Copernicus Publications http://www.the-cryosphere.net/8/2163/2014/tc-8-2163-2014.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 1994-0416 1994-0424 doi:10.5194/tc-8-2163-2014 https://doaj.org/article/fbd2d1fa445a47f0ae2c463f6b799eda The Cryosphere, Vol 8, Iss 6, Pp 2163-2176 (2014) Environmental sciences GE1-350 Geology QE1-996.5 article 2014 ftdoajarticles https://doi.org/10.5194/tc-8-2163-2014 2022-12-31T00:27:37Z Sea ice melt pond fraction ( f p ), linked with lower sea ice surface albedo and increased light transmittance to the ocean, is inadequately parameterised in sea ice models due to a lack of observations. In this paper, results from a multi-scale remote-sensing program dedicated to the retrieval of level first-year sea ice (FYI) f p from dual co- and cross-polarisation C-band synthetic aperture radar (SAR) backscatter are detailed. Models which utilise the dominant effect of free-water melt ponds on the VV / HH (vertical transmit and vertical receive / horizontal transmit and horizontal receive) polarisation ratio at high incidence angles are tested for their ability to provide estimates of the subscale f p . Retrieved f p from noise-corrected Radarsat-2 quad-polarisation scenes are in good agreement with observations from coincident aerial survey data, with root mean square errors (RMSEs) of 0.05–0.07 obtained during intermediate and late stages of ponding. Weak model performance is attributed to the presence of wet snow and slush during initial ponding, and a synoptically driven freezing event causing ice lids to form on ponds. The HV / HH (horizontal transmit and vertical receive / horizontal transmit and horizontal receive) ratio explains a greater portion of variability in f p , compared to VV / HH, when ice lids are present. Generally low HV channel intensity suggests limited applications using dual cross-polarisation data, except with systems that have exceptionally low noise floors. Results demonstrate the overall potential of dual-polarisation SAR for standalone or complementary observations of f p for process-scale studies and improvements to model parameterisations. Article in Journal/Newspaper Sea ice The Cryosphere Directory of Open Access Journals: DOAJ Articles The Cryosphere 8 6 2163 2176
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
R. K. Scharien
K. Hochheim
J. Landy
D. G. Barber
First-year sea ice melt pond fraction estimation from dual-polarisation C-band SAR – Part 2: Scaling in situ to Radarsat-2
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description Sea ice melt pond fraction ( f p ), linked with lower sea ice surface albedo and increased light transmittance to the ocean, is inadequately parameterised in sea ice models due to a lack of observations. In this paper, results from a multi-scale remote-sensing program dedicated to the retrieval of level first-year sea ice (FYI) f p from dual co- and cross-polarisation C-band synthetic aperture radar (SAR) backscatter are detailed. Models which utilise the dominant effect of free-water melt ponds on the VV / HH (vertical transmit and vertical receive / horizontal transmit and horizontal receive) polarisation ratio at high incidence angles are tested for their ability to provide estimates of the subscale f p . Retrieved f p from noise-corrected Radarsat-2 quad-polarisation scenes are in good agreement with observations from coincident aerial survey data, with root mean square errors (RMSEs) of 0.05–0.07 obtained during intermediate and late stages of ponding. Weak model performance is attributed to the presence of wet snow and slush during initial ponding, and a synoptically driven freezing event causing ice lids to form on ponds. The HV / HH (horizontal transmit and vertical receive / horizontal transmit and horizontal receive) ratio explains a greater portion of variability in f p , compared to VV / HH, when ice lids are present. Generally low HV channel intensity suggests limited applications using dual cross-polarisation data, except with systems that have exceptionally low noise floors. Results demonstrate the overall potential of dual-polarisation SAR for standalone or complementary observations of f p for process-scale studies and improvements to model parameterisations.
format Article in Journal/Newspaper
author R. K. Scharien
K. Hochheim
J. Landy
D. G. Barber
author_facet R. K. Scharien
K. Hochheim
J. Landy
D. G. Barber
author_sort R. K. Scharien
title First-year sea ice melt pond fraction estimation from dual-polarisation C-band SAR – Part 2: Scaling in situ to Radarsat-2
title_short First-year sea ice melt pond fraction estimation from dual-polarisation C-band SAR – Part 2: Scaling in situ to Radarsat-2
title_full First-year sea ice melt pond fraction estimation from dual-polarisation C-band SAR – Part 2: Scaling in situ to Radarsat-2
title_fullStr First-year sea ice melt pond fraction estimation from dual-polarisation C-band SAR – Part 2: Scaling in situ to Radarsat-2
title_full_unstemmed First-year sea ice melt pond fraction estimation from dual-polarisation C-band SAR – Part 2: Scaling in situ to Radarsat-2
title_sort first-year sea ice melt pond fraction estimation from dual-polarisation c-band sar – part 2: scaling in situ to radarsat-2
publisher Copernicus Publications
publishDate 2014
url https://doi.org/10.5194/tc-8-2163-2014
https://doaj.org/article/fbd2d1fa445a47f0ae2c463f6b799eda
genre Sea ice
The Cryosphere
genre_facet Sea ice
The Cryosphere
op_source The Cryosphere, Vol 8, Iss 6, Pp 2163-2176 (2014)
op_relation http://www.the-cryosphere.net/8/2163/2014/tc-8-2163-2014.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
1994-0416
1994-0424
doi:10.5194/tc-8-2163-2014
https://doaj.org/article/fbd2d1fa445a47f0ae2c463f6b799eda
op_doi https://doi.org/10.5194/tc-8-2163-2014
container_title The Cryosphere
container_volume 8
container_issue 6
container_start_page 2163
op_container_end_page 2176
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