A wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over Antarctica (2000–2009)

Melting is mapped over Antarctica at a high spatial resolution using a novel melt detection algorithm based on wavelets and multiscale analysis. The method is applied to Ku-band (13.4 GHz) normalized backscattering measured by SeaWinds onboard the satellite QuikSCAT and spatially enhanced on a 5 km...

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Published in:The Cryosphere
Main Authors: Steiner, N., Tedesco, M.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-8-25-2014
https://tc.copernicus.org/articles/8/25/2014/
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spelling ftcopernicus:oai:publications.copernicus.org:tc20335 2023-05-15T13:54:27+02:00 A wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over Antarctica (2000–2009) Steiner, N. Tedesco, M. 2018-09-27 application/pdf https://doi.org/10.5194/tc-8-25-2014 https://tc.copernicus.org/articles/8/25/2014/ eng eng doi:10.5194/tc-8-25-2014 https://tc.copernicus.org/articles/8/25/2014/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-8-25-2014 2020-07-20T16:25:12Z Melting is mapped over Antarctica at a high spatial resolution using a novel melt detection algorithm based on wavelets and multiscale analysis. The method is applied to Ku-band (13.4 GHz) normalized backscattering measured by SeaWinds onboard the satellite QuikSCAT and spatially enhanced on a 5 km grid over the operational life of the sensor (1999–2009). Wavelet-based estimates of melt spatial extent and duration are compared with those obtained by means of threshold-based detection methods, where melting is detected when the measured backscattering is 3 dB below the preceding winter mean value. Results from both methods are assessed by means of automatic weather station (AWS) air surface temperature records. The yearly melting index, the product of melted area and melting duration, found using a fixed threshold and wavelet-based melt algorithm are found to have a relative difference within 7% for all years. Most of the difference between melting records determined from QuikSCAT is related to short-duration backscatter changes identified as melting using the threshold methodology but not the wavelet-based method. The ability to classify melting based on relative persistence is a critical aspect of the wavelet-based algorithm. Compared with AWS air-temperature records, both methods show a relative agreement to within 10% based on estimated melt conditions, although the fixed threshold generally finds a greater agreement with AWS. Melting maps obtained with the wavelet-based approach are also compared with those obtained from spaceborne brightness temperatures recorded by the Special Sensor Microwave/Image (SSM/I). With respect to passive microwave records, we find a higher degree of agreement (9% relative difference) for the melting index using the wavelet-based approach than threshold-based methods (11% relative difference). Text Antarc* Antarctica Copernicus Publications: E-Journals The Cryosphere 8 1 25 40
institution Open Polar
collection Copernicus Publications: E-Journals
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language English
description Melting is mapped over Antarctica at a high spatial resolution using a novel melt detection algorithm based on wavelets and multiscale analysis. The method is applied to Ku-band (13.4 GHz) normalized backscattering measured by SeaWinds onboard the satellite QuikSCAT and spatially enhanced on a 5 km grid over the operational life of the sensor (1999–2009). Wavelet-based estimates of melt spatial extent and duration are compared with those obtained by means of threshold-based detection methods, where melting is detected when the measured backscattering is 3 dB below the preceding winter mean value. Results from both methods are assessed by means of automatic weather station (AWS) air surface temperature records. The yearly melting index, the product of melted area and melting duration, found using a fixed threshold and wavelet-based melt algorithm are found to have a relative difference within 7% for all years. Most of the difference between melting records determined from QuikSCAT is related to short-duration backscatter changes identified as melting using the threshold methodology but not the wavelet-based method. The ability to classify melting based on relative persistence is a critical aspect of the wavelet-based algorithm. Compared with AWS air-temperature records, both methods show a relative agreement to within 10% based on estimated melt conditions, although the fixed threshold generally finds a greater agreement with AWS. Melting maps obtained with the wavelet-based approach are also compared with those obtained from spaceborne brightness temperatures recorded by the Special Sensor Microwave/Image (SSM/I). With respect to passive microwave records, we find a higher degree of agreement (9% relative difference) for the melting index using the wavelet-based approach than threshold-based methods (11% relative difference).
format Text
author Steiner, N.
Tedesco, M.
spellingShingle Steiner, N.
Tedesco, M.
A wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over Antarctica (2000–2009)
author_facet Steiner, N.
Tedesco, M.
author_sort Steiner, N.
title A wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over Antarctica (2000–2009)
title_short A wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over Antarctica (2000–2009)
title_full A wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over Antarctica (2000–2009)
title_fullStr A wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over Antarctica (2000–2009)
title_full_unstemmed A wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over Antarctica (2000–2009)
title_sort wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over antarctica (2000–2009)
publishDate 2018
url https://doi.org/10.5194/tc-8-25-2014
https://tc.copernicus.org/articles/8/25/2014/
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-8-25-2014
https://tc.copernicus.org/articles/8/25/2014/
op_doi https://doi.org/10.5194/tc-8-25-2014
container_title The Cryosphere
container_volume 8
container_issue 1
container_start_page 25
op_container_end_page 40
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