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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Main Authors: N. Steiner, M. Tedesco
Format: Article
Language:English
Published: Copernicus Publications 2014-01-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/8/25/2014/tc-8-25-2014.pdf
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spelling doaj-01426c56772145ce884c3556e23684ac2020-11-24T23:51:51ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242014-01-0181254010.5194/tc-8-25-2014A wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over Antarctica (2000–2009)N. Steiner0M. Tedesco1The City College of New York at the City University of New York, New York, USAThe City College of New York at the City University of New York, New York, USAMelting 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).http://www.the-cryosphere.net/8/25/2014/tc-8-25-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author N. Steiner
M. Tedesco
spellingShingle N. Steiner
M. Tedesco
A wavelet melt detection algorithm applied to enhanced-resolution scatterometer data over Antarctica (2000–2009)
The Cryosphere
author_facet N. Steiner
M. Tedesco
author_sort N. Steiner
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)
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2014-01-01
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).
url http://www.the-cryosphere.net/8/25/2014/tc-8-25-2014.pdf
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