Matchup Characteristics of Sea Surface Salinity Using a High-Resolution Ocean Model

Sea surface salinity (SSS) satellite measurements are validated using in situ observations usually made by surfacing Argo floats. Validation statistics are computed using matched values of SSS from satellites and floats. This study explores how the matchup process is done using a high-resolution num...

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Main Authors: Frederick M. Bingham, Severine Fournier, Susannah Brodnitz, Karly Ulfsax, Hong Zhang
Format: Article
Language:English
Published: MDPI AG 2021-07-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/13/15/2995
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spelling doaj-df15d82e225f49b0a05a0b8f7e47366f2021-08-06T15:30:45ZengMDPI AGRemote Sensing2072-42922021-07-01132995299510.3390/rs13152995Matchup Characteristics of Sea Surface Salinity Using a High-Resolution Ocean ModelFrederick M. Bingham0Severine Fournier1Susannah Brodnitz2Karly Ulfsax3Hong Zhang4Center for Marine Science, University of North Carolina Wilmington, Wilmington, NC 28403, USAJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USACenter for Marine Science, University of North Carolina Wilmington, Wilmington, NC 28403, USACenter for Marine Science, University of North Carolina Wilmington, Wilmington, NC 28403, USAJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USASea surface salinity (SSS) satellite measurements are validated using in situ observations usually made by surfacing Argo floats. Validation statistics are computed using matched values of SSS from satellites and floats. This study explores how the matchup process is done using a high-resolution numerical ocean model, the MITgcm. One year of model output is sampled as if the Aquarius and Soil Moisture Active Passive (SMAP) satellites flew over it and Argo floats popped up into it. Statistical measures of mismatch between satellite and float are computed, RMS difference (RMSD) and bias. The bias is small, less than 0.002 in absolute value, but negative with float values being greater than satellites. RMSD is computed using an “all salinity difference” method that averages level 2 satellite observations within a given time and space window for comparison with Argo floats. RMSD values range from 0.08 to 0.18 depending on the space–time window and the satellite. This range gives an estimate of the representation error inherent in comparing single point Argo floats to area-average satellite values. The study has implications for future SSS satellite missions and the need to specify how errors are computed to gauge the total accuracy of retrieved SSS values.https://www.mdpi.com/2072-4292/13/15/2995surface salinityocean modelingrepresentation errorsatellite validationmatchups
collection DOAJ
language English
format Article
sources DOAJ
author Frederick M. Bingham
Severine Fournier
Susannah Brodnitz
Karly Ulfsax
Hong Zhang
spellingShingle Frederick M. Bingham
Severine Fournier
Susannah Brodnitz
Karly Ulfsax
Hong Zhang
Matchup Characteristics of Sea Surface Salinity Using a High-Resolution Ocean Model
Remote Sensing
surface salinity
ocean modeling
representation error
satellite validation
matchups
author_facet Frederick M. Bingham
Severine Fournier
Susannah Brodnitz
Karly Ulfsax
Hong Zhang
author_sort Frederick M. Bingham
title Matchup Characteristics of Sea Surface Salinity Using a High-Resolution Ocean Model
title_short Matchup Characteristics of Sea Surface Salinity Using a High-Resolution Ocean Model
title_full Matchup Characteristics of Sea Surface Salinity Using a High-Resolution Ocean Model
title_fullStr Matchup Characteristics of Sea Surface Salinity Using a High-Resolution Ocean Model
title_full_unstemmed Matchup Characteristics of Sea Surface Salinity Using a High-Resolution Ocean Model
title_sort matchup characteristics of sea surface salinity using a high-resolution ocean model
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2021-07-01
description Sea surface salinity (SSS) satellite measurements are validated using in situ observations usually made by surfacing Argo floats. Validation statistics are computed using matched values of SSS from satellites and floats. This study explores how the matchup process is done using a high-resolution numerical ocean model, the MITgcm. One year of model output is sampled as if the Aquarius and Soil Moisture Active Passive (SMAP) satellites flew over it and Argo floats popped up into it. Statistical measures of mismatch between satellite and float are computed, RMS difference (RMSD) and bias. The bias is small, less than 0.002 in absolute value, but negative with float values being greater than satellites. RMSD is computed using an “all salinity difference” method that averages level 2 satellite observations within a given time and space window for comparison with Argo floats. RMSD values range from 0.08 to 0.18 depending on the space–time window and the satellite. This range gives an estimate of the representation error inherent in comparing single point Argo floats to area-average satellite values. The study has implications for future SSS satellite missions and the need to specify how errors are computed to gauge the total accuracy of retrieved SSS values.
topic surface salinity
ocean modeling
representation error
satellite validation
matchups
url https://www.mdpi.com/2072-4292/13/15/2995
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AT susannahbrodnitz matchupcharacteristicsofseasurfacesalinityusingahighresolutionoceanmodel
AT karlyulfsax matchupcharacteristicsofseasurfacesalinityusingahighresolutionoceanmodel
AT hongzhang matchupcharacteristicsofseasurfacesalinityusingahighresolutionoceanmodel
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