Determination of AATSR Biases Using the OSTIA SST Analysis System and a Matchup Database

J. D. Stark Met Office, Exeter, United Kingdom

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C. Donlon Met Office, Exeter, United Kingdom

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A. O’Carroll Met Office, Exeter, United Kingdom

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G. Corlett Space Research Centre, University of Leicester, Leicester, United Kingdom

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Abstract

Sea surface temperature (SST) analyses are produced on a daily basis at the Met Office using the Operational SST and Sea Ice Analysis (OSTIA) system. OSTIA uses satellite SST data, provided by international agencies via the Global Ocean Data Assimilation Experiment (GODAE) High-Resolution SST Pilot Project (GHRSST-PP) regional/global task sharing (R/GTS) framework, which includes an estimate of bias error (available online at http://www.ghrsst-pp.org). The OSTIA system produces a foundation SST estimate (SSTfnd), which is the SST that is free of diurnal variability, at a resolution of 1/20° (∼6 km). Global coverage outputs are provided each day in GHRSST-PP L4 netCDF format. The verification and intercomparison of the OSTIA analysis, with observations and analyses, has revealed a cold bias of approximately 0.1 K in the OSTIA outputs. Because OSTIA uses the operational 1-km Envisat Advanced Along-Track Scanning Radiometer (AATSR) ATS_NR_2P data [via the GHRSST-PP/European Space Agency (ESA) Medspiration Project, available online at http://www.medspiration.org] as a reference dataset for bias adjustment of other satellite data, the AATSR data were identified as the likely cause of the observed bias. To test this, a series of experiments were carried out in June 2006 using the Medspiration AATSR observations in which the Single Sensor Error Statistics (SSES) bias estimate was assigned fixed magnitudes of 0.0, 0.05, 0.15, and 0.2 K. The authors find that the AATSR data have approximately zero bias relative to in situ buoys. Because AATSR measures the SST skin temperature (SSTskin) and was given a mean global SSTskin deviation of −0.17 K (based on in situ radiometer data), this result suggests that ATS_NR_2P SSTskin data have a warm bias of 0.17 K. Using a matchup database of near-contemporaneous 10 arc min AATSR and in situ data, the authors find that the AATSR SSTskin dual- and triple-window retrievals have a warm bias of 0.14 and 0.17 K, respectively, between August 2002 and July 2006. The results of the experiments confirm that the current Medspiration SSES bias correction provided with the Medspiration AATSR L2P observations is poorly specified. The database was not configured to test the relationship between the cloud proximity confidence value and the AATSR bias error. Based on the matchup database and reanalysis results, the authors suggest that Medspiration be modified to use an SSES bias estimate of 0.17 K for all category 2–6 proximity confidence values for the current AATSR dual-view SST ATS_NR_2P products to provide a correct SSTskin estimate. In response to the results presented in this study, operational changes have been made to the Medspiration processing, which improve the bias estimates provided in the AATSR data. The authors suggest that a concerted effort be invested to develop the most appropriate SSES for the AATSR class of sensors that have specific characteristics that must be included in the SSES estimation scheme. The main elements of such a scheme are presented in this paper.

Corresponding author address: John Stark, Met Office, FitzRoy Road, Exeter, Devon EX1 3PB, United Kingdom. Email: john.stark@metoffice.gov.uk

Abstract

Sea surface temperature (SST) analyses are produced on a daily basis at the Met Office using the Operational SST and Sea Ice Analysis (OSTIA) system. OSTIA uses satellite SST data, provided by international agencies via the Global Ocean Data Assimilation Experiment (GODAE) High-Resolution SST Pilot Project (GHRSST-PP) regional/global task sharing (R/GTS) framework, which includes an estimate of bias error (available online at http://www.ghrsst-pp.org). The OSTIA system produces a foundation SST estimate (SSTfnd), which is the SST that is free of diurnal variability, at a resolution of 1/20° (∼6 km). Global coverage outputs are provided each day in GHRSST-PP L4 netCDF format. The verification and intercomparison of the OSTIA analysis, with observations and analyses, has revealed a cold bias of approximately 0.1 K in the OSTIA outputs. Because OSTIA uses the operational 1-km Envisat Advanced Along-Track Scanning Radiometer (AATSR) ATS_NR_2P data [via the GHRSST-PP/European Space Agency (ESA) Medspiration Project, available online at http://www.medspiration.org] as a reference dataset for bias adjustment of other satellite data, the AATSR data were identified as the likely cause of the observed bias. To test this, a series of experiments were carried out in June 2006 using the Medspiration AATSR observations in which the Single Sensor Error Statistics (SSES) bias estimate was assigned fixed magnitudes of 0.0, 0.05, 0.15, and 0.2 K. The authors find that the AATSR data have approximately zero bias relative to in situ buoys. Because AATSR measures the SST skin temperature (SSTskin) and was given a mean global SSTskin deviation of −0.17 K (based on in situ radiometer data), this result suggests that ATS_NR_2P SSTskin data have a warm bias of 0.17 K. Using a matchup database of near-contemporaneous 10 arc min AATSR and in situ data, the authors find that the AATSR SSTskin dual- and triple-window retrievals have a warm bias of 0.14 and 0.17 K, respectively, between August 2002 and July 2006. The results of the experiments confirm that the current Medspiration SSES bias correction provided with the Medspiration AATSR L2P observations is poorly specified. The database was not configured to test the relationship between the cloud proximity confidence value and the AATSR bias error. Based on the matchup database and reanalysis results, the authors suggest that Medspiration be modified to use an SSES bias estimate of 0.17 K for all category 2–6 proximity confidence values for the current AATSR dual-view SST ATS_NR_2P products to provide a correct SSTskin estimate. In response to the results presented in this study, operational changes have been made to the Medspiration processing, which improve the bias estimates provided in the AATSR data. The authors suggest that a concerted effort be invested to develop the most appropriate SSES for the AATSR class of sensors that have specific characteristics that must be included in the SSES estimation scheme. The main elements of such a scheme are presented in this paper.

Corresponding author address: John Stark, Met Office, FitzRoy Road, Exeter, Devon EX1 3PB, United Kingdom. Email: john.stark@metoffice.gov.uk

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  • Donlon, C. J., Minnett P. J. , Gentemann C. , Nightingale T. J. , Barton I. J. , Ward B. , and Murray M. J. , 2002: Toward improved validation of satellite sea surface skin temperature measurements for climate research. J. Climate, 15 , 353369.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Donlon, C. J., and Coauthors, 2006: The Global Ocean Data Assimilation Experiment High Resolution Sea Surface Temperature Pilot Project (GHRSST-PP) Data Processing Specification version 1.7 (GDSv1.7). GODAE, 270 pp.

  • International Global Ocean Data Assimilation Experiment Steering Team, 2001: The Global Ocean Data Assimilation Experiment: Strategic Plan. GODAE Rep. 6, 23 pp.

  • Lorenc, A. C., Bell R. S. , and Macpherson B. , 1991: The Meteorological Office analysis correction data assimilation scheme. Quart. J. Roy. Meteor. Soc., 117 , 5989.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Martin, M., Hines A. , and Bell M. , 2007: Data assimilation in the FOAM operational short-range ocean forecasting system: A description of the scheme and its impact. Quart. J. Roy. Meteor. Soc., 133 , 981995.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Merchant, C. J., Harris A. R. , Maturi E. , and Maccallum S. , 2005: Probabilistic physically based cloud screening of satellite infrared imagery for operational sea surface temperature retrieval. Quart. J. Roy. Meteor. Soc., 131 , 27352755.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Merchant, C. J., and Coauthors, 2008: Deriving a sea surface temperature record suitable for climate change research from the along-track scanning radiometers. Adv. Space Res., 41 , 111.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Noyes, E. J., Minnett P. J. , Remedios J. J. , Corlett G. K. , Good S. A. , and Llewellyn-Jones D. T. , 2006: The accuracy of AATSR sea surface temperatures in the Caribbean. Remote Sens. Environ., 101 , 3851.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • O’Carroll, A. G., Eyre J. R. , and Saunders R. W. , 2008: Three-way error analysis between AATSR, AMSR-E, and in situ sea surface temperature observations. J. Atmos. Oceanic Technol., 25 , 11971207.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • O’Carroll, A. G., Watts J. G. , Horrocks L. A. , Saunders R. W. , and Rayner N. A. , 2006: Validation of the AATSR Meteo product sea surface temperature. J. Atmos. Oceanic Technol., 23 , 711726.

    • Crossref
    • Search Google Scholar
    • Export Citation
  • Rayner, N., Parker D. , Horton E. , Folland C. , Alexander L. , Rowell D. , Kent E. , and Kaplan A. , 2003: Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J. Geophys. Res., 108 .4407, doi:10.1029/2002JD002670.

    • Search Google Scholar
    • Export Citation
  • Saunders, P. M., 1967: The temperature at the ocean-air interface. J. Atmos. Sci., 24 , 269273.

  • Stark, J. D., Donlon C. J. , Martin M. J. , and McCulloch M. E. , 2007: OSTIA: An operational, high resolution, real time, global sea surface temperature analysis system. Proc., Oceans 2007, Marine Challenges: Coastline to Deep Sea, Aberdeen, Scotland, IEEE/OES, 1–4.

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    • Export Citation
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