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Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions

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Abstract

In order to investigate the validity of buoy-observed sea surface temperature (SST), we installed special instruments to measure near-surface ocean temperature on the TRITON buoy moored at 2.07°N, 138.06°E from 2 to 13 March 2004, in addition to a standard buoy sensor for the regular SST measurement at 1.5-m depth. Large diurnal SST variations were observed during this period, and the variations of the temperatures at about 0.3-m depth could be approximately simulated by a one-dimensional numerical model. However, there was a notable discrepancy between the buoy-observed 1.5-m-depth SST (SST1.5m) and the corresponding model-simulated temperature only during the daytime when the diurnal rise was large. The evaluation of the heat balance in the sea surface layer showed that the diurnal rise of the SST1.5m in these cases could not be accounted for by solar heating alone. We examined the depth of the SST1.5m sensor and the near-surface temperature observed from a ship near the buoy, and came to the conclusion that the solar heating of the buoy hull and/or a disturbance in the temperature field around the buoy hull would contribute to the excessive diurnal rise of the SST1.5m observed with the TRITON buoy. However, the temperature around the hull was not sufficiently homogenized, as suggested in a previous paper. For the diurnal rise of the SST1.5m exceeding 0.5 K, the daytime buoy data became doubtful, through dynamics that remain to be clarified. A simple formula is proposed to correct the unexpected diurnal amplitude of the buoy SST1.5m.

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References

  • Barton, I. J., P. J. Minnett, K. A. Maillet, C. J. Donlon, S. J. Hook, A. T. Jessup and T. J. Nightingale (2004): The Miami2001 infrared radiometer calibration and intercomparison. Part II: Shipboard results. J. Atmos. Oceanic Technol., 21, 268–283.

    Article  Google Scholar 

  • Donlon, C. J., S. J. Keogh, D. J. Baldwin, I. S. Robinson, I. Ridley, T. Sheasby, I. J. Barton, E. F. Bradley, T. J. Nightingale and W. J. Emery (1998): Solid-state radiometer measurements of sea surface skin temperature. J. Atmos. Oceanic Technol., 15, 775–787.

    Article  Google Scholar 

  • Donlon, C. J., T. Nightingale, L. Fiedler, G. Fisher, D. Baldwin and I. S. Robinson (1999): The calibration and intercalibration of sea-going infrared radiometer systems using a low cost blackbody cavity. J. Atmos. Oceanic Technol., 16, 1183–1197.

    Article  Google Scholar 

  • Donlon, C. J., P. J. Minnett, C. Gentemann, T. J. Nightingale, I. J. Barton, B. Ward and M. J. Murray (2002): Toward improved validation of satellite sea surface skin temperature measurements for climate research. J. Climate, 15, 353–369.

    Article  Google Scholar 

  • Fairall, C. W., E. F. Bradley, D. P. Rogers, J. B. Edson and G. S. Young (1996a): Bulk parameterization of air-sea fluxes for tropical ocean-global atmosphere coupled-ocean atmosphere response experiment. J. Geophys. Res., 101, 3747–3764.

    Article  Google Scholar 

  • Fairall, C. W., E. F. Bradley, J. S. Godfrey, G. A. Wick, J. B. Edson and G. S. Young (1996b): Cool-skin and warm-layer effects on sea surface temperature. J. Geophys. Res., 101, 1295–1308.

    Article  Google Scholar 

  • Fairall, C. W., A. B. White, J. B. Edson and J. E. Hare (1997): Integrated shipboard measurements of the marine boundary layer. J. Atmos. Oceanic Technol., 14, 338–359.

    Article  Google Scholar 

  • GHRSST-PP Science Team (2005): The recommended GHRSST-PP data processing specification GDS (Version 1 revision 1.6), report, 245 pp., The GHRSST-PP International Project Office, Exeter, U.K. (available at: https://doi.org/ghrsstpp.jrc.it/documents/GDS-v1.6.zip).

    Google Scholar 

  • Kawai, Y. and H. Kawamura (2000): Study on a platform effect in the in situ sea surface temperature observations under weak wind and clear sky conditions using numerical models. J. Atmos. Oceanic Technol., 17, 185–196.

    Article  Google Scholar 

  • Kawai, Y. and H. Kawamura (2002): Evaluation of the diurnal warming of sea surface temperature using satellite-derived marine meteorological data. J. Oceanogr., 58, 805–814.

    Article  Google Scholar 

  • Kearns, E. J., J. A. Hanafin, R. H. Evans, P. J. Minnett and O. B. Brown (2000): An independent assessment of Pathfinder AVHRR sea surface temperature accuracy using the Marine Atmosphere Emitted Radiance Interferometer (MAERI). Bull. Am. Meteorol. Soc., 81, 1525–1536.

    Article  Google Scholar 

  • Kondo, J., Y. Sasano and T. Ishii (1979): On wind-driven current and temperature profiles with diurnal period in the oceanic planetary boundary layer. J. Phys. Oceanogr., 9, 360–372.

    Article  Google Scholar 

  • Kuroda, Y. (2001): TRITON: Present status and future plan, Japan Marine Science and Technology Center. report, 31 pp., Yokosuka, Japan. On-line document available at: https://doi.org/www.jamstec.go.jp/jamstec/TRITON/future/pdf/Status.pdf

  • Ohlmann, J. C. and D. A. Siegel (2000): Ocean radiant heating. Part II: Parameterizing solar radiation transmission through the upper ocean. J. Phys. Oceanogr., 30, 1849–1865.

    Article  Google Scholar 

  • Price, J. F., R. A. Weller and R. Pinkel (1986): Diurnal cycling: Observations and models of upper ocean response to diurnal heating, cooling, and wind mixing. J. Geophys. Res., 91, 8411–8427.

    Article  Google Scholar 

  • Saunders, P. M. (1967): The temperature at the ocean-air interface. J. Atmos. Sci., 24, 269–273.

    Article  Google Scholar 

  • Schlüessel, P., W. J. Emery, H. Grassl and T. Mammen (1990): On the bulk-skin temperature difference and its impact on satellite remote sensing of sea surface temperature. J. Geophys. Res., 95, 13341–13355.

    Article  Google Scholar 

  • Soloviev, A. V. and R. Lukas (1997): Observation of large diurnal warming events in the near-surface layer of the western equatorial Pacific warm pool. Deep-Sea Res. Part I, 44, 1055–1076.

    Article  Google Scholar 

  • Sui, C.-H., X. Li, K.-M. Lau and D. Adamec (1997): Multiscale air-sea interactions during TOGA COARE. Mon. Wea. Rev., 125, 448–462.

    Article  Google Scholar 

  • Wang, W. and M. J. McPhaden (2001): What is the mean seasonal cycle of surface heat flux in the equatorial Pacific? J. Geophys. Res., 106, 837–857.

    Article  Google Scholar 

  • Wick, G. A., J. C. Ohlmann, C. W. Fairall and A. T. Jessup (2005): Improved oceanic cool skin corrections using a refined solar penetration model. J. Phys. Oceanogr., 35, 1986–1996.

    Article  Google Scholar 

  • Yokoyama, R., S. Tanba and T. Souma (1995): Sea surface effects on the sea surface temperature estimation by remote sensing. Int. J. Remote Sens., 16, 227–238.

    Article  Google Scholar 

  • Zeng, X. and A. Beljaars (2005): A prognostic scheme of sea surface skin temperature for modeling and data assimilation. Geophys. Res. Lett., 32, L14605, doi:10.1029/2005GL023030.

    Article  Google Scholar 

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Correspondence to Yoshimi Kawai.

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Kawai, Y., Kawamura, H., Tanba, S. et al. Validity of sea surface temperature observed with the TRITON buoy under diurnal heating conditions. J Oceanogr 62, 825–838 (2006). https://doi.org/10.1007/s10872-006-0101-3

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  • DOI: https://doi.org/10.1007/s10872-006-0101-3

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