Abstract
A new method deriving surface air temperature from specific humidity is proposed. Surface atmospheric pressure and relative humidity in addition to specific humidity are necessary in order to derive surface air temperature. Assuming effects of variation of atmospheric pressure and relative humidity are small, climatological values are used for those values. Derived surface air temperature is compared with in situ surface air temperature. A cross-correlation coefficient is high and the rms error is small. However, the agreement between them varies spatially. The errors are largest in the eastern equatorial region and high-latitudes. The former may be caused by a large sampling error and remarkable internannual variation related to ENSO phenomena. On the other hand, the latter may be related to sensitivity of saturated vapor curve to air temperature. Sensible heat fluxes are estimated by using derived surface air temperature and compared with that by in situ data. For the whole North Pacific, a cross-correlation coefficient, a mean error and an rms difference are 0.89 W m−2, 0.58 W m−2 and 8.03 W m−2, respectively.
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Abbott, M. R. and D. B. Chelton (1991): Advances in passive remote sensing of the ocean.Rev. Geophys., Supplement, 571–589.
Blanc, T. V. (1985): Variation of bulk-derived surface flux, stability, and roughness results due to the use of different transfer coefficient schemes.J. Phys. Oceanogr.,15, 650–669.
Giese, B. S. and D. R. Cayan (1993): Surface heat flux parameterizations and tropical Pacific sea surface temperature simulations.J. Geophys. Res.,98, 6979–6989.
Hsu, S. A. and B. W. Blanchard (1989): The relationship between total precipitable water and surface-level humidity over the sea surface: A further evaluation.J. Geophys. Res.,94, 14539–14545.
Iwasaka, N. and K. Hanawa (1990): Climatologies of marine meteorological variables and surface fluxes in the North Pacific computed from COADS.Tohoku Geophys. J.,33, 185–239.
Kondo, J. (1975): Air-sea bulk transfer coefficients in diabatic conditions.Bound-Layer Meteor.,9, 91–112.
Kubota, M. (1994): A mechanism for the accumulation of floating marine debris north of Hawaii.J. Phys. Oceanogr.,24, 1059–1064.
Kubota, M. and A. Shikauchi (1994): Sensible and latent heat flux in the North Pacific using satellite data.Proceedings of PORSEC-94, 55–60.
Liu, W. T. (1986): Statistical relation between monthly mean precipitable water and surface level humidity over global oceans.Mon. Wea. Rev. 114, 1591–1602.
Liu, W. T., K. B. Katsaros and J. A. Businger (1979): Bulk parameterization of air-sea exchanges of heat and water vapor including the molecular constraints at the interface.J. Atmos. Sci.,36, 1722–1735.
Liu, W. T., W. Tang and P. P. Niiler (1991): Humidity profiles over the ocean.J. Climate,4, 1023–1034.
Owen, P. R. and W. R. Thomson (1963): Heat transfer across rough surfaces.J. Fluid Mech.,15, 321–334.
Shikauchi, A. (1994): Estimate of latent and sensible heat fluxes over the North Pacific by using satellite data. Master's Thesis, Tokai University, 107 pp. (in Japanese).
Slutz, R. J., S. J. Lubker, J. D. Hiscox, S. D. Woodruff, R. L. Jenne, D. H. Joseph, P. M. Steurer and J. D. Elms (1985): Comprehensive Ocean-Atmosphere Data Set; Release 1, NOAA Environmental Research Laboratories, Climate Research Program, Boulder, CO, 268 pp. (NTIS PB86-105723).
Thadathil, P., A. Shikauchi, Y. Sugimori and M. Kubota (1993): A statistical method to get surface level air-temperature from satellite observations of precipitable water.J. Oceanogr.,49, 551–558.
Weare, B. C. (1989): Uncertainties in estimates of surface heat fluxes derived from marine reports over the tropical and subtropical oceans.Tellus,41A, 357–370.
Woodruff, S. D., R. J. Slutz, R. L. Jenne and P. M. Steurer (1987): A comprehensive ocean-atmosphere data set.Bull. Amer. Meteor. Soc.,68, 1239–1250.
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Kubota, M., Shikauchi, A. Air temperature at ocean surface derived from surface-level humidity. J Oceanogr 51, 619–634 (1995). https://doi.org/10.1007/BF02235456
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DOI: https://doi.org/10.1007/BF02235456