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Parameters of the Rossby Similarity Law for the Sensible Heat and Vapor Fluxes in the Planetary Boundary Layer over the Ocean

With the radiosonde data obtained over the ocean in AMTEX, the parameters C and D of the Rossby similarity law in the planetary boundary layer are evaluated. The height of the planetary boundary layer, h, is assumed to be 0.3 u*/1 f I and concerning the profiles of temperature and humidity the laminar sub-layer above the sea surface is taken into account. The parameter C evaluated takes a large value in plus and minus signs for the unstable and the stable conditions, respectively, near the neutral conditions. This result seems to disagree with the previous results in which the value of C changes gradually in the near-neutral conditions. However, if examined in detail it is understood that our result is quite reasonable and does not contradict them. The values of sensible heat and vapor fluxes calculated by the Rossby similarity law with the empirical equations obtained in the present work are very well consistent with those by the bulk method.