Evolution of stable internal boundary layers over a cold sea

The situation studied in this paper relates to air flow from a heated land surface out over a water surface with much lower temperature. Observations from the Baltic Sea, where this kind of situation prevails for two thirds of the time, indicate that several distinct flow regimes occur. Simulations...

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Bibliographic Details
Published in:Journal of Geophysical Research, Washington, DC Washington, DC, 1997-01, Vol.102 (C1), p.1091-1099
Main Authors: Smedman, Ann‐Sofi, Bergström, Hans, Grisogono, Branko
Format: Article
Language:English
Subjects:
Earth, ocean, space
Exact sciences and technology
External geophysics
Marine
Physics of the oceans
Sea-air exchange processes
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Summary:The situation studied in this paper relates to air flow from a heated land surface out over a water surface with much lower temperature. Observations from the Baltic Sea, where this kind of situation prevails for two thirds of the time, indicate that several distinct flow regimes occur. Simulations with a numerical boundary layer model for various combinations of geostrophic wind speed, Vg, and bulk temperature difference between land and sea, ΔΘ, have been performed. They show that, initially, stratification is always stable in the air layers near the sea surface but after some time transition to a near‐neutral layer capped by an inversion takes place. The simulations, as well as the results of a simple analytical study, indicate that the transition takes place at a certain time of over water transport, te, which can be calculated when the bulk parameter ΔΘ is known. Measurements of boundary layer temperature and wind profiles at three sites in the Baltic Sea area strongly support this result. Thus, for measurements representing traveling times less than te, derived with the above mentioned expression, a stable boundary layer is always found. For traveling times larger than te, a mixed layer is found (provided ΔΘ is not large enough to cause quasi‐frictional decoupling). Turbulence measurements made at the three sites simultaneously with the profiles show that (u*/Vg)103 is between almost zero and 25 for the stable cases and between 25 and 46 for the mixed layer cases.
ISSN:0148-0227
2169-9275
2156-2202
2169-9291
DOI:10.1029/96JC02782