caa a22 4500 475777670 CHVBK 20180406123635.0 cr unu---uuuuu 170329e20000501xx s 000 0 eng 10.1023/A:1002623712237 doi (NATIONALLICENCE)springer-10.1023/A:1002623712237 Aircraft Observations Of The Mean And Turbulent Structure Of A Shallow Boundary Layer Over The Persian Gulf [Elektronische Daten] [Ian Brooks, David Rogers] Stable internal boundary layers form when warm air isadvected over a cooler surface, a common occurrence incoastal areas. The internal boundary layer deepenswith distance along-wind, eventually reachingequilibrium with the surface and becoming a fullydeveloped marine boundary layer. We presentobservations of the late stages of internalboundary-layer evolution made bythe U.K. Meteorological Office'sC-130 Hercules research aircraft over the Persian Gulfin April 1996. Northwesterly winds brought warm dryair from the surrounding desert landmass across thecooler waters of the Gulf. Loss of heat to the surfaceresulted in the formation of a shallow, stableinternal boundary layer downwind of the coast. The aircraftmeasurements were made several hundred kilometresdownwind, by which point the original deep convectiveboundary layer had been eroded away and the internalboundary layer was well developed, effectively a newmarine atmospheric boundary layer. Throughout most ofits depth the boundary layer was statically stable anda downward heat flux of approximately 15 W m-2was observed; however, an exceptionally strong latentheat flux, in excess of 250 W m-2 near thesurface, was sufficient to overcome the downwards heatflux and maintain weak buoyant convection in the lower30-50% of the boundary layer. Scaling of boundary-layer turbulence statistics usinglocal similarity theory produces results in agreementwith previous studies. Because of the strong humiditycontribution to the buoyancy flux, however, care isrequired with the definition of the similarity scales.It is usual for either the sensible heat or buoyancyflux to be used in the definitions of both thetemperature and length scales; the latter being usedover water where humidity plays a significant role indetermining stability. In the present case we findthat while the buoyancy flux is appropriate in thedefinition of the length scale, the temperature scalemust be defined in terms of the sensible heat flux. Kluwer Academic Publishers, 2000 Internal boundary layer nationallicence Local similarity nationallicence Brooks Ian Scripps Institution of Oceanography, La Jolla, California, U.S.A. aut Rogers David Scripps Institution of Oceanography, La Jolla, California, U.S.A. aut Boundary-Layer Meteorology Kluwer Academic Publishers 95/2(2000-05-01), 189-210 0006-8314 95:2<189 2000 95 10546 https://doi.org/10.1023/A:1002623712237 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1023/A:1002623712237 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Brooks Ian Scripps Institution of Oceanography, La Jolla, California, U.S.A aut NATIONALLICENCE 700 1- Rogers David Scripps Institution of Oceanography, La Jolla, California, U.S.A aut NATIONALLICENCE 773 0- Boundary-Layer Meteorology Kluwer Academic Publishers 95/2(2000-05-01), 189-210 0006-8314 95:2<189 2000 95 10546 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer