Transport at the Air-Sea Interface: Measurements, Models and by Christoph S. Garbe, Robert A. Handler, Bernd Jähne
By Christoph S. Garbe, Robert A. Handler, Bernd Jähne
One key uncertainty in predictions of destiny weather is as a result of the inability of data of shipping strategies within the air-water interface; this poses the most move resistance among oceans and surroundings. This e-book reports fresh development within the domain names of experimental approach reviews in addition to machine stimulation. It represents an early technique of merging insights received in either fields and broadens our figuring out of air-water fuel and warmth exchange.
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Additional info for Transport at the Air-Sea Interface: Measurements, Models and Parametrizations (Environmental Science and Engineering Environmental Science)
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B. H. Brumley and G. H. Jirka. Near-surface turbulence in a grid-stirred tank. J. , (183):236–263, 1987. C. R. Chu and G. H. Jirka. Turbulent gas flux measurements below the air-water interface of a grid-stirred tank. Intl J. Heat Mass Transfer, 35(8):1957–1968, 1992. P. V. Danckwerts. Significance of liquid-film coefficients in gas absorption. , 43:1460–1467, 1951. J. S. Gulliver and M. J. Halverson. Air-water gas transfer in open channels. Water Resources Research, 25(8):1783–1793, 1989. Herlina. Gas transfer at the air-water interface in a turbulent flow environment.
3 cm/s [22]. The levels of turbulence generated in this study spanned both low and high turbulence flow regimes suggested by Theofanus [24] so that a sufficiently wide spectrum of turbulent eddies could be investigated. 5 shows a flow sequence of 12 instantaneous velocity and concentration fields for a near-interface image area of 8 × 12 mm. The light and dark colors indicate the regions with low and high dissolved oxygen concentration, respectively. In all images, a very thin dark layer, immediately below the interface, indicating the boundary layer in which the oxygen concentration decreases rapidly from saturated to the bulk concentration can be observed.
3 cm hr−1 [40]. However, several other works reach different conclusions. The estimate of Krakauer et al. [22] provides a global gas transfer velocity indistinguishable from the original while that of Naegler et al. 3). In Krakauer et al. [22] regional specific gas transfer rates were obtained. While only small regional differences in wind and gas transfer were observed, the functional dependence of gas transfer was nearly linear, contrary to other recent work that, a priori, assumed a quadratic dependence [31, 37].