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By Bardos C. (ed.), Lasry J.M. (ed.), Schatzman M. (ed.)

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There is some evidence that such continental effects on nucleus concentration at sea are far reaching. Hess (1948, 1951) found the following distinct differences between the mean concentrations of Aitken nuclei in the western and the eastern parts of the North Atlantic Ocean: Year 1948 1948 1951 1951 Western part Eastern part (nuclei per cm-) 575 813 1512 1229 478 504 462 887 Similar results have been reported by Ohta (1951) for the Pacific Ocean (see Table IV). The authors attribute the higher concentration in the western parts of the oceans to continental influences which affect the air masses traveling in general from west to east.

This error is particularly large with very small nuclei. With regard to possible errors caused by coalescence or shattering of nuclei upon impact, Woodcock and Gifford (1949) were able to show that these were not significant, even at very high air speed. 2 Size Distribution. The sea-salt nuclei produced at the sea surface are raised to higher levels by turbulence and convection until this vertical transport is hindered or limited at the top of an inversion layer. In the following we shall try to present some information on the size distributions existing in different layers and regions of the marine atmosphere.

18°C roughly corresponds to the mean increase of the intake temperature caused by the heating originating from the ship. This value will, of course, depend on the ship concerned and vary according to circumstances. 9°C. On the other hand, investigations carried out by Arnot (1955) and Benditskii (1958) have shown that the heating effect seems to be less serious under different conditions. In addition, results of a comparison reported by Kirk and Gordon (1952) indicated that the transfer of heat from the engine room to the intake pipe is smaller while the ship is under way than the value obtained while the ship is on station.

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Bifurcation and Nonlinear Eigenvalue Problems: Proceedings by Bardos C. (ed.), Lasry J.M. (ed.), Schatzman M. (ed.)


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