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By A. Eliassen, E. Kleinschmidt Jr. (auth.), Julius Bartels (eds.)

45 downwards simply because (j at the usual raises with top; yet this end doesn't keep on with from (18.3) whilst the dependency of Kc upon ~o is considered. s 2 ERTELl and PRIESTLEY and SWINBANK have proven that the upward eddy­ flux of brilliant warmth needs to be greater than indicated by way of (18.3), simply because this formulation doesn't account for the truth that emerging eddies are systematically hotter than sinking eddies due to the influence of buoyancy. The reader is observed the studies by means of SUTTON [22], [23] and PRIESTLEY and SHEP­ PARD [15) for additional info touching on eddy-flux of warmth and turbulent diffusion. 19. RICHARDSON'S criterion. The right-hand facet of (15.10) represents the speed of creation of eddy power. The final time period represents strength loss by way of dissipation; so that the eddy strength might be maintained, it's for this reason worthwhile that P div V" - (! V" v" . grad. v > O.

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