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Figure 4 shows time-height cross sections of area-mean θ ′ w ′ ¯ and q ′ w ′ ¯ in cases A02 to A20.

Figure 4 Time-height cross sections of area-mean θ ′ w ′ ¯ (upper panels) and q ′ w ′ ¯ (lower panels).

Time-height cross sections of area-mean θ ′ w ′ ¯ for cases B1, B3, and B5 are shown in the upper panels of Figure 8.

Figure 9 shows time-height cross sections of area-mean u ′ w ′ ¯ for UZ values of 0 and 3 m · s 1 · km 1.

Figure 13 Time-height cross sections of area-mean θ ′ w ′ ¯ (left panels), q ′ w ′ ¯ (middle panels), and u ′ w ′ ¯ (right panels).

Figure 5 Time-height cross sections of area-mean u ′ w ′ ¯ in U Z  = 0 and 3 (m · s -1  · km -1 ; upper and lower panels, respectively).

The eddy momentum flux is sensitive to the initial vertical shear of zonal flow UZ. Figure 5 shows time-height cross sections of area-mean u ′ w ′ ¯ for UZ values 0 and 3 m · s-1 · km-1.

The domain area is 16 times larger than in sections 'Convective adjustment in unstable layer (case A)' and 'Microscale eddies induced by turbulent thermal flux (case B)'. Figure 13 shows time-height cross sections of area-mean θ ′ w ′ ¯, q ′ w ′ ¯, and u ′ w ′ ¯ for large-domain experiments of cases A10 and B3 under the condition U Z  = 0 m · s 1 · km 1.

Such strong wind shear forms via convective adjustment (Figure 5) and turbulent mixing (Figure 9). Figure 9 Time-height cross sections of area-mean u ′ w ′ ¯ in U Z  = 0 and 3 (m · s -1  · km -1 ; upper and lower panels, respectively).

For this optimum value of flow entrainment ratio w, the value of area ratio At/Ad (cross section of minimum area of primary nozzle/cross section of constant area duct) can be estimated for an ejector's optimum design.

Open image in new window Fig. 2 Geologic cross section of study area (Cornet and Trayssac 1952, modified by Chibane and Ali-Rahmani 2015) Open image in new window Fig. 3 Geologic Map of study area.