Free Access

Fig. 1


Notation used, showing temperature as a function of depth through half of a semiconvective layer of thickness d, from the middle (z = 0) of the stagnant zone (of thickness ds), to the middle of the overturning zone at z = d/2. ΔT is the temperature difference across the whole layer, across the overturning zone. The solute profile has the same shape but different amplitudes ΔS and .

Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.

Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.

Initial download of the metrics may take a while.