In semi-diurnal tides like ours the strongest ebb and flow current is present during the second and third hours after the height or the ebb of the tide, after and before which the flow is considerably slower.
Kukuzala nokurhoxa okuphantse kwaba kokwasemini njengoku bohla koku kwethu kunamandla kunye nokuhamba komsinga kukhona ngexesha lemizuzwana emibini neeyure ezintathu emva kobude okanye ukuboha kokuzala nokurhoka, emva okanye phambi kohambo oluqwalaselekayo okuhamba kancinci.