As the thermocline rises up a sloping lake bed, it can also cause benthic turbulence by convective overturning, whereas the falling thermocline experiences
storage tank with closed water circuit, stratified thermal storage, thermocline tank and water stratified tank storage but in all cases the significant
permanent thermocline. The temperature difference through this layer may be as large as 20°C, depending on latitude. The permanent thermocline coincides