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Les plongées d'eaux profondes ponctuelles sont représentées par la pastille noire, la thermocline entre les deux couches de densité ? 1 et ? 2 est située à la profondeur h. Le bassin possède une profondeur uniforme égale à H. Les remontées d'eaux profondes sont uniformes au niveau de la thermocline ,
où sont représenté les processus importants pour la THC : les forçages de surface en chaleur (heat uxes) et en eau douce (freshwater uxes), la formation d'eau profonde (deep water formation), la glace de mer (sea ice), le vent (wind), le mélange diapycnal (diapycnal mixing), les ondes internes (internal waves), le mélange dû aux upwelling forcé par le vent (mixing driven upwelling), le tranport de volume (volume transport) et le prol du passage de Drake (prole of Drake passage ), p.22, 2006. ,