392
DYNAMICAL OCEANOGRAPHY
(regime 1) whereas the low salinity and temperature states are non-convective
and exist for Φ S < −1/3 (regime 2). Regime 3 is exactly located in the interval
−5/7 < Φ S < −1/3 and in this regime, multiple equilibria exist. Note that
regime 4 is not reached here, because Φ T > 0.
DYNAMICAL OCEANOGRAPHY
(regime 1) whereas the low salinity and temperature states are non-convective
and exist for Φ S < −1/3 (regime 2). Regime 3 is exactly located in the interval
−5/7 < Φ S < −1/3 and in this regime, multiple equilibria exist. Note that
regime 4 is not reached here, because Φ T > 0.