In addition, presence of the barrier layer in
pre-Jangmi profile is influencing the results: the pre-Jangmi
salinity profile (squares at middle plot in Fig. 5) shows that,
within the 80m deep ML, there exists a shallower layer of
fresher ( 0.1 psu) water, and such a structure may reduce
the amount of cooling associated with the typhoon passage
(Wang et al., 2011)