Using data from closely spaced CTD profiles taken after the 1993 major infl
ow of North Sea water, we investigate the characteristics and generation me
chanisms of finestructure intrusions in the Baltic halocline. Due to the st
rong prevalence of salinity over temperature in density stratification, the
salt fingering is not possible, and diffusive convection has a limited eff
ect on thermohaline intrusions in the halocline. Some evidence for inertial
oscillations as a driving mechanism for the intrusions is found. In severa
l occasions, we observed odd intrusion-like structures crossing isopycnals
in such a way that the along-layer density ratio is approximately equal to
the vertical density ratio. We show that these 'odd intrusions' are not lik
ely to be generated from the interleaving process, and several alternate sc
enarios for their generation are suggested. (C) 1999 Elsevier Science B.V.
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