deletions | additions       diff --git a/section_Adriatic_Sea_morphology_and__.tex b/section_Adriatic_Sea_morphology_and__.tex  index 9d0d7fe..5d8fae8 100644  --- a/section_Adriatic_Sea_morphology_and__.tex  +++ b/section_Adriatic_Sea_morphology_and__.tex 
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Marked morphological differences characterize the basin along its longitudinal transversal axes. Accordingly the Adriatic Sea can be divided into three sub-basins (Artegiani et al., 1996).  The northern sub-basin is characterized by a shallow average depth of ~35 m with a very weak bathymetric gradient toward south-east where the 100 m bathymetric line is met in front of Giulianova (Italy).  and gently slopes toward the 100 m bathymetric line (in front of Giulianova, Italy) and is characterised by an extremely shallow mean depth (about 30 m) with a very weak bathymetric gradient along the major axis, and by a strong river runoff (~ 3000 m3 s-1) relative to the receiving basin; in fact, Po and the other northern Italian rivers are believed to be the source of about 20\% of the total Mediterranean river runoff (Hopkins, 1992).