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ENVIRONMENTAL IMPACT STUDY Rn: 03-033 CONTAINER TERMINAL PLOCE PAGE: 16 On the basis of the data under (5) information is obtained for the area of Ploèe with regard to geodetic zero (Trieste) that: Mean sea level SRM = +0.32 m SNNžR = +0.12 m (hydrographic zero) Extr.NžR10 = -0.22 m Extr.NžR100 = -0.32 m A SVVšR = + 0.35 m Extr.VR10 = +1.00 m Extr.VR100 = +1.10 m According to this long-term forecast we can see, a piece of information interesting for us, that in the ten-year return period the possible amplitude is about 1.22 m while in the hundred-year return period the maximum possible oscillation of the level is 1.42 m which should be taken into consideration in designing the port quay. The latest investigations of sea level fluctuations in the port of Ploèe are shown in the study of the Croatian Hydrographic Institute (4). On the basis of measurements conducted continuously from March 2002 to March 2003, calculations were made of the values of the sea mean level (SRM) and of the hydrographic zero (HN) in the area of the port of Ploèe, and these were compared with the geodetic zero (GN) and mareographic zero (MN) (mareograph measures the height of the sea level in relation to the mareographic zero). The relationships are as follows: SRM - HN = 24.5 cm SRM - MN = 121.1 cm SRM - GN = 42.2 cm HN - MN = 96.6 cm HN - GN = 17.7 cm GN - MN = 78.9 cm With regard to shortness of measured period a survey of relationships of SRM, HN and GN in Split based on 19-year measurements is given too. Namely, because of astronomic parametres which influence the tidal fluctuations of the sea level, it is exactly this time period that is necessary for an accurate definition of the hydrographic zero. Therefore: SRM - HN = 20.2 cm SRM - GN = 30.7 cm HN - GN = 10.5 cm Consequently, the difference between SRM and HN in Split is slightly smaller than in Ploèe which is the consequence of semi-diurnal components which have higher amplitudes in Ploèe than in Split. Furthermore, in the investigated period the mean sea water level in Split is by about 10 cm higher than in the several-year period and this relationship is also valid in the port of Ploèe aquatorium. It is therefore to be assumed that the values of HN and SRM in Ploèe in the investigated one-year period are about 10cm higher than in the 19-year period, which has to be taken into consideration during planning of activities over a longer time period. The graphic presentation of daily sea level values is shown in fig. 9 RIJEKAPROJEKT d.o.o.
HEIGHT OF SEA LEVEL (m) HEIGHT OF SEA LEVEL (m) ENVIRONMENTAL IMPACT STUDY Rn: 03-033 CONTAINER TERMINAL PLOCE PAGE: 17 Figure 14. Mean annual values of the sea level height in relation to the mareographic zero in Ploèe in the period from March 2002 - March 2003 Here we can see consistency with previously mentioned source, having taken into consideration the extrapolation for a long-term period Figure 15. Values of sea level height in Ploèe recorded during occurrence of port standing waves. RIJEKAPROJEKT d.o.o.
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