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SCM SCO
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Highest salinity occurs across the bay in May and lowest salinity occurs in
September to November (Fig 3.7). There is a significant drop in salinity between May
and June, reaching up to 9 PSU (NNB and SCI) at the beginning of the wet season.
Non-parametric Mann-Whitney tests indicate that salinities among the defined WQ
clusters are significantly different (p<0.05) except for NCI and SCM, and NCO and CS
with non-significant statistical differences at p=0.12 and p=0.51 respectively.
The salinity patterns derived from monthly data shown here are clearly an
oversimplification when compared to high frequency data (15 min sampling rate) as
those reported by the BNP for NCI, SCI and SCM (BNP 2008; Bellmund et al. 2009). In
fact, salinity in the mangrove areas is substantially different from the salinity further east
in Biscayne Bay, displaying frequent hypersalinity conditions and responding more to
groundwater variability than to local canal flow. A consequence of salinity variability is
that extension of estuarine conditions (salinity < 20 PSU) in the bay is rather variable.
According to Bellmund et al. (2009) average estuarine area for the wet season (2004-
2008 period) was 2,714 hectares, but in the dry season it contracted to only 454
hectares. FIU’s data indicate that estuarine conditions have occurred since June 1996
in only 14% and 7% of the records for MBS and SCI, respectively. These figures clearly
indicate how little Biscayne Bay resembles a true estuary.
Figure 3.7: Seasonal variability of Salinity in Biscayne Bay
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