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SCM SCO SNB |
CS MBS NCI NCO NNB SCI SCM SCO SNB |
Surface 0.00% 1.65% 0.37% 0.74% 0.37% 1.72% 0.99% 0.09% 0.74% |
Bottom 1.11% 3.14% 2.58% 1.48% 2.95% 2.46% 1.23% 1.57% 1.97% |
49 |
Finally, we compared similarities (differences) in nutrient concentration among |
segments using Kruskal-Wallis test for three parameters of interest for numeric nutrient |
criteria development, TN, TP and CHLa. Results are shown in Table 3.2. Differences in |
Total Nitrogen distribution are not statistically significant for CS-NCI; NCO-SNB-NNB; |
NCI-SNB-NNB; and SNB-NNB. For TP, there are not statistically significant differences |
for MBS-NCO; SCI-CS-NCI; SCM-SCI; and CS-NCO-NCI. For CHLa, there are not |
statistically significant differences for MBS-NCO; and CS-NCI. In summary, for those |
segment pairs (triplets) with no significant differences the same criteria may apply. |
Table 3.2: Results of Kruskal-Wallis test comparing TN, TP and CHLa distribution |
among segments of Biscayne Bay. Probabilities highlighted in bold (p>0.05) are those |
pairs whose differences are not statistically significant. |
MBS SCI SCO SCM C S NCO NCI SNB NNB |
MBS 1 * * * * * * * * |
SCI 0.000 1 * * * * * * * |
SCO 0 0 1 * * * * * * |
SCM 0 0 0 1 * * * * * |
C S 0 0 0 0.012 1 * * * * |
NCO 0 0 0.000 0 0.002 1 * * * |
NCI 0 0 0 0.001 0.458 0.018 1 * * |
SNB 0 0 0 0 0.020 0.285 0.127 1 * |
NNB 0 0 0 0 0.050 0.246 0.221 0.846 1 |
MBS SCI SCO SCM C S NCO NCI SNB NNB |
MBS 1 * * * * * * * * |
SCI 0.000 1 * * * * * * * |
SCO 0 0.000 1 * * * * * * |
SCM 0 0.009 0.340 1 * * * * * |
C S 0.001 0.795 0.001 0.036 1 * * * * |
NCO 0.269 0.053 0 0.000 0.044 1 * * * |
NCI 0.000 0.295 0.021 0.193 0.470 0.006 1 * * |
SNB 0 0 0 0 0 0 0 1 * |
NNB 0 0 0 0 0 0 0 0 1 |
MBS SCI SCO SCM C S NCO NCI SNB NNB |
MBS 1 * * * * * * * * |
SCI 0 1 * * * * * * * |
SCO 0 0 1 * * * * * * |
SCM 0 0.016 0 1 * * * * * |
C S 0 0.016 0 0 1 * * * * |
NCO 0.661 0 0 0 0 1 * * * |
NCI 0 0.075 0 0.000 0.568 0 1 * * |
SNB 0 0 0 0 0 0 0 1 * |
NNB 0 0 0 0 0 0 0 0.000 1 |
p-value for Total Nitrogen |
p-values for Total Phosphorous |
p-values for Chlorophyll-a |
50 |
TREND ANALYSIS |
Biscayne Bay has been a dynamic environment over the last 500 years, |
experiencing marked salinity and benthic habitat variability. Some changes may be |
connected to anthropogenic intervention while others seem to respond to regional or |
global changes. Salinity has increased, seagrass has declined; open-marine species |
have replaced estuarine assemblages and the reduction of managed freshwater |
deliveries into BB has been coupled with increases in foraminifera abundance (Archaias |
and Articulina) since 1947 and declines in Thalassia after 1950 (Wingard et al 2004). |
Since the middle 1980’s significant regional ecosystem shifts have been documented in |
South Florida coastal waters (Boesch et al. 1993; Fourqurean and Robblee 1999; Hunt |
and Nuttle 2007; Briceño and Boyer 2010). Some of the significant changes were: |
seagrass die-off beginning in 1987; large plankton blooms in the western and central |
portions of the Florida Bay (Robblee et al. 1991); increased phytoplankton abundance |
(Phlips and Badylak 1996); increased turbidity; significant declines in fisheries and |
shrimp harvest (Tabb and Roessler 1989; Tilmant 1989); sponge mass mortality in hard |
bottom areas of southern Florida Bay (Butler et al. 1995); extended coral bleaching in |
the Florida Keys reef tract after the 1980’s; and sustained nutrient concentration decline |
in waters leaving the Everglades (Briceño and Boyer 2007, 2008). |
Recent changes in BB have been reported by Migliaccio et al. (2008) who |
studied biogeochemical trends from years 1996 to 2007, using DERM, NPS and FIU |
data. They reported increasing trend for chlorophyll-a likely responding to the increase |
in NH4-N, SRP, and TPO4-P, in turn responding to a dramatic population increase and |
land use change in the watershed from agricultural land to residential and urbanizing |
areas. |
Our analysis of time-series components was performed with Akritas Theil/Sen |
regression (ATS) for secular trend (Appendix 9) and Zcusum charts for detailed |
scrutiny. A Cusum chart is a plot of the cumulative sum of deviations (Sn= Σ[zi-T] for |
i=1….n) from a target (T), in our case, the time-series grand mean, against n, the |
sample number (or date if regularly sampled) (Ewan, 1963). Cusum charts and Cusum |
analysis are standard procedure in the field of industrial process control (Duncan 1974; |
Grant and Leavenworth 1980; Montgomery 2001). For a detailed explanation on |
51 |
construction, properties and applications of Zcusum charts, the reader is referred to |
Appendix 4). Visual inspection of Zcusum charts gives a detailed history of the |
parameters variability along the time-line or another variable gradient providing more |
information than ATS, ordinary linear regression or Line of Organic Correlation. |
Finally, we must always keep in mind that trend analysis is limited to the window |
of observation; trends change with continued data collection. In addition, water quality in |
South Florida may fluctuate according to disturbance events of longer periodicity, and |
trends may even reverse during a given period of record. |
Total Nitrogen |
As shown in Fig 3.19, TN declined across the Bay displaying two cycles common |
to all segments during the POC. From 1996 to 1999 values were in general above |
average (positive Zcusum slope), followed by a decline to below average values until |
2002, except in SCO where the decline began in 1998. The second cycle extends from |
2003 to 2007, with the break from above to below average approximately occurring at |
the end of 2004. In MBS the second cycle is less developed. Finally, seasonality is |
crudely developed, perhaps reflecting managed water deliveries non tuned to natural |
rain cycles and water inflow. |
Total Phosphorous |
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