Falmouth Group 8

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Station 1

At station 1, transmissivity values near the surface were on average approximately 4.30. This peaks at around 10m  depth around 4.32 and remains at similar values at deeper depths. The range in the values at specific depths is approximately 0.04, with an overall range of 4.28-4.33.


Transmissivity-Figure 1

Salinity increases in the first 10 meters from 35.0 to 35.2 from there the salinity decreases to a minimum 34.9 at 27.4 meters. The overall change in salinity from 1.2m to 27.4 m is negative 0.1.Silicon concentration remains constant, 1.56µmol/L in the first 10 meters it then decreases at a constant rate to 1.45µmol/L at 27.4 meters. Phosphate concentration at the surface water is 7.8x10-4µmol/L and increases in the first 10 meters to 0.00105µmol/L. The concentration decreases to a minimum of 6.1x10-4µmol/L at 27.4 meters showing an overall decrease of 1.7x10-4µmol/L. Nitrate concentration shows a continued decrease from 13.01µmol/L at 1.2 meters to 1.92µmol/L at 27.4 meters, an overall decrease 11.09µmol/L. The graph shows that after 10 meters there is a greater rate of decrease in Nitrate concentration at a rate of 0.31µmol/L per meter. All the changes shown by the nutrient concentrations occur before the estimated 1% irradiance depth, which was calculated using the secchi disk values.


Nutrients-Figure 2

Fluorescence-Figure 3

Error range: 0.473-0.375 = 0.98

The graph shows that the general trend in fluorescence increases between 0 and 9m by 0.7. For the rest of the water column fluorescence is relatively stable averaging at about 0.445. The graph shows one outlier at 21m with a fluorescence of 0.678.  


ADCP Transect- Figures 4,5&6

In terms of backscatter, the ADCP readings are generally consistent apart from the extremities at either end showing high anomalous readings from the turning boat’s wake. On the left side of the diagram tidal flow seemed to exhibit signs of the coriolis force in action as it was being directed southwards to the right at approximately 0.5 m/s.

Evidence of changes in the flow regime can be observed with flow on one side of the estuary proceeding in a southerly direction down to -0.5 m/s with regards to north velocity, whilst the tidal flow on the other side of the estuary appeared to be moving in a northerly direction at up to 0.5 m/s. This is also evident from the current directions displayed on the ship track.


Click graphs to enlarge

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