Animation of year 2001 FerryBox results


View animation files directly or see full descriptions below

                 Click here for an animation of the offshore bloom, May 2001
                Click here for an animation of the Southampton Water bloom June 2001
                Click here for an animation of the salinity and chorophyll data with a clock indicator of tidal range
 

What the animations show

The data have been animated to assist in data interpretation. In each of the diagrams
the amount of chlorophyll is indicated by a colour scale.  This ranges from low values
in the blue. The bloom takes off when chlorophyll  levels are in excess of 10 mg/m3
(the green range), peaking around 40 mg/m3  this year indicated by red and pink colours.
The Red Falcon ferry makes up to 16 crossings each day between Town Quay to the north
and Cowes to the south on the Isle of Wight (data every minute).

This plot is a single frame from the animation of the spatial distribution of chlorophyll
along the ferry track. In this example high chlorophyll levels (seen in orange) are found
offshore close to the Isle of Wight.


 
 
 

Between April and August of this year there were 2 main blooms associated with neap tides.
Animation of the data obtained allows us to look at the distribution of phytoplankton during
these two main blooms.

Development of the first bloom of diatoms in May can be followed from one spring tide to
the next.  Individual ferry tracks from day 129 (on the 9th May) to day 145 (on the 25th May)
have been strung together and show the development of an offshore bloom.

Click here for an animation of the offshore bloom, May 2001

        Low chlorophyll indicated by blue colours increased into the green colours over the track of
        the ferry.   The main activity is seen in the Solent.  The chlorophyll levels peaked (at over
        30 mg/m3 indicated by orange and red colours) on day 137, on the neap tide.  The
        chlorophyll levels remained high but very patchy after the neap tide due to the large
        slicks of phaeocystis which were not broken up by the higher energy spring tides.

Another animation of the ferry tracks show the development of the phytoplankton
blooms in June from one spring tide on day 159 (8th June) to the next on day 174
(23rd June). In this case the picture is clearer than the May bloom as the chlorophyll
levels were low on each of the spring tides.  The peak of the bloom is on
the neap tide (day 167).

Click here for an animation of the Southampton Water bloom June 2001

        This time the chlorophyll levels increase in Southampton Water and remain low offshore.
        Chlorophyll levels peaked inshore, near Southampton, on the neap tide on day 167.
        It is thought that low nutrient levels in the higher salinity water limit development
        of the bloom offshore.

Chlorophyll and salinity contours

Contours of chlorophyll and salinity with respect to latitude can also be produced
from the data.  This allows us to look at the spatial distribution of chlorophyll in
Southampton Water and the Solent with additional temporal information.  Tidal
information has been illustrated by a clock, it is largest (with hands
pointing to midnight) when the tidal range is largest (on a spring tide).

Here the distribution of chlorophyll and salinity is shown on a neap tide, day 137.
The clock size is small (the hands pointing to  6:30) indicating a neap tide.
In this example the bloom is seen offshore with some indication of high
chlorophyll being washed up Southampton Water with the high tide.


On the springs the tidal range is larger so the low salinity water is seen spreading
further out into the Solent on the ebb tide.  The chlorophyll levels tended to be low
on the spring tide this year.  This is in contrast to previous years, however it is an
easier picture to interpret as we would not expect to see blooms associated with
high energy spring tides.

On a spring tide high water is at midnight and midday, animation of
hese files show the change in tidal range and progression of the tide as the
high salinity peak moves to the right.  In many cases the chlorophyll and
salinity can be correlated by close examination of these images.
 

We can string individual frames together to obtain an overall picture of
chlorophyll related to position, time and the tides from day 115 (25th April)
to day 227 (15th August).

Click here for an animation of the salinity and chorophyll data with a clock indicator of tidal range

        Salinity values increase through the year.  At the start of this animation
        during a spring tide low salinity and low chlorophyll values are seen.
        After a short period of missing data the chlorophyll concentrations
        start to increase around the spring tide on day 129 in May.
        They continue to increase, especially offshore, peaking on the neap tide on day 137.

        After this time the chlorophyll levels are high and patchy offshore.  Around
        day 154 at the start of June the chlorophyll values are low again (on the spring tide).
        After this time they increase further north (in Southampton Water) and peak on day
        167 (the 16th June), on a neap tide.

        Chlorophyll values decrease towards the following spring tide increasing around
        the neap tide (day 183 at the start of July) although the chlorophyll concentrations
        are halved compared with the May and June blooms.  On the following neap tides
        on days 196 in July and 226in August chlorophyll levels remain low.

Further work is needed to link this with other factors such as the weather
and nutrient levels.
 
 


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Page last updated by SUH 25 Sept 2001 (Pagnani 5-Dec-2008).