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Concentrations of suspended chlorophyll in the tidal Yorkshire Ouse and Humber Estuary
Uncles, R.; Easton, A.E.; Griffiths, M.L.; Howland, R.J.M.; Harris, C.; Joint, I.; King, R.; Morris, A.; Plummer, D. (1998). Concentrations of suspended chlorophyll in the tidal Yorkshire Ouse and Humber Estuary. Sci. Total Environ. 210-211: 367-375. https://dx.doi.org/10.1016/s0048-9697(98)00024-2
In: Science of the Total Environment. Elsevier: Amsterdam. ISSN 0048-9697; e-ISSN 1879-1026, meer
|  |
| Trefwoorden |
ANE, British Isles, England, Humberside, Humber Es
Particulates > Suspended particulate matter
Salinity
Mouth of the Humber [Marine Regions]
|
| Author keywords |
Yorkshire Ouse, Chlorophyll a, Phaeopigments |
| Auteurs | | Top |
- Uncles, R.
- Easton, A.E.
- Griffiths, M.L.
|
- Howland, R.J.M.
- Harris, C.
- Joint, I.
|
- King, R.
- Morris, A.
- Plummer, D.
|
| Abstract |
in the tidal reaches of the Yorkshire Ouse and Humber Estuary, UK, are presented for the period March 1994–March 1995. Chlorophyll a concentrations were<3 μg l−1 throughout the tidal Ouse and Humber during March and April 1994. Generally, concentrations were also low in the non-tidal Yorkshire Ouse (<4 μg l−1). Increases in chlorophyll a in the non-tidal river during May–August corresponded with increased concentrations in the tidal river, with highest concentrations occurring at the lowest observed salinities. Large declines in chlorophyll a concentrations, from 60 to<13 μg l−1, occurred along a transect from the non-tidal river to the tidal river during summer, which probably resulted from a combination of net negative growth rates and mortality in the extremely turbid receiving waters. Chlorophyll a concentration decreased to<10 μg l−1 (but usually<5 μg l−1) in the non-tidal river during autumn and was less than 1 μg l−1 throughout much of the winter. Concentrations were also at a minimum within the tidal river and Humber. However, a noticeable feature was a local maximum of chlorophyll a at the interface between fresh and brackish waters, which was associated with the zone of higher turbidit |
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