Optical remote sensing in support of eutrophication monitoring in the southern North Sea
Vera De Cauwer, Kevin Ruddick, YoungJe Park, Bouchra Nechad and Michael Kyramarios
Abstract
Spring mean
and maximum chlorophyll a (chl a) concentrations are main factors to
determine the eutrophication status of the Belgian waters as agreed within
OSPAR in 2002. Other important assessment parameters to measure the degree of
nutrient enrichment - the amounts of inorganic phosphate and nitrogen in winter
- appeared to be above thresholds for most measurements performed in the period
1974-2002. As the standard in situ monitoring programme does not give a
clear picture of the temporal and spatial distribution of chl a, it is logical to complement these
measurements with optical remote sensing. However, chlorophyll concentrations
derived from sensors such as SeaWiFS are unreliable in the Case 2 waters of
this region because of high particulate and dissolved yellow substance
absorption. Another important limitation of ocean colour sensors is the amount
of useful images due to cloud cover. The combination of data from different
ocean colour sensors in order to enable a better temporal coverage might be
hampered by the different chlorophyll retrieval algorithms used. This study
compares different global chl a
algorithms (MODIS, SeaWiFS, MERIS) as well as a turbid water algorithm for the
Southern North Sea. This is done by running the different algorithms on in
situ reflectance spectra collected at 107 stations in the period 2001-2002
over the Southern North Sea and comparing them with in situ chl a concentrations, as well as by running
the algorithms on a MERIS image of the 29th of July 2002. Based on
this validation the accuracy of these products and their suitability for
eutrophication monitoring in the Southern North Sea are assessed.
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History
Submitted: 25 July 2003
Revised: 06 February 2004
Accepted: 03 March 2004
Citation
De Cauwer V, K Ruddick, YJe Park, B Nechad & M Kyramarios, 2004. Optical remote sensing in support of eutrophication monitoring in the southern North Sea. EARSeL eProceedings 3(2), 208-221
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ISSN 1729-3782
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