2006
DOI: 10.1007/3-540-33648-6
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Marine Eutrophication in Perspective

Abstract: The use of general descriptive names, registered names, trademarks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use.

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Cited by 38 publications
(11 citation statements)
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“…The OSPAR Commission has jurisdiction for the broader European North-East Atlantic Ocean, thus has contracting parties additional to those counties that border the North Sea (Belgium, Netherlands, Germany, Denmark, Norway, and the United Kingdom). As recounted in detail by de Jong (2006), eutrophication began to command attention after the occurrence of hypoxic events in the German Bight of the North Sea in 1981 and 1982 that followed from the rapid growth of phosphorus and, particularly, nitrogen discharges from the continental rivers during the 1960s and 1970s. The environmental ministers of the OSPAR contracting parties agreed in 1987 to reduce the river loads of dissolved inorganic phosphorus and nitrogen to 50% of the levels in 1985 by the year 1995.…”
Section: North Seamentioning
confidence: 99%
“…The OSPAR Commission has jurisdiction for the broader European North-East Atlantic Ocean, thus has contracting parties additional to those counties that border the North Sea (Belgium, Netherlands, Germany, Denmark, Norway, and the United Kingdom). As recounted in detail by de Jong (2006), eutrophication began to command attention after the occurrence of hypoxic events in the German Bight of the North Sea in 1981 and 1982 that followed from the rapid growth of phosphorus and, particularly, nitrogen discharges from the continental rivers during the 1960s and 1970s. The environmental ministers of the OSPAR contracting parties agreed in 1987 to reduce the river loads of dissolved inorganic phosphorus and nitrogen to 50% of the levels in 1985 by the year 1995.…”
Section: North Seamentioning
confidence: 99%
“…Considerable confidence in the estimate of precision in the slope of the relative flux with wavelength can be gained by examining the internal agreement among the HST standards: i) Bohlin (2007a) illustrates the <<1% agreement of the three primary WD models with their calibrated fluxes, which means that if the slope of any model, which depends primarily on T eff , is in error, then the other two model temperatures must be similarly in error in order to make the same change in flux vs. wavelength for all three stars from 0.12-2.5 µm. ii) The NICMOS photometric calibration is based on the HST primary standard G191B2B and the secondary standard P330E per de Jong (2006), where the consistency of the absolute spectrophotometry is confirmed for these two SEDs from the CAL-SPEC 8 database. In particular, de Jong's Figure 2 shows an agreement of 0.8-1.4% between the NICMOS calibrations derived from the SEDs for P330E and G191B2B over the combined 0.9-2.4 µm range of the three cameras.…”
Section: Uncertaintiesmentioning
confidence: 99%
“…Experts and scientists from different disciplines, users of the knowledge and affected people are part of this extended forum. Often new institutions have to be introduced to function as science–policy interfaces, such as in the cases of climate change and sea management (Boehmer‐Christiansen 1994; de Jong 2006). An extended forum should be regarded as an integral part of participative forms of ‘good governance’.…”
Section: Concepts and Questionsmentioning
confidence: 99%
“…Nevertheless, we think that the third position is most appropriate and effective because it is compatible with other positions, as demonstrated by the ecologists of Alterra. In discussions on climate change (Boehmer‐Christiansen 1994) and sea management (de Jong 2006), experience with this strategy is already available.…”
Section: Ecology and Policymentioning
confidence: 99%