Deep Sea Research Part I: Oceanographic Research Papers
On the sensitivity of ecosystem box model simulations on mixed-layer depth estimates
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Cited by (14)
N:Si ratios and the 'balance of organisms': PROWQM simulations of the northern North Sea
2005, Journal of Sea ResearchCitation Excerpt :No adequate climatology of Surface Mixed Layer (SML) thickness was available for this region, and so comparisons of simulated and observed SML thickness used FLEX observations from spring 1976 and PROVESS observations from autumn 1998. A time series of mixed layer depths during the FLEX was taken from Eigenheer et al. (1996), who defined the SML as the layer (next to the sea surface) in which the vertical gradient of daily mean temperature was less than 0.02 °C m− 1. In autumn 1998, regular CTD profiles were made by all ships visiting the PROVESS site, and the data assembled by Luyten et al. (2002).
The PROWQM physical-biological model with benthicpelagic coupling applied to the northern North Sea
2002, Journal of Sea ResearchCitation Excerpt :Mills et al. (1994) suggested that the phytoplankton critical depth (Sverdrup, 1953) exceeded the depth of the water column prior to the start of stratification at station CS in the central North Sea. The FLEX observations summarised by Eigenheer et al. (1996) show some increase in chlorophyll and production, and a decrease in nitrate concentration, prior to stratification. In our standard simulation, the spring bloom, defined as occurring when chlorophyll concentration exceeded 1 mg m−3, started before the commencement of persistent stratification.
The impact of thermal stratification on phytoplankton and nutrient dynamics in shelf seas: A model study
1997, Journal of Sea Research