INFLUENCE OF VARIABILITY IN WATER TRANSPORT ON PHYTOPLANKTON BIOMASS AND COMPOSITION IN THE SOUTHERN NORTH-SEA - A MODELING APPROACH (FYFY)

Citation
Aj. Vandenberg et al., INFLUENCE OF VARIABILITY IN WATER TRANSPORT ON PHYTOPLANKTON BIOMASS AND COMPOSITION IN THE SOUTHERN NORTH-SEA - A MODELING APPROACH (FYFY), Continental shelf research, 16(7), 1996, pp. 907
Citations number
37
Categorie Soggetti
Oceanografhy
Journal title
ISSN journal
02784343
Volume
16
Issue
7
Year of publication
1996
Database
ISI
SICI code
0278-4343(1996)16:7<907:IOVIWT>2.0.ZU;2-O
Abstract
A model for phytoplankton composition and succession coupled to a tran sport model for the southern North Sea is presented. This model is use d to examine the time and spatial variability in phytoplankton biomass and succession. Long term time variability due to the variability in horizontal water transport is studied by using daily varying transport fields for the period 1970-1981. These transport fields result from s imulations with a circulation model driven by realistic wind fields fo r this period. Selective factors for phytoplankton are resource compet ition and zpoplankton grazing. This leads to a general abundance of ed ible phytoplankton groups in the whole southern North Sea, while poorl y edible groups mainly occur in the eutrophicated coastal areas. Apart from this, phytoplankton groups which are specialized in growth under nitrogen-limited conditions are selected in open sea while, near the Dutch coast and the German Eight, phosphate-specialized groups are sel ected. From a comparison of simulations with yearly averaged and daily varying transport fields, it is concluded that differences with respe ct to the annual mean phytoplankton biomass are negligible. However, l arge differences are found for the distribution and abundance of speci fic phytoplankton groups. A simulation for the period 1970-1981 shows that part of the observed variability in spring biomass as well as the variability in the duration of dominance and abundance of species nea r the Dutch coast can be attributed to the variability in the horizont al water transport.