Review of the Biological Oceanography of the Strait of Georgia: Pelagic Environment

1983 ◽  
Vol 40 (7) ◽  
pp. 1064-1094 ◽  
Author(s):  
P. J. Harrison ◽  
J. D. Fulton ◽  
F. J. R. Taylor ◽  
T. R. Parsons

Different components of the food web in the Strait of Georgia are reviewed. The phytoplankton are dominated by diatoms; however, flagellates may dominate in the winter. Chlorophyll a concentrations may range from < 1 mg∙m−3 in the winter to > 15 mg∙m−3 during blooms. The average annual primary productivity is about 280 g C∙m−2 for the strait, but it is higher in frontal areas at the north and south ends of the strait and near the Fraser River plume. Light limits primary productivity during the winter months, while nutrients (nitrogen) and grazing are the limiting factors during the late spring and summer. Turbidity and salinity effects occur near the Fraser River plume. The surface macrozooplankton community is composed chiefly of copepods. Mid- and deep-water communities consist of euphausiids, chaetognaths, and some deep-living copepods, which overwinter at depth. The standing stock of macrozooplankton (> 350 μm) to 400 m, ranges from 0.1 to 2.0 g wet wt∙m−3. Few estimates of secondary production and standing stock estimates of microzooplankton have been made. Horizontal patches of zooplankton have been encountered and may be important feeding sites for some fish. Standing stock associations of the dominant species in the food web of the strait are reasonably well known, but assessment of food web dynamics from these limited standing stock measurements is often inaccurate. There is a noticeable absence of data on how rate processes affect standing stocks, and it is particularly an understanding of these interrelationships that is needed for fisheries management. There is an urgent need for more interaction between biological oceanographers and fisheries scientists, particularly in the area of zooplankton grazing by larval fish.


1970 ◽  
Vol 27 (7) ◽  
pp. 1251-1264 ◽  
Author(s):  
T. R. Parsons ◽  
R. J. LeBrasseur ◽  
W. E. Barraclough

Data have been accumulated on seasonal levels of nutrients, primary production, and zooplankton. The occurrence and abundance of larval fish in the surface layers have been reported together with an approximate estimate of the standing stock of commercially exploited fish. The results indicate that beyond local effects, the Strait of Georgia is comparable in productivity to other nearshore waters at the same latitude. The total primary productivity of the waters was found to be approximately 120 g C/m2 per year, but a high degree of areal patchiness in all production data emphasizes the necessity of basing predictions about particular subareas on knowledge specific to the subareas in question.



1993 ◽  
Vol 50 (7) ◽  
pp. 1456-1466 ◽  
Author(s):  
M. A. St. John ◽  
S. G. Marinone ◽  
J. Stronach ◽  
P. J. Harrison ◽  
J. Fyfe ◽  
...  

Model simulations revealed that wind mixing was the dominant physical mechanism that added nitrate to the surface layer and subsequently enhanced primary productivity in the Strait of Georgia. Simulations of high Fraser River runoff showed that the enhanced stability of the water column in the vicinity of the riverine plume made wind mixing of nutrients into the surface layer more difficult. We propose that this increase in stability results in an earlier onset of the spring bloom in regions influenced by Fraser River runoff. During the summer, an increase in the buoyancy of surface water due to the freshwater plume reduces nitrate concentration in the surface layer and thereby limits primary production in the plume area. The reduced impact of wind events on nitrate fluxes is the result of a greater energy requirement to break down the more buoyant surface layer. Results indicate that during the fall, when light is again limiting and surface nitrate concentrations increase due to wind mixing by fall storms, the freshwater runoff from the Fraser River results in a more stable water column (similar to the spring situation) in the southern Strait, resulting in the potential for a fall bloom.



1981 ◽  
Vol 6 (2-3) ◽  
pp. 201-221 ◽  
Author(s):  
J.A. Stronach




1990 ◽  
Vol 143 (1-2) ◽  
pp. 139-146 ◽  
Author(s):  
W.P. Cochlan ◽  
P.J. Harrison ◽  
P.J. Clifford ◽  
K. Yin


1995 ◽  
Vol 52 (3) ◽  
pp. 644-650 ◽  
Author(s):  
Richard J. Beamish ◽  
Chrys-Ellen M. Neville

River lamprey (Lampetra ayresi) enter the Strait of Georgia from the Fraser River and feed almost exclusively on Pacific herring (Clupea harengus) and salmon (Oncorhynchus spp.). Although the major prey of river lamprey is Pacific herring, the greater effect of lamprey predation was on the populations of chinook (O. tshawytscha) and coho (O. kisutch) salmon. In 1990 and 1991, river lamprey killed a minimum of 20 million and 18 million chinook salmon, respectively, and a minimum of 2 million and 10 million coho salmon in the same years. In 1991, river lamprey in the Fraser River plume killed an equivalent of approximately 65 and 25% of the total Canadian hatchery and wild production of coho and chinook salmon, respectively. These estimates are probably low because river lamprey also feed in other areas and the abundance estimates are conservative. These high mortality rates indicate that river lamprey predation must be considered as a major source of natural mortality of chinook and coho salmon in the Strait of Georgia.





1988 ◽  
Vol 23 (1) ◽  
pp. 179-614 ◽  
Author(s):  
J. A. Stronach ◽  
P.B. Crean ◽  
T.S. Murty

Abstract The Fraser River forms a well-defined layer of brackish water in the Strait of Georgia, with associated strong surface currents and salinity contrasts between it and the much deeper underlying waters. The numerical solution of a rotating, non-linear, reduced gravity, vertically integrated, upper layer model to describe the motion of this large river plume is described. Results from extensive field observations including tracking of surface drifters and CTD surveys are used to adjust and verify the model. Comparisons of observed and computed velocity and salinity fields show that the model simulates well the dominant flow patterns of the plume. A hindcast of two time periods in June and November 1986 is presented. Both hindcasts were characterized by periods of calm winds as well as the passage of reasonably intense storms, so that the response of the plume to wind forcing, as distinct from the wind-free situation, was quite well delineated.



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