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Phytoplankton Responses to Vertical Tidal Mixing

  • Chapter
Tidal Mixing and Plankton Dynamics

Part of the book series: Lecture Notes on Coastal and Estuarine Studies ((COASTAL,volume 17))

Abstract

Vertical mixing of the water column in estuaries and other coastal environments requires an input of mechanical energy that is mainly provided by the tides, the wind stress on the water surface and the fresh water runoff. Variations in these three sources are known to have a marked influence on the phytoplankton. At the seasonal scale, river runoff has been identified as an important driving force of phytoplankton dynamics. For example, Gilmartin (1964) has shown that the increased river runoff during the winter in Indian Arm (a fjord of Western Canada) destabilizes the water column which favors the replenishment of the surface mixed layer in nutrients. These nutrients are subsequently used for the initiation of the phytoplankton spring bloom, when the water column stabilizes following the decrease in runoff. At the time scale of a few days, physical transient phenomena (wind storms, periodic upwelling, etc.) associated with the passage of frontal disturbances (Heath, 1973; Walsh et al., 1977) are also strong destabilizing agents of the water column. Iverson et al. (1974), Takashi et al. (1977), Walsh et al. (1978), Walsh (1981) and Legendre et al. (1982) have reported intermittent phytoplankton blooms following stabilization of a water column previously destabilized by strong winds.

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Demers, S., Legendre, L., Therriault, JC. (1986). Phytoplankton Responses to Vertical Tidal Mixing. In: Bowman, M.J., Yentsch, C.M., Peterson, W.T. (eds) Tidal Mixing and Plankton Dynamics. Lecture Notes on Coastal and Estuarine Studies, vol 17. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-4966-5_1

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