Introduction
My long term objectives are to improve our understanding and ability
to quantitatively measure ocean mixing. The ocean is affected by
mixing in at least two ways:
1. Climate. The "global ocean conveyor
belt" transfers warm low-latitude waters to higher latitudes where the
heat is released, cooling the tropics and warming the temperate
zones. Due to the high heat capacity of water, the upper 1 m of ocean
carries about the same heat energy as the entire atmosphere, so that
heat storage and transport by the ocean controls climate, particularly
in maritime areas. The oceanic poleward heat flux and the timing of
ocean response to atmospheric warming are both very sensitive to rates
of ocean mixing (Solokov and Stone, 1998) such that the uncertainties
in mixing are comparable with other uncertainties involved in climate
prediction.
2. Ecological health. The ocean recycles and stores nutrients that
supply the growth of marine phytoplankton, which "...generate roughly
half the planetary primary production, affect the abundance and
diversity of marine organisms, drive marine ecosystem functioning, set
upper limits to fishery yields", and "...influence climate processes
and bio-geochemical cycles." (Boyce et al, 2010). Ocean mixing
modulates the supply of nutrients to the photic zone, and controls the
upper ocean density stratification that supports phytoplankton
growth. Recent observed declines in ocean health (DFO, 2010) have a
variety of likely causes, but may originate in part from the
global-scale decline in phytoplankton abundance noted by Boyce et al
(2010).
Ocean mixing is driven by several physical ocean processes that
receive energy from large scales and use that energy to drive
turbulent mixing: internal waves, thermohaline intrusions, and shear
instabilities, to name a few. We quantify the present rate of ocean
mixing by directly measuring turbulence (Oakey, 1982, Ruddick, Anis
and Thompson, 2000), but the only way to predict the changes in ocean
mixing due to upcoming changes in our ocean climate is via
observational process studies and models that link ocean turbulence to
larger scale phenomena such as thermohaline intrusions (Ruddick,
Oakey, and Hebert, 2010). In addition to using laboratory tank
experiments to simulate ocean mixing processes, my colleagues and I
are developing new ways to visualize and understand mixing processes,
using sound, billions of tiny tracer particles, and laser beams.