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Shelf-break front

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Shelf-Break Fronts are a process by which stratification of the water column occurs. This stratification normally results in thermoclines, since they occur where a sudden change in water depth causes a constriction of the current flow. They can be expressed as a ratio of their potential energy due to maintaining mixed (non-stratified) conditions, to the dissipated energy produced by the current being forced across the sudden change in depth. This can be expressed as:

${\displaystyle Ratio={\frac {Pot.Energy}{DissipatedEnergy}}}$^[1]

The energy terms can be expressed in very detailed equations, but with constant terms factored out, the important terms are water velocity (average velocity, ${\displaystyle \left\vert {\bar {U}}\right\vert }$) and water depth (h). The equation for the stratification index can be expressed as:

${\displaystyle S=\log _{10}{\frac {h}{C_{D}{\left\vert {\bar {U}}\right\vert }^{3}}}}$^[1]

Where ${\displaystyle C_{D}}$ is a friction coefficient, approximated as 0.003 for a sandy bottom. This index can be calculated for any coastal region, usually in the range of +3 (highly stratified) to -2 (highly turbulent).

The stratification index for a Shelf Break Front is an indication of how productive phytoplankton will be. When the stratification index is approximately 1.5, this produces a nutrient-rich environment for the growth of phytoplankton. Too much higher, and the stratification of the water column will not cause the upwellings of nutrients needed for the phytoplankton to prosper, too much lower, and the water will be too turbulent for the phytoplankton to use the nutrients available. Stability of the front, in addition to nutrients,^[2] is a key to phytoplankton production. An illustration of the stratification index for Narragansett Bay is shown here, with the average speeds estimated, using actual bathymetry for the bay, and an estimated ${\displaystyle C_{D}}$ for silt, which composes much of the bay's bottom. Using the Stokes Spreadsheet,^[3] and some customization on the size of silt particles, I used a ${\displaystyle C_{D}}$ = 0.0011. More accurate speed measurements and detailed ${\displaystyle C_{D}}$ values for the Bay's bottom could yield a higher fidelity image.

Narragansett Bay Stratification Index

Notice the green color (a stratification index of approximately 1.5) along the edges of the Northern Bay and near some of the islands. These areas are favorable to the formation of algal blooms in the Narraganset Bay habitat due to the stratification index being approximately 1.5. Algae have been observed in high concentration in some of these areas, but not all of them.

Using flow cytometry, results ^[5] have determined that the relative abundance of picophytoplankton (<2${\displaystyle \mu }$m), small nanophytoplankton (2 to 10 ${\displaystyle \mu }$m) and large nanophytoplankton (10-20 ${\displaystyle \mu }$m) are greatly affected by the stratification index of the water column. Cell diversity was greatest in the presence of moderate levels of stratification. If the turbulence is too high, their numbers remain stable or fall, but if there is no turbulence, their numbers do fall. It is postulated that the nutrient-rich boundary layer around each phytoplankton cell is not exhausted, but renewed, by this moderate level of turbulence.^[2]