By assigning varying values for wind stress and surface heat flux, they were able to develop parameterizations for mixing depth and turbulent diffusivity using the LES model, and apply them to a phytoplankton model to monitor the response.
32.
A strong seasonality is also observed with respect to the remote, North Pacific influence in the tropical Atlantic, via ENSO events that induce western equatorial wind stress anomalies ( WEA ), which in return modulate the tropical Atlantic ocean-atmosphere dynamics.
33.
When the isle's red cedars proved too gnarled and knotty from salt and wind stress to be turned into pencil slats, he had the vision to secure it as a family retreat and, as much as possible, leave it be.
34.
Where h is the upper-layer thickness anomaly, ? is the wind stress, c is the Rossby wave speed that depends on latitude, ? 0 is the density of sea water and f 0 is the Coriolis parameter at a reference latitude.
35.
During anticyclonic regimes where the wind stress curl is negative freshwater is pumped into the Beaufort Gyre; during cyclonic regimes where wind stress curl is positive freshwater is released into the Arctic Ocean, where it can then flow into the North Atlantic.
36.
During anticyclonic regimes where the wind stress curl is negative freshwater is pumped into the Beaufort Gyre; during cyclonic regimes where wind stress curl is positive freshwater is released into the Arctic Ocean, where it can then flow into the North Atlantic.
37.
The maximum in freshwater content released into the ocean waters coincides with a maximum in wind stress curl ( i . e ., a minimum in Ekman pumping ), allowing for a high volume of freshwater to seep into the Arctic Ocean circulation.
38.
This form of wind stress causes hanging traffic lights to blow a foot or more up and down in the air, occasionally cartwheeling over and over, and, rarely, to crash down onto the streets below, becoming lethal at worst and useless at best.
39.
During April and May when the SST front is still strong, the seasonal warming makes the region conductive to atmospheric convection, and surface wind stress curls turn weakly positive along the front on the background of negative curls that drive the subtropical gyre.
40.
The result is that the models have very different wind stresses over the Southern Ocean, with the CM2.0 exhibiting the common bias of winds that are shifted equatorward but the CM2.1 model being one of the few that have winds close to the correct latitude and magnitude in this region ( Russell et al ., 2006 ).
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