In particular, the formation of shocks and the consequent a) departure from local thermal equilibrium, which may be important for baryogenesis, and b) the generation
of vorticity which may be important in the origin of primordial magnetic fields.
Not exact matches
In the study, the research team identified three distinctive characteristic regimes with regard to the degree
of slip at the interface and revealed the underlying molecular mechanisms for each regime: (i) the z - to - x chain rotation mechanism in the
vorticity plane in the weak flow regime,
which effectively diminishes the wall friction against chain movement along the flow direction, (ii) the repetitive chain detachment - attachment (out -
of - plane wagging) and disentanglement mechanism in the intermediate regime, and (iii) irregular (chaotic) chain rotation and tumbling mechanisms in the strong flow regime.
It's always worth remembering that the other end
of the AMOC involves two main factors: (1)
vorticity - mixing
of heat from surface waters into the deep abyssal ocean (
which decreases density causing the Atlantic Deep Water to start rising above the colder Antarctic Bottom Water) and (2) the wind - driven upwelling around the Antarctic Circumpolar Current.
Banded patterns in the relative
vorticity field continued when assessing absolute
vorticity, and even carried through to calculations
of genesis potential index (
which relies on not only absolute
vorticity, but also RH, mixing ratio, and potential intensity in m / s).
Below are animations
of the zonal wind and
vorticity at the level in the model that corresponds roughly to the estimated level
of the cloud tops from
which the observed flows are inferred.
The
vorticity is shown in polar view at the level in the model that corresponds roughly to the estimated level
of the cloud tops from
which the observed flow is inferred (0.75 bar).
This is consistent with regional patterns
of potential
vorticity anomalies,
which, as discussed, may be associated with Rossby wave breaking and western boundary currents.
It works not by spinning in the wind, but by taking advantage
of a phenomenon called
vorticity, or the Kármán vortex street,
which is a «repeating pattern
of swirling vortices.»
These snow bands may emerge as the defining characteristic
of this particular snowstorm,
which is carrying an especially large amount
of «waviness» known as negative equivalent potential
vorticity.