The effect of
baroclinicity on the wind in the planetary boundary layer.
In the future, as a result of decreasing
baroclinicity, the importance of large-scale precipitation might decline.
Although high-resolution wind data are not available, presumably the kinematics of the sea-breeze circulation was predominantly forced by the larger-scale mesoscale
baroclinicity rather than the microscale surface variations.
Researchers suspect they may be part of the reason why a storm becomes tornadic while in other conditions with the same shear and instability, no tornado occurs, as they provide microscale "
baroclinicity" to the storm.
In the case of the zonally averaged observables, we obtain weak autocorrelations and fast convergence to [[xi].sub.[delta]] in the middle of the channel where the
baroclinicity is the strongest, versus high autocorrelations and slow convergence at the margins of the channel, where instead the
baroclinicity is weak.
The effect of Gulf Stream-induced
baroclinicity on U.S.
Specifically, there was low-level
baroclinicity evident over the four state region, and a low-level trough over the Rockies.
1) The barotropic motion was studied in the previous experimental runs, whereas the role of the
baroclinicity is still open to question.
While most meteorologists will agree on a list of essential front characteristics (e.g., enhanced
baroclinicity, anomalous relative vorticity, and static stability), historic debate has shown that we must accept a certain degree of freedom in the practical definition of a front.
Section 3 describes the climatological differences in precipitation, lower-tropospheric
baroclinicity, and synoptic-scale cyclone activity between the experiments with and without modified topography.
The ACRE-induced increases in the vertical flux of wave activity are consistent with enhanced upper-tropospheric
baroclinicity and baroclinic wave amplitudes.
According to the study, the
baroclinicity during Changma periods is strengthened compared to the whole summer, being associated with the occurrence of the Changma front and the main portion of precipitation over the Korean Peninsula is accompanied with enhanced
baroclinicity north of the rainfall area.