How do you create a model that accommodates years with various combinations
of zonal flow or meridional flow?
The reversed direction
of zonal flow grinds eddies carrying heat and particles, and confinement is improved.
Not exact matches
Zonal flows take the stripe structure that
flows in the opposite direction to each other, and these
flows are known to perform an important role in the suppression
of the turbulence.
Thus instead
of a strong
zonal wind that keeps cold polar air locked in the Arctic, there is a tendency for a less
zonal flow and thus more cold air outbreaks to middle latitudes.
Poleward eddy momentum fluxes interact with the
zonal mean
flow to sustain latitudinal displacements
of the mid-latitude westerlies (Limpasuvan and Hartmann, 2000; Rashid and Simmonds, 2004, 2005).
The discovery by the Juno spacecraft that Jupiter's gravity field is north — south asymmetric5 and the determination
of its non-zero odd gravitational harmonics J3, J5, J7 and J9 demonstrates that the observed
zonal cloud
flow must persist to a depth
of about 3,000 kilometres from the cloud tops6.
MD wave fades moving deeper into SH due to lack
of land mass & land impediment to antarctic circumpolar (southern ocean)
flow --(need midlatitude
zonal land - sea contrast for meridional deflection
of westerlies = differential land - sea equator - pole column - integrated - temperature gradient response to solar forcing, easily measured using a simple wavelet tachometer, which detects externally governed universal constraint)
The sea ice in the Siberian Arctic is peaking, its effect on the meridional temperature gradient strong, promoting increased
zonal flow of large - scale winds, which advect warm air and moisture over the Eurasian continent from the Atlantic and disrupt vertical stratification near the surface and promote high cloudiness, both
of which lead to increasing temperatures — greatest at low altitudes and high latitudes.
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.
Unfortunately, there is actually quite good model agreement on the overall pattern over the East Pacific through the end
of the month: the huge ridge over the Eastern Pacific is expected to persist and perhaps grow even more, continuing the extraordinarily dry pattern over California but allowing for occasionally large swings in temperature as a very cold airmass over Canada is occasionally able to spill westward in weak or even slightly retrogressive (east to west)
zonal flow.
The
zonal velocity is shown 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).
We find robust relationships among seasonal and regional patterns
of weaker poleward thickness gradients, weaker
zonal upper - level winds, and a more meridional
flow direction.
In our paper, we have dealt with the zonally averaged
zonal winds as the mean
flow and excluded from our consideration packets
of quasistationary planetary waves trapped in predominantly meridional elongated waveguides, specifically those originating in the tropics.
Poleward and / or more
zonal jetstreams mean that the troposphere is bit warmer as the rate
of energy
flow through the troposphere increases.
A rapidly warming Arctic leads to a tendency to less
zonal (westerly)
flow and more blocking (or easterly events), which has an impact on western continents
of more cold air in the winter and perhaps more continental droughts in the summer.
Now, as the global trend swings from warming to cooling these winds switched from
zonal to meridional
flow causing dramatic increases in variability
of temperature and precipitation.
This is important because climate change is reflected most in these latitudes as the Circumpolar vortex shifts between
Zonal and Meridional
flow and the amplitude
of the Rossby Waves vary.
The Atlantic Meridional Overturning Circulation (AMOC)-- characterized by warm surface waters
flowing northward and cold deep waters
flowing southward throughout the Atlantic basin — is defined as the
zonal integral
of the northward mass flux at a particular latitude.
Insofar as the New Zealand landmass interrupts what would otherwise be a mainly
zonal flow, it effectively splits it, such that, in general terms, the water
flows in a clockwise direction around the northern half and anticlockwise around the southern half
of New Zealand, and the merged
flow continues eastward.
Two effects are identified that each contribute to a slower eastward progression
of Rossby waves in the upper - level
flow: 1) weakened
zonal winds, and 2) increased wave amplitude.
Persistence
of waves can not only occur with high pressure, but also e.g. with low pressure systems (potentially leading to flooding) or with persistent
zonal flow (supporting the occurrence
of extreme cyclones).
In a new study published in the Journal
of Climate, the Community Earth System Model Large Ensemble (CESM - LENS)
of simulations is used to explore how various characteristics
of the mid-latitude atmospheric circulation (
zonal flow, synoptic blockings, jet stream meanders) evolve along the course
of the 21st century under the RCP8.5 scenario
of anthropogenic emissions.
Figure 2.2 on page 9 shows contour plots
of the perturbation
of the steady state
zonal flow (not shown in published manuscript).
Most
of the time, winds in the atmosphere
flow from west to east; this is called «
zonal flow» and it's responsible for our everyday weather.