Clearly recognizable is the prograde (superrotating)
equatorial jet and alternating off - equatorial jets.
Also recognizable are Rossby wave packets especially on
the equatorial jet, with retrograde propagation and phase lines that have the characteristic chevron shape indicating angular momentum transport into the jet, as is observed to occur.
They discovered
an equatorial jet in the wind velocities based on image data from July 2016 and that the jet existed at least two months after that.
«Although it remains unclear why such
an equatorial jet appears, the mechanisms that could cause it are limited and related to various theories about superrotation.
Observations by Japan's Venus climate orbiter Akatsuki have revealed
an equatorial jet in the lower to middle cloud layer of the planet's atmosphere, a finding that could be pivotal to unraveling a phenomenon called superrotation.
«
Equatorial jet in Venusian atmosphere.»
This shift is caused by
an equatorial jet with dramatically variable wind - speeds — at their fastest, pushing vast amounts of cloud across the planet.
The study by the Planetary Sciences Group reports that this gigantic storm is another of the agents of change in
the equatorial jet stream.
«Peculiarities of huge
equatorial jet stream in Saturn's atmosphere revealed.»
Liu, J., and T. Schneider, 2015: Scaling of off -
equatorial jets in giant planet atmospheres.
Not exact matches
near the
equatorial regions, as the
jet stream model predicts.
Changes in climate can cause the polar
jet stream — the boundary between the cold North Pole air and the warm
equatorial air — to migrate south, bringing with it cold, Arctic air.
The suspected companion star also might be responsible for a pair of high - speed
jets of gas that lie at right angles to this
equatorial ring.
The
equatorial dash vent mixes horizontal and vertical air
jets to precisely angle the flow as you desire, controlled by moving a dot on a crosshair on the touchscreen.
The Paramagnetic Oxygen Transport Thesis explains the failure of Brewer - Dobson
equatorial ozone formation, the Ozone Hole in 1983, continued Antarctic cold temps concurrent with Arctic warming, mid-latitude ozone formation which accelerates
jet streams and elongates Rossby wave loops, and wandering magnetic poles which control extreme weather and climate change.
Schneider, T., and J. Liu, 2009: Formation of
jets and
equatorial superrotation on Jupiter.