An AVE with a diameter of 200 meters (m) and a height of 50 m to 100 m would produce
a rising air column (the vortex) with a diameter of 30 m extending up to 15 km into the atmosphere.
Not exact matches
In the same process that occurs over Earth's deserts, the
rising cells form spinning
columns while cool
air descends through the middle.
This is because terrestrial hurricanes form when an inflow of
air along the ocean surface sops up moisture and
rises in a halo of updrafts to create towering
columns of rain clouds.
Habib explains that it would have been able to cross broad stretches of ocean by taking advantage of thermals (
rising columns of
air created over warmer - than - normal patches of ocean) to gain altitude, then gliding until it reached the next thermal.
These spinning
columns of dirt can
rise hundreds of feet in the
air.
ACME: Launch Radio sounding balloon to investigate the water vapour in the
air column rising up to the troposphere.
Simply put: There is less
air within the
column of
air that
rises upward from the surface.
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The oily vapour (carrying the «comforting messages»)
rises in a
column of warm
air above the diffuser.
Burnt orange glow observed in the crater of volcano and in thick
column of ash
rising nearly two miles into the
air
Because contraction of the vortex tends to require faster rotation (conservation of angular momentum), which increases centrifugal acceleration, which opposes contraction, it becomes hard for
air to flow in sideways to take the space of warmer
air that is
rising when the
air is spinning; thus, a
rising column of
air can pull up on
air from below.
As the waves
rise, the
air inside each
column (above sea level) is compressed and forced out of a small opening at the top.
The Annual Mean graph shows there is slightly more CO2 near the ground... and levels decrease slightly until you reach 4 km... so it is back to the drawing board... either CO2 sinks because it is heavier than
air and / or near ground CO2 doesn't heat up enough to
rise in the
air column.
The latter results from kinetic energy being converted to potential energy as warm
air rises against the force of gravity in a convective
column.
Stephen Wilde says: July 18, 2013 at 9:17 pm «The latter results from kinetic energy being converted to potential energy as warm
air rises against the force of gravity in a convective
column.»
The solar gain on those
columns of
air can provide up to a 100 degree Fahrenheit
rise in temperature.
This
rising column of
air will soon cool down to the temperature of the surrounding
air and stop
rising unless condensation begins first.
A thunderstorm event might be best depicted as a run - away
rising column of
air that is becoming progressively warmer than the surrounding
air as condensing water vapor yields its heat of vaporization until almost all water vapor has condensed out and then cooling at a rate of 9.8 deg C per 1000 meters, it eventually reaches a warmer layer of
air and spreads out like smoke over a ceiling.
The
rising arrows represent
columns of
air, but I believe the descending arrows represent, by in large, a more diffuse long - term circulation.
Each
column of collector glazing has corrugated aluminum behind it, and as the
air heats up, it
rises naturally.
In a
column of
air under a gravitational field which, unlike our atmosphere, is in thermal isolation, the quicker molecules will tend to
rise higher and lose some of that velocity (or energy) and the slower ones will fall and gain velocity.
That
air would sink and then get pulled under the
rising column of convection, adding more energy.
One interesting question is to what extent they fall in the
rising column and to what extent the end up outside that in drier
air where evaporation occurs rapidly and changes the properties of adjoining
air.
What makes
air rise from the surface when evaporation occurs is increased pressure horizontally which increases buoyancy of the less dense parcel by forcing it upward vertically for a reduction of pressure at the base of the
column.
Thus condensation must result in an increase in surface pressure and if the
rising column of fresh vapour rich
air is continued then the descending
column is displaced to an adjacent location as we see all the time in the real atmosphere.
People here are not distinguishing between localised pressure effects where one parcel of
air abuts another and surface pressure effects as a result of a
rising or descending
column.
Stephen said, «What makes
air rise from the surface when evaporation occurs is increased pressure horizontally which increases buoyancy of the less dense parcel by forcing it upward vertically for a reduction of pressure at the base of the
column.»
Thus there would be no precipitation in the middle of a wide
rising column of moist
air.
The
rising water compresses the
air column above it.
As we get hotter, more megatons of water evaporate and
rise to the top of the
air column, then condense dumping their heat high above the CO2 blocking level letting it rush to space.
Not only bubbles of methane
rising off the sea bottom, but also methane «chimneys» -
columns of potent methane gas that are strong enough that they don't break apart while journeying to the surface but
rise straight up and burst into the
air.