Changes in polar
vortex winds high in the stratosphere can alter the global conveyor belt of ocean circulation.
Not exact matches
Water heats more slowly than land, creating pressure differences that drive
high - speed
winds; fast - burning fires spawn flame - breathing
vortices; the pressure waves of a plane on takeoff transform water into ice.
Colder temperatures and weaker
high - altitude
winds may make the arctic polar
vortex even more intense in future winters and trigger greater ozone loss, says atmospheric scientist Paul Newman of NASA's Goddard Space Flight Center in Greenbelt, Maryland, although the losses probably won't approach those in Antarctica.
The model also predicts a radial flow, which sucks
winds from the
high - speed jet streams toward the
vortex center.
Wind vortices blowing across the crater slowly formed a radial moat in the sediment, eventually leaving only the off - center Mount Sharp, a 3 - mile -
high peak similar in height to the rim of the crater.
Material from both eruptions was unable to penetrate the Antarctic stratosphere at
high altitudes last year because the eruptions occurred after the establishment of the winter
vortex of circumpolar
winds, which cuts off the upper stratosphere above Antarctica.
Normally, cold air is kept locked up in the Arctic by a spinning
vortex of air bounded by fast
winds high in the atmosphere called the jet stream.
This phenomenon, called von Kármán
vortex shedding, affects any elongated structure caught in
wind or water currents such as lampposts,
high rises and the long vertical pipes used for drilling oil at sea.
For one thing there has been a noticeable expansion of the great belt of dry,
high - altitude polar
winds — the so - called circumpolar
vortex — that sweep from west to east around the top and bottom of the world.»
It was determined that a major cause of changes in the size and extent of the Antarctic ozone hole are the intense
wind patterns and circulations associated with the extensive Antarctic
high - pressure zone and the surrounding
wind pattern known as the Circumpolar
Vortex.
«In winter, the freezing Arctic air is normally «locked» by strong circumpolar
winds several tens of kilometers
high in the atmosphere, known as the stratospheric polar
vortex, so that the cold air is confined near the pole,» said study co-author Marlene Kretschmer from the Potsdam Institute of Climate Impacts Research in Germany, in a press release.
These are both complex phenomena, but a sudden stratospheric warming event typically occurs when energy from the lower atmosphere travels upwards, and this can disrupt the area of low pressure and
high westerly
winds that comprise the polar
vortex.
At times of
high winds speeds, the
vortex may be «blown away» and de-stabilised but power would be adequate in any case.
If the
wind field contains energy at the inertial frequency or
higher (daily and six - hourly cases), then
Vortex Rossby waves and near inertial waves are excited as ageostrophic expression of the vigorous eddy field.