Antarctic vortex

Antarctic vortex

[ant¦ärt·ik ′vȯr‚teks]
(meteorology)
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The 2018 ozone hole was strongly influenced by a stable and cold Antarctic vortex -- the stratospheric low pressure system that flows clockwise in the atmosphere above Antarctica.
The smaller ozone hole in 2017 was strongly influenced by an unstable and warmer Antarctic vortex - the stratospheric low pressure system that rotates clockwise in the atmosphere above Antarctica.
Brune, "Free radicals within the Antarctic vortex: the role of CFCs in Antarctic ozone loss," Science, vol.
Table 1: Values of criterion PV contour used to define the edge of the Antarctic vortex. Isentropic surface 450 K 500 K 550 K 600 K 650 K Waugh's (PVU) -23.0 -27.0 / -29.0 / Ours (PVU) -23.3 -26.8 -28.8 -31.7 -32.1
The amount of ozone lost so far this year already exceeds the total lost in 1988, a year when several large weather patterns formed in the Southern Hemisphere and disturbed the Antarctic vortex -- a ring of winds circling the pole that seal off the Antarctic stratosphere.
In comparison, the Antarctic vortex is very stable and lasts until the middle of spring.
The method works inside the Antarctic vortex because ozone levels there drop to extremely low values.
In particular, he says, scientists are baffled by a new finding concerning the size of the chemical "reaction vessel.' Researchers who believed that chemistry was the driving force behind the ozone hole had originally assumed that unusual chemical conditions would extend throughout the entire Antarctic vortex. However, says Watson, the aircraft observations revealed that "the area of perturbed chemistry is actually smaller than the area of the classical meteorologic vortex.'