«These extra particles may enhance the heterogeneous reactions, leading to ozone destruction, and
this ozone depletion above Antarctica may worsen in 1992 by spreading to altitudes beyond the 12 to 20 kilometres layer.»
In contrast to this, strong
ozone depletion above the Arctic was observed in a few cold winters only.
Not exact matches
The
ozone hole is a severe
depletion of the
ozone layer
above Antarctica that was first detected in the 1980s.
«This year, our balloon - borne instruments measured nearly 100 percent
ozone depletion in the layer
above South Pole Station, Antarctica, that was 14 to 19 kilometers (9 to 12 miles)
above Earth's surface,» said Bryan Johnson, a researcher at NOAA's Earth System Research Laboratory in Boulder, Colorado.
The temperature of the stratosphere is one of the key factors in the springtime
depletion of
ozone above the Antarctic where in winter it gets colder than anywhere else on Earth, encouraging icy particles to form in polar stratospheric clouds.
Chlorine monoxide, which is produced by a similar series of reactions involving icy particles in the stratosphere, is blamed for the springtime
depletion of
ozone above Antarctica.
And
ozone loss
above the Antarctic, where numbing cold creates high - altitude clouds that speed
ozone depletion, remains an intractable challenge.
By 2040 there is not only an
ozone hole
above the Antarctic for the entire year, but severe
ozone depletion at much lower, more populous latitudes.
«This year, our balloon - borne instruments measured nearly 100 percent
ozone depletion in the layer
above South Pole Station, Antarctica, that was 14 to 19 kilometers (9 to 12 miles)
above Earth's surface,» Bryan Johnson, a researcher at NOAA's Earth System Research Laboratory in Boulder, Colorado, said, in the statement.
The team attributes the change to patterns of higher winds, traceable to
ozone depletion high
above Antarctica, and to global warming.
The
above entry is posted under the following topic (s): Atmospheric Chemistry and Composition • Climate Variability and Change • Other • Impacts of
Ozone Depletion •
Less intense
depletion of
ozone occurs
above the Arctic and in mid-latitudes of both hemispheres.
I think her data implies that a more active sun producing more solar protons, in causing more
depletion of
ozone above 45Km, cools the mesosphere thereby enhancing the upward energy flux from stratosphere to mesosphere thus cooling the stratosphere too.
The Shindell and Schmidt abstract
above says: «It has been suggested that both Antarctic
ozone depletion and greenhouse gases have contributed to these trends.»
Satellites and weather balloon measurements show that the stratosphere, the layer from 10 to 50 kilometres
above the Earth, is indeed cooling (although this is partly due to the
depletion of the
ozone layer).