In their prediction of future climate, many IPCC models did not consider
the expected ozone recovery and its potential impacts on climate change.
Not exact matches
As things stand, scientists
expect the first signs of
recovery of springtime
ozone depletion in the polar stratosphere around the year 2065.
Worldwide bans on the worst
ozone depleting chemicals has halted growth of
ozone depletion, after years of worsening, and signs of
recovery are
expected to become statistically detectable in the next several years.
Continued monitoring and process studies of
ozone and
ozone - depleting gases are required if we hope to be able to discern if the
ozone layer is recovering as
expected, or whether additional actions are necessary to ensure the
recovery of the
ozone layer.
As a result of these activities, NOAA has led the effort to guide the
recovery of the
ozone layer, to ensure the
recovery proceeds as
expected, and to note areas or action that might allow a faster
recovery or hinder
recovery.
Continued declines in
ozone - depleting gases are
expected to allow for a
recovery of the
ozone layer, but not until the middle of the 21st century.
Continued monitoring of
ozone and
ozone - depleting substances is essential for verification of
ozone layer
recovery as
expected by about 2050, which hinges on the complete elimination of atmospheric
ozone - depleting substances.
Opposite signed trends in the Southern Hemisphere middle latitude jetstream are
expected in response to the
recovery of the Antarctic
ozone hole (Son et al., 2010; Arblaster et al., 2011; Polvani et al., 2011).
On top of the additional contraction
expected from
ozone recovery, this suggests that the rapid pace of Hadley Cell expansion observed since 1980 will likely not be maintained through the first half of the 21st century.
Ozone recovery in the tropical stratosphere is expected to be faster and the recovery of the polar ozone hole is expected to be slower because of the CO2 - induced cooling of the stratosphere (and increase the number of polar stratospheric clo
Ozone recovery in the tropical stratosphere is
expected to be faster and the
recovery of the polar
ozone hole is expected to be slower because of the CO2 - induced cooling of the stratosphere (and increase the number of polar stratospheric clo
ozone hole is
expected to be slower because of the CO2 - induced cooling of the stratosphere (and increase the number of polar stratospheric clouds).