Research led by the Universities of Leicester and Edinburgh and 12 other research institutions show
where surface ozone levels are important for human health.
Not exact matches
I used was the
surface temperature responses from histAll --(histGHG + histNatural) to obtain the response to aerosols +
ozone + land - use and derive the enhancement of the response for that case relative to WMGHGs that I called E. Calculation of TCR based on histAll in a model is approximately the same as calculating the sum of responses to histGHG, histNat, and histInhomogeneous
where the latter includes the factor E.
An example of this kind of surprise happened in relation to the Antarctic
ozone hole,
where unexpected chemistry on
surfaces of ice particles lead to much more efficient destruction of
ozone in the polar vortex than had been expected, making an existing concern into a serious problem.
Scientists believe it is responsible for cooling the stratosphere, the layer of the atmosphere
where the
ozone layer is located, approximately 12.4 miles (20 kilometers) above the Earth's
surface.
Ozone - depleting substances are emitted by human activity at the planet's surface and eventually travel to the stratosphere, where there the chlorine atoms and certain other constituent parts break apart the three oxygen atoms that make up an ozone mole
Ozone - depleting substances are emitted by human activity at the planet's
surface and eventually travel to the stratosphere,
where there the chlorine atoms and certain other constituent parts break apart the three oxygen atoms that make up an
ozone mole
ozone molecule.
The tropopause layer between the troposphere and stratosphere, 8 miles to 11 miles above Earth's
surface, is the point
where water vapor,
ozone and other gases enter the stratosphere.