«With our hot, dry summers, we tend to see higher
ozone levels because ozone is formed with a combination of air pollution and sunlight.
Potential study limitations include being geographically confined to Baltimore and the decision to not measure indoor
ozone levels because previous studies found those levels to be low indoors in the city.
Not exact matches
The Antarctic
ozone hole forms and expands during the Southern Hemisphere spring (August and September)
because of the high
levels of chemically active forms of chlorine and bromine in the stratosphere.
Increasing
levels of
ozone, in turn, trap more heat, exacerbating the urban heat island effect: Cities are normally about five to 10 degrees hotter than surrounding suburbs
because asphalt and cement absorb sunlight, generating a vicious cycle of escalating pollution and heat.
Ozone doesn't just live high in Earth's atmosphere; near the ground, it contributes to smog, and ground - level ozone has gradually increased in most places because of industrial pollution from vehicles and fossil - fuel bur
Ozone doesn't just live high in Earth's atmosphere; near the ground, it contributes to smog, and ground -
level ozone has gradually increased in most places because of industrial pollution from vehicles and fossil - fuel bur
ozone has gradually increased in most places
because of industrial pollution from vehicles and fossil - fuel burning.
The findings are timely
because the Environmental Protection Agency is developing stricter regulations for ground -
level ozone, a primary component in photochemical smog.
This is
because warmer temperatures and other changes in the atmosphere related to a changing climate, including higher atmospheric
levels of methane, spur chemical reactions that lead to
ozone.
«Enhanced
ozone production in urban areas is a concern
because of the population size potentially impacted and
because air pollution
levels could be already elevated due to local and mobile sources,» explains Larsen.
The
ozone season is selected
because it is the part of the year with highest temperatures and strongest solar radiation and thus the time when photochemical reactions of
ozone precursor gases are most likely to produce high
ozone levels (Rice, 2014).
NOx emissions can both increase crop growth and diminish it
because NOx gases help catalyze the formation of ground -
level ozone and this gas is toxic to plant life.
China and South Asia, on the other hand, will see the most
ozone - related damage to wheat, rice and soybean crops
because of the chronically high
levels of toxic air pollution.
In addition, ground -
level ozone (O3) and secondary particulate matter are often referred to among the CAC
because they both are by - products of chemical reactions between the CACs that take place in the atmosphere.
Rising
levels of
ozone is a big and growing problem
because it weakens a plant's immune system, producing brown spots on leaves.
Even though the stratosphere has an opposite lapse rate to the troposphere
because of the
ozone absorption, the effect of increasing GHGs is the same, i.e. since it is above the effective radiating
level, it will cool.
Because ozone rapidly decreases with height (very little
ozone above 35 km),
ozone loss is estimated to have caused only half of the cooling at the higher
levels of the stratosphere.
Crops, which tend to be situated in areas with high
ozone levels, would be particularly stunted
because they are fertilized.
In 1990 CO2 accounted for more than 98 % by weight of the total emissions of the five main GHGs (low -
level ozone is not considered here or elsewhere in this sheet
because its impacts, although large, are still difficult to quantify).
An ocean of pure chlorine at sea
level would have zero effect on the
ozone layer,
because it can't get up there.
And
ozone changes are again implicated
because that
level of 50Km is so close to that
level of 45Km (mentioned by Joanna Haigh) where the
ozone reaction seems to change.
Since a sustainable future based on the continued extraction of coal, oil and gas in the «business - as - usual mode» will not be possible
because of both resource depletion and environmental damages (as caused, e.g., by dangerous sea
level rise) we urge our societies to -LSB-...] Reduce the concentrations of warming air pollutants (dark soot, methane, lower atmosphere
ozone, and hydrofluorocarbons) by as much as 50 % [and] cut the climate forcers that have short atmospheric lifetimes.
Levels of protective
ozone are stabilizing
because of the Montreal Protocol.
That increase will have a disproportionately large impact on vegetation
because ozone concentrations in many locations will rise above the critical
level where adverse effects are observed in plants and ecosystems.
A good example is the consensus of chemistry models that projected a slow decline in stratospheric
ozone levels in the 1980s, but did not predict the emergence of the Antarctic
ozone hole
because they all lacked the equations that describe the chemistry that occurs on the surface of ice crystals in cold polar vortex conditions — an «unknown unknown» of the time.