Impact: Replacing old ozone analyzers at existing stations and adding new sites on the west and east coast of the U.S. would increase the reliability and scope
of surface ozone measurements (which may be impacted by industrial activity in Asia).
Schnell, J.L., M.J. Prather, B. Josse, V. Naik, L.W. Horowitz, P. Cameron - Smith, D. Bergmann, G. Zeng, D.A. Plummer, K. Sudo, T. Nagashima, D.T. Shindell, G. Faluvegi, and S.A. Strode, 2015: Use of North American and European air quality networks to evaluate global chemistry - climate modeling
of surface ozone.
Methane, which is increasing in the atmosphere, contributes to increased ozone globally and will enhance baseline levels
of surface ozone across the United States.
The TOAR database
of surface ozone metrics is now publicly available and can be used by scientists and policymakers around the world to quantify the impacts of ozone on human health and vegetation.
«We created the largest database
of surface ozone from hourly observations at more than 4,800 monitoring sites worldwide, and we're making these data freely available to anyone who wants to investigate the impact of ozone on human health, vegetation, and climate.»
Emissions from vehicles, power plants, industrial operations, and other human activities are a primary cause
of surface ozone, which is one of six main pollutants regulated in the U.S. by the Clean Air Act.
Not exact matches
We can not blow up the world and continue to live on it; we can not destroy the
ozone layer without risking skin cancer; we can not pollute all waters and be able to drink; we can not denude the
surface of trees and expect the soil not to erode.
To address those and other questions, the TOAR research team has produced the first - ever global - scale scientific assessment
of tropospheric
ozone, based on all available
surface observations and the peer - reviewed literature.
One
of the unexpected consequences
of the October 28 flare was a fivefold increase in
ozone - destroying nitric oxide at 70 miles above Earth's
surface.
The European Space Agency's Venus Express spacecraft has detected the spectral signature
of ozone in a thin layer 100 kilometres above the planet's
surface.
The Montreal Protocol — one
of the world's most successful environmental treaties — has protected the stratospheric
ozone layer and avoided enhanced UV radiation reaching the earth's
surface,» said UN Under - Secretary - General and UNEP Executive Director Achim Steiner.
Lu developed «SMOG», short for
Surface Meteorology and
Ozone Generation, as part
of a group led by Richard Turco, head
of the atmospheric chemistry group at UCLA.
For instance,
ozone depletion in the atmosphere occurs because
of chemical reactions
of hydrochloric acid on the
surface of ice crystals and aerosols in the upper atmosphere.
Without the
ozone layer, ultraviolet rays from the sun would reach the
surface at nearly full force, causing skin cancer and, more seriously, killing off the tiny photosynthetic plankton in the ocean that provide oxygen to the atmosphere and bolster the bottom
of the food chain.
Such model included meteorological factors like levels
of aerosols, anthropogenic and biogenic volatile organic compounds (VOCs),
ozone, carbon dioxide, methane, and other items that influence global temperature — the
surface albedo among them.
Over the last 50 years satellite and ground - based records over Antarctica show
ozone column amounts ranging from 100 to 400 Dobson units, which translates to about 1 millimeter (1/25 inch) to 5 millimeters (1/6 inch)
of ozone in a layer if all
of the
ozone were brought down to the
surface.
The large size
of this year's
ozone hole will likely result in increases
of harmful ultraviolet rays at Earth's
surface, particularly in Antarctica and the Southern Hemisphere in the coming months.
In the high atmosphere,
ozone plays a crucial role in shielding the
surface from harmful levels
of ultraviolet light.
For starters, the orbiter beamed back incredibly detailed stereo photos
of the
surface, measured the
ozone distribution in the planet's atmosphere, and confirmed the presence
of water ice at the south pole.
The
ozone concentrations in his measurements remained nearly constantly below the detection limit
of approx. 10 ppbv in the entire vertical range from the
surface of Earth to an altitude
of around 15 kilometres.
On Earth, temperature inversion occurs because
ozone in the stratosphere absorbs much
of the sun's ultraviolet radiation, preventing it from reaching the
surface, protecting the biosphere, and therefore warming the stratosphere instead.
Twenty to 40 %
of ozone coverage might have been lost — in turn, doubling the amount
of UV radiation that reached Earth's
surface, the team reports in a paper in press in Gondwana Research.
Reactions on the
surfaces of these particles then release chlorine, which attacks
ozone.
The nano - catalyst filter uses a technology that decomposes elements
of cigarette smoke using oxygen radical, which is generated by decomposing
ozone in the air on the
surface of the manganese - oxide - based nano - catalyst filter.
In addition, the larger than expected loss
of UV light meant less stratospheric
ozone up to 45 kilometers above the
surface, but more above that line.
She collected pollen and irradiated it in a lab for 3 minutes with UV light, simulating the amount
of UV that can reach the Earth's
surface in Patagonia and other regions in the southern hemisphere under the seasonal
ozone hole.
Because
ozone in the troposphere is a precursor to OH, they deployed weather balloons equipped with measuring devices known as sondes to measure the amount
of ozone in the air from the
surface to the stratosphere.
Earth's
ozone layer, 10 kilometres above the
surface, is produced when light from the Sun interacts with molecules
of oxygen in our atmosphere, and it produces an unmistakable signal that could be detected by JWST.
Scientists at NASA, the National Oceanic and Atmospheric Administration, as well as other international agencies constantly monitor the stratospheric
ozone layer and the levels
of ozone - depleting chemicals at Earth's
surface.
[Peter Cumpson and Naoko Sano, Stability
of reference masses V: UV /
ozone treatment
of gold and platinum
surfaces]
Certain particles may have a damaging effect on the
ozone layer, vital for keeping harmful UV rays away from the
surface of the Earth.
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.
My main problem with that study is that the weather models don't use any forcings at all — no changes in
ozone, CO2, volcanos, aerosols, solar etc. — and so while some
of the effects
of the forcings might be captured (since the weather models assimilate satellite data etc.), there is no reason to think that they get all
of the signal — particularly for near
surface effects (tropospheric
ozone for instance).
The TOAR database contains the world's largest collection
of ozone metrics, calculated consistently from hourly
ozone observations at all available
surface monitoring sites around the globe.
All reported metric values meet a data capture criterion
of > 75 % (TOAR -
Surface Ozone Database).
Consistency for
surface ozone levels was more difficult to achieve due to the influence
of emissions from up - wind regions.
A team
of researchers from the NASA's Jet Propulsion Laboratory in California and the Wageningen University in the Netherlands measured the amount
of ozone between 10,000 and 30,000 feet above the Earth's
surface.
The affected layer
of the atmosphere, high above Earth's
surface, is rich in
ozone.
«The increased use
of clean energy sources that do not emit greenhouse gases or conventional air pollutants... would be doubly beneficial to global food security, as they do not contribute to either climate change or increased
surface -
ozone concentrations,» she said.
No specific mention
of the «volume cold enough for
ozone loss» trend line is made in the Nature text, although it is stated that «Certain clouds in the stratosphere provide
surfaces on which CFC decay products are converted into forms that destroy
ozone â??
By 2060 the
ozone layer is effectively extinct and without it, the Earth's
surface is a much less friendly place: You would only have to be outside for about five minutes to get sunburned and the incidence
of skin cancer would increase substantially.
In the lower stratosphere — closest to the
surface and close to the equator — increased CO2 is slowing the production
of new
ozone, especially in the spring.
What is still contentious is what the result implies for the YD climate change and the megafaunal extinctions, incorporating the ideas
of both the broad large scale cometary debris impact scenario at low grazing angles, and the direct asteroidal impact into water and ice covered
surfaces, and all that implies with the ice sheet disruptions, megatsunamis and the
ozone layer and atmospheric effects and disruption that are possible in these events.
I wonder could that have allowed a great deal
of extra incoming UV - B to warm
surface ozone (both man - made and natural) lending to increased
surface temperatures?
The point being that w / out ongoing decimation from soot, wind,
ozone (
surface ozone pollution that warms from UV), the AO and greenhouse gases, the ice would have been more likely to recover from the impact
of such an event.
With no
ozone, the atmospheric temperature would decrease monotonically, and we would instead have to speak
of cooling
of the «upper atmosphere» in conjunction with the
surface warming due to increasing GHGs.
The lack
of ozone is chilling the middle and upper atmosphere, altering wind patterns in a way that keeps comparatively warm air from reaching the
surface.
The springtime stratospheric
ozone hole &
surface ozone also have an impact, and the combination
of soot &
surface ozone would exceed the impact from greenhouse gases (soot deposition alone is on par with greenhouse gases in the boreal thaw).
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.
Again, no mention
of soot or
surface ozone.