We've used the NASA Goddard Institute for Space Studies (GISS) climate model to examine the impact of a wetter stratosphere on climate and
on ozone over populated areas (this study did not look at polar ozone).
Not exact matches
As Matthew Hoffmann has argued [2], the
ozone negotiations marked a normative shift
over the desirability of universal participation in global environmental negotiations, a shift that was locked into the initial negotiations
on climate change.
In three separate indoor UV chambers, Benca exposed the dwarf pines to 7.5, 10 and 13 times Berkeley's normal UV - B intensity, in line with estimates of the impact Siberian Trap eruptions would have had
on the
ozone layer if their emissions occurred
over various lengths of time, ranging from 400,000 years to less than 200,000 years.
First sighted
over Antarctica in the mid-1980s, the so - called
ozone hole led to an international ban
on CFCs in 1987.
The newly discovered phenomenon
over the South Seas boosts
ozone depletion in the polar regions and could have a significant influence
on the future climate of Earth — also because of rising air pollution in South East Asia.
Senator Tom Carper (DE), top Democrat
on the panel, cited an interview in which Hartnett White suggested that low - level
ozone, an air pollutant, wasn't harmful unless «you put your mouth
over the tailpipe of a car for 8 hours every day.»
Data from observations in Japan itself show that the greatest loss of
ozone — 4.5 per cent
over the past 10 years — occurred
over the city of Sapporo, which lies
on the same latitude as Marseilles.
Between 1969 and 1989
ozone over North America and Europe in the winter - spring season declined
on average by about 3 per cent per decade.
Such a standard would be based
on a cumulative, weighted total of daily 12 - hour
ozone exposures to plants and crops
over a three - month period.
The temperature trends in Antarctica depend
on the time interval and season one looks at, because certain forcings, such as
ozone depletion, are particularly important
over restricted past time intervals and during particular seasons.
Now that we're
on ozone depletion, I read a few years ago that NOx
over mid-latitudes in N. America, due to agriculture (chem fertilizers) & car - driving, was causing a thinning of the
ozone layer.
Images from the latter can show how
ozone amounts differ from season - to - season and how clouds are formed
over volcanoes
on the planet.
And finally, current theories based
on greenhouse gas increases, changes in solar, volcanic,
ozone, land use and aerosol forcing do a pretty good job of explaining the temperature changes
over the 20th Century.
He has published
over 100 articles
on topics including the climatic effects of greenhouse gases, stratospheric
ozone depletion, and small particles.
The debate
over this may rage
on in tiny pockets of the internet (and in some cases in mainstream media), but truthfully «
Ozone» by Geardome skirts awfully close to art and delivers an experience that's complex and dazzling in its execution.
I was the one who first did the long term plot of springtime minimum
ozone values, and this convinced Joe Farman that there really was something going
on over Antarctica.
The optimism is based
on the often forgotten environmental progress and victories that have been achieved
over the past decades, including fixing the
ozone hole, remediation of our rivers and lakes, great improvements in air quality and the rescue of many endangered species.
* The role of the US in global efforts to address pollutants that are broadly dispersed across national borders, such as greenhouse gasses, persistent organic pollutants,
ozone, etc...; * How they view a president's ability to influence national science policy in a way that will persist beyond their term (s), as would be necessary for example to address global climate change or enhancement of science education nationwide; * Their perspective
on the relative roles that scientific knowledge, ethics, economics, and faith should play in resolving debates
over embryonic stem cell research, evolution education, human population growth, etc... * What specific steps they would take to prevent the introduction of political or economic bias in the dissemination and use of scientific knowledge; * (and many more...)
Also, due to the multiplicity of anthropogenic and natural effects
on the climate
over this time (i.e. aerosols, land - use change, greenhouse gases,
ozone changes, solar, volcanic etc.) it is difficult to accurately define the forcings.
There were early bans
on CFC aerosol propellants and actions by environmentalists, together with the predictable opposition of vested interests; but the «tipping point» was the discovery by British Antarctic survey scientists of an «
ozone hole»
over Antartica in October 1984.
But then the other thing going
on is those same protons run to the closing isobars of the earth EMF away from the tropics, and there reduce
ozone, and create
over time a concentration of
ozone over the tropics, thereby increasing the intensity of the ITCZ and increasing tropical storm probabilities, as the wind then wanes under 500.
Warming must occur below the tropopause to increase the net LW flux out of the tropopause to balance the tropopause - level forcing; there is some feedback at that point as the stratosphere is «forced» by the fraction of that increase which it absorbs, and a fraction of that is transfered back to the tropopause level — for an optically thick stratosphere that could be significant, but I think it may be minor for the Earth as it is (while CO2 optical thickness of the stratosphere alone is large near the center of the band, most of the wavelengths in which the stratosphere is not transparent have a more moderate optical thickness
on the order of 1 (mainly from stratospheric water vapor; stratospheric
ozone makes a contribution
over a narrow wavelength band, reaching somewhat larger optical thickness than stratospheric water vapor)(in the limit of an optically thin stratosphere at most wavelengths where the stratosphere is not transparent, changes in the net flux out of the stratosphere caused by stratospheric warming or cooling will tend to be evenly split between upward at TOA and downward at the tropopause; with greater optically thickness
over a larger fraction of optically - significant wavelengths, the distribution of warming or cooling within the stratosphere will affect how such a change is distributed, and it would even be possible for stratospheric adjustment to have opposite effects
on the downward flux at the tropopause and the upward flux at TOA).
As for longer trends, there are of course other factors that could play a role, but you perhaps don't realise that the association of the trends
over the last few decades with human forcings (which include other GHGs, aerosols, land use,
ozone depletion etc.) are not just based
on a correlations.
And then I met Erik Conway, and Erik had made the link to what had happened
over the
ozone hole, and then we started doing research, started digging a little bit, found this link for Fred Seitz back to the tobacco industry, and that I remember very clearly because I remember that day, I called Erik
on the phone and I said, «Erik, we need to write a book.»
«Since they've descended
on this blog to troll, I've found that many of the climate change skeptics here still think that tobacco has no link with cancer, still think that acid rain and the
ozone hole don't exist, and still think that the DDT ban was just «The Man» trying to exert power
over the little guy.
On the onset of spring, when the Sun comes up
over the polar night but the air is still winter - cold,
over the Arctic all conditions can suddenly be met to set the catalytic
ozone breakdown reaction in motion: sunlight, moist, CFKs [yes, they're still around] and temperatures of -90 ºC (or colder).
The Polar Environment Atmospheric Research Laboratory (PEARL) in Eureka, Nunavut, which made key measurements last winter used to detect and analyze the largest
ozone hole ever detected
over the Arctic, will cease year - round operations
on April 30.
, lightning related insurance claims, Lyme disease, Malaria, malnutrition, Maple syrup shortage, marine diseases, marine food chain decimated, Meaching (end of the world), megacryometeors, Melanoma, methane burps, melting permafrost, migration, microbes to decompose soil carbon more rapidly, more bad air days, more research needed, mountains break up, mudslides, next ice age, Nile delta damaged, no effect in India, nuclear plants bloom, ocean acidification, outdoor hockey threatened, oyster diseases,
ozone loss,
ozone repair slowed,
ozone rise, pests increase, plankton blooms, plankton loss, plant viruses, polar tours scrapped, psychosocial disturbances, railroad tracks deformed, rainfall increase, rainfall reduction, refugees, release of ancient frozen viruses, resorts disappear, rift
on Capitol Hill, rivers raised, rivers dry up, rockfalls, rocky peaks crack apart, Ross river disease, salinity reduction, Salmonella, sea level rise, sex change, ski resorts threatened, smog, snowfall increase, snowfall reduction, societal collapse, songbirds change eating habits, sour grapes, spiders invade Scotland, squid population explosion, spectacular orchids, tectonic plate movement, ticks move northward (Sweden), tides rise, tree beetle attacks, tree foliage increase (UK), tree growth slowed, trees less colourful, trees more colourful, tropics expansion, tsunamis, Venice flooded, volcanic eruptions, walrus pups orphaned, wars
over water, water bills double, water supply unreliability, water scarcity (20 % of increase), weeds, West Nile fever, whales move north, wheat yields crushed in Australia, white Christmas dream ends, wildfires, wine — harm to Australian industry, wine industry damage (California), wine industry disaster (US), wine — more English, wine — no more French, wind shift, winters in Britain colder, wolves eat more moose, wolves eat less, workers laid off, World bankruptcy, World in crisis, Yellow fever.
He has published
over 100 articles
on topics including the climatic effects of greenhouse gases, stratospheric
ozone depletion, and small particles.
Tagaris, E., K. Manomaiphiboon, K. J. Liao, L. R. Leung, J. H. Woo, S. He, P. Amar, and A. G. Russell, 2007: Impacts of global climate change and emissions
on regional
ozone and fine particulate matter concentrations
over the United States.
Impacts of global climate change and emissions
on regional
ozone and fine particulate matter concentrations
over the United States
The Hill reports, «Republican lawmakers are planning an all - out assault
on Obama's environmental agenda, including rules
on mercury and other air toxics from power plants, limits
on ground - level
ozone that causes smog, mountaintop mining restrictions and the EPA's attempt to redefine its jurisdiction
over streams and ponds.»
He says that the increased solar brightness
over the past 20 years has not been enough to cause the observed climate changes, but believes that the impact of intense sunshine
on the
ozone layer and cloud cover could be affecting the climate more than the sunlight itself.
Nevertheless, even the potential for drastic
ozone loss is scary enough to warrant a lot more research — and since nobody knows how soon an
ozone hole might open up
over New York or Chicago or Miami, it makes sense to get
on it.
As of this writing, there is observational and modeling evidence that: 1) both annular modes are sensitive to month - to - month and year - to - year variability in the stratospheric flow (see section
on Stratosphere / troposphere coupling, below); 2) both annular modes have exhibited long term trends which may reflect the impact of stratospheric
ozone depletion and / or increased greenhouse gases (see section
on Climate Change, below); and 3) the NAM responds to changes in the distribution of sea - ice
over the North Atlantic sector.
As part of my degree, I completed a project
on changes in surface ultraviolet radiation and
ozone depletion
over Melbourne.
The change in total solar irradiance
over recent 11 - year sunspot cycles amounts to < 0.1 %, but greater changes at ultraviolet wavelengths may have substantial impacts
on stratospheric
ozone concentrations, thereby altering both stratospheric and tropospheric circulation patterns... This model prediction is supported by paleoclimatic proxy reconstructions
over the past millennium.
Over the last 21 years global implementation of the Montreal Protocol
on Substances that Deplete the
Ozone Layer (Montreal Protocol) as successfully phased out the consumption and production of ozone - depleting substances (ODS) by 95 % in developed countries and 50 - 75 % of the ODS in developing count
Ozone Layer (Montreal Protocol) as successfully phased out the consumption and production of
ozone - depleting substances (ODS) by 95 % in developed countries and 50 - 75 % of the ODS in developing count
ozone - depleting substances (ODS) by 95 % in developed countries and 50 - 75 % of the ODS in developing countries.
Drawing
on case studies of past environmental debates such as those
over acid rain and
ozone depletion, science policy experts Roger Pielke Jr. and Daniel Sarewitz argue that once next generation technologies are available that make meaningful action
on climate change lower - cost, then much of the argument politically
over scientific uncertainty is likely to diminish.26 Similarly, research by Yale University's Dan Kahan and colleagues suggest that building political consensus
on climate change will depend heavily
on advocates for action calling attention to a diverse mix of options, with some actions such as tax incentives for nuclear energy, government support for clean energy research, or actions to protect cities and communities against climate risks, more likely to gain support from both Democrats and Republicans.
The second factor is the insulating effect of the atmosphere of which well
over 90 % results from atmospheric water in the form of clouds and water vapour with the remaining 10 % due primarily from CO2 and
ozone with just a slightly detectable effect from methane and a trivial effect from all the other gases named in tyhe Kyoto Accord that is so small it can't even be detected
on measurements of the Earth's radiative spectrum.
On ground level
ozone they say they have a high confidence that the base line will change
over the 21st century from either slightly less to slightly more, but it won't be exactly the same.
Three British scientists shocked the world when they revealed
on May 16th, 1985 — 25 years ago — that aerosol chemicals, among other factors, had torn a hole in the
ozone layer
over the South Pole.
As the Antarctic sea ice reached record levels, scientists floated several hypotheses, including possible changes in the
ozone hole
over Antarctica, or increased amounts of fresh water — which freezes more easily —
on the surface of the ocean around Antarctica.
22
Ozone in the stratosphere filters out much of the harmful ultraviolet radiation from the sun View Figure 25 on page 379 of your textbook In the 1970s scientists noticed that the ozone layer over Antarctica was growing thinner OZONE DEPL
Ozone in the stratosphere filters out much of the harmful ultraviolet radiation from the sun View Figure 25 on page 379 of your textbook In the 1970s scientists noticed that the ozone layer over Antarctica was growing thinner OZONE DEPL
Ozone in the stratosphere filters out much of the harmful ultraviolet radiation from the sun View Figure 25
on page 379 of your textbook In the 1970s scientists noticed that the
ozone layer over Antarctica was growing thinner OZONE DEPL
ozone layer over Antarctica was growing thinner OZONE DEPL
ozone layer
over Antarctica was growing thinner
OZONE DEPL
OZONE DEPL
OZONE DEPLETION
a keep point to think about ------ in winter
over the Arctic ---- there is no sunshine ---- 24 hours a day of darkness ------ so what happens the
Ozone it dissipates during the time period of no sun shine ------ does the lack of
Ozone to harm us ---- as it is not blocking the UV radiation ---- there is no sun shine so all is fine ---- when spring comes and the sun is shining and UV radiation is present ------ guess what ---- the
Ozone is created ---- and blocks the UV radiation -------- this has been going
on for millions of years ---- this yearly cycle
As obvious
on figures 6 - A and 6 - B, Ttop and Ptop are determined by the water vapour that radiates
over some 1900 cm - 1 much more than the 40 cm - 1 of the tropospheric CO2 near 614 cm - 1 and 718 cm - 1.; stratospheric radiation to the cosmos is not very important because the cooling of each layer is exactly equal to its heating mostly by UV absorbed by
Ozone.
As for the
ozone hole
over Antarctica, scientists have only recently started to quantify the impact of
ozone depletion and recovery
on the surface climate.
While the results do not show a significant impact
on human health, especially considering that most of the
ozone loss documented in this study occurs
over the northern polar region, they are important scientifically.
«A lot of impacts
on ozone, like those caused by humans, are very subtle and happen
over long periods of time,» says Jackman.
A satellite view of the status of the
ozone layer
over the Antarctic pole
on Aug. 5.