But the warming does not have an immediate effect
on ozone loss and our observations show that ozone loss still continues these days.
But the warming does not have an immediate effect
on ozone loss and our observations show that ozone loss still continues these days.
Not exact matches
Ozone treatment caused no changes in the PLGA and no
loss of function, with cells still able to grow
on the polymer scaffold, as they would in treatments.
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.
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??
He also cautions that the 2005 numbers are still preliminary, however there is a clear trend towards increasing potential for Arctic
ozone loss, which is realised or not depending
on the vagaries of each individual winter.
He also cautions that the 2005 numbers are still preliminary, however there is a clear trend towards increasing potential for Arctic
ozone loss, which is realised or not depending
on the vagaries of each individual winter.
For many decades, the symptoms of unsustainable human exploitation of the natural environment have been mounting: species extinction, the
loss of biodiversity, air and water pollution, soil erosion, acid rain, destruction of rainforests,
ozone depletion - the list goes
on.»
, 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.
It's no surprise the science article titled, «Unprecedented Arctic
ozone loss in 2011» appeared in Nature,
on October 2, 2011.
The potential risks are enormous: disrupting the food chain, damaging the
ozone layer, the
loss of monsoon rains in Asia — the list goes
on.
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.
Speaking
on behalf of the World Meteorological Organization, Braather was keen to stress that this year's Arctic
ozone loss record was not because the Montreal Protocol isn't working.
That growth of sea ice could have potentially been caused by the influx of freshwater as glaciers
on land melted, or from changes in the winds that whip around the continent (changes that could be linked to warming or the
loss of
ozone high in the atmosphere).
But not only must models of
ozone loss and recovery factor in global warming — abnormally low stratospheric
ozone has also a marked effect
on climate change here and now.
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.
The evolution of the forcing due to stratospheric O3
loss hinges
on the rate of recovery of the
ozone layer, with special regards to the spatial structure of such a recovery in the mid - to high latitudes.
It has been suggested that a top - down allocation approach is more appropriate for boundaries where human activities exert a direct impact
on the Earth (that is, climate change, ocean acidification,
ozone depletion and chemical pollution), while a multiscale approach is more appropriate for boundaries that are spatially heterogeneous (that is biogeochemical flows, freshwater use, land - system change, biodiversity
loss and aerosol loading).8 Even with a top - down approach and a single global boundary, however, allocation is fraught with difficult ethical issues.
Geir Braathen, senior scientific officer with the World Meteorological Organization in Geneva, concurs that «scientists have not agreed
on any threshold
ozone loss, like 250 or 260 Dobson units [for a hole].»
What made 2011 different — and a watershed — argues Michelle Santee (a JPL colleague of Manney's and coauthor
on the new paper), is that at long last, «the magnitude of the [Arctic]
loss is comparable to that in the early Antarctic
ozone holes in the mid 1980s.»
Increased water vapor in the stratosphere makes it warmer
on the ground by trapping heat, while the
ozone loss makes it colder
on the ground.
This week, it's a paper
on bromine - and iodine - mediated
ozone loss in marine boundary layer environments (see a good commentary here).