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VATIS Update Ozone Layer Protection is published 6 times a year to keep the readers up to date
of most of the relevant and latest technological developments and events in the field of
Ozone Layer Protection. The Update is tailored to policy-makers, industries and technology
transfer intermediaries. |
Co-Publisher
Ozone Cell
Ministry of Environment and Forests, Govt. of India
Editorial Board
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Cyclic ozone hole proves
cosmic ray theory |
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A scientist from the University
of Waterloo, Canada, says that an observed cyclic hole in the
ozone layer provides proof of a new ozone depletion theory
involving cosmic rays, a theory outlined in his recent study.
Dr. Qing-Bin Lu, a professor of physics and astronomy, said it
was generally accepted for more than two decades that the
Earths ozone layer is depleted by chlorine atoms produced by
the suns ultraviolet (UV) light-induced destruction of
chlorofluorocarbons (CFCs) in the atmosphere. But mounting
evidence supports a new theory that says cosmic rays, rather
than the suns UV light, play the dominant role in breaking
down ozone-depleting molecules and then ozone. Cosmic rays are
energy particles that originate in the space.
In his study, Dr. Lu analyses reliable cosmic ray and ozone
data in the period 1980-2007 which cover two full 11-year
solar cycles. The data unambiguously show the time
correlations between cosmic ray intensity and global ozone
depletion, as well as between cosmic ray intensity and the
ozone hole over the South Pole. This finding not only
provides a fingerprint for the dominant role of the cosmic-ray
mechanism in causing the ozone hole, but also contradicts the
widely accepted photochemical theory, Dr. Lu said. These
observations cannot be explained by the photochemical model.
Instead, they force one to conclude that the cosmic ray
mechanism plays the dominant role in causing the hole.
In the first submission of his paper to Physical Review
Letters in August 2008, Dr. Lu predicted one of the severest
ozone losses in 2008-2009, as a result of the cosmic ray
cycle. His study quantitatively predicted that the mean total
ozone in the October hole over Antarctica would be depleted to
around 187 DU. The latest satellite data sets from the
National Aeronautics and Space Administration (NASA) of the
United States later showed that the mean total ozone in the
ozone hole in October 2008 was 197 DU, within five per cent of
Dr. Lus prediction.
Recent scientific assessments of ozone depletion by the World
Meteorological Organization and the United Nations Environment
Programme, using photochemical models, had predicted that
global ozone will recover (or increase) by 1-2.5 per cent
between 2000 and 2020 and that the Antarctic springtime ozone
hole will shrink by 5-10 per cent between 2000 and 2020. In
sharp contrast, the cosmic ray theory predicted one of the
severest ozone losses over the South Pole in 2008-2009 and
another large hole around 2019-2020.
Source: www.exchangemagazine.com |
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Ozone recovery to be uneven
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In the United States, new
research by scientists from the National Aeronautics and Space
Administration (NASA) and University of Maryland (UM) suggests
that the ozone layer of the future is unlikely to look much
like the past because greenhouse gases are changing the
dynamics of the atmosphere.
Previous studies had shown that while the build-up of
greenhouse gases makes it warmer in troposphere, it actually
cools the upper stratosphere. This cooling slows the chemical
reactions that deplete ozone in the upper stratosphere and
allows natural ozone production in that region to outpace
destruction by chlorofluorocarbons (CFCs). Accumulation of
greenhouse gases also changes the circulation of stratospheric
air masses from the tropics to the poles, NASA scientists
note. In Earths middle latitudes, that means ozone is likely
to over-recover, growing to concentrations higher than they
were before the mass production of CFCs. In the tropics,
stratospheric circulation changes could even prevent the ozone
layer from fully recovering.
Dr. Feng Li, an atmospheric scientist at UMs Goddard Earth
Sciences and Technology Centre and lead author of the study,
says that circulation is just as important as cooling. It is
not one process or the other, but both, he adds. The findings
are based on a detailed computer model that includes
atmospheric chemical effects, wind changes and solar radiation
changes. Dr. Lis experiment is part of an ongoing
international effort organized by the United Nations
Environment Programmes Scientific Assessment Panel to assess
the state of the ozone layer. Dr. Li, working with Dr. Richard
Stolarski and Dr. Paul Newman of NASAs Goddard Space Flight
Centre, found that greenhouse gases alter a natural
circulation pattern that influences ozone distribution. The
Brewer-Dobson circulation is like a pump to the stratosphere,
moving ozone from the lower parts of the atmosphere, into the
upper stratosphere over the tropics. Air masses then flow
north or south through the stratosphere, away from the tropics
towards the poles.
The Arctic would benefit from the surplus ozone in the
northern hemisphere and from the overall decline of ODS to
recover by 2025. The globally averaged ozone and Antarctic
concentrations would catch up by 2040, as natural atmospheric
production of ozone resumes. However, Dr. Lis model shows a
continuing ozone deficit in the stratosphere over the tropics.
In fact, when the model run ended at year 2100, the ozone
layer over the tropics still showed no signs of recovery.
Source: www.sciencedaily.com
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Swedens ozone layer now
thickest in decades
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The ozone layer over Sweden was
thicker in this February than it has been in decades, just a
year after the second-thinnest level was recorded, the Swedish
Meteorological and Hydrological Institute (SMHI) has said.
Measurements taken at SMHIs Norrkoeping station showed the
ozone layer was 426 Dobson units (DU) in February, the
thickest since recordings there began in 1988. At the Vindeln
station in northern Sweden, where measurements began in 1991,
a record high of 437 DU was recorded.
We have to go as far back to the measurements taken in
Uppsala between 1951 and 1966 to find levels that high, SMHI
said in a statement. There, the highest level for February was
in 1957, when a value of 439 DU was recorded.
The circumpolar whirl over the Arctic a polar high-pressure
system formed of a distinct column of cold air that develops
during the long polar night disappeared very quickly in
mid-January, and the stratosphere warmed up quickly in the
space of a few days, SMHI explained. As a result, the low
temperatures that usually cause rapid depletion of the ozone
layer did not take place, it said. The ozone layer over
Sweden usually is at its thickest level during the spring,
before thinning during the summer and reaching a minimum
during the winter, says SMHI.
Source:
www.google.com |
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Model relates South Poles
ozone levels and wind patterns |
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The dominant mode of climate
variability across the Southern Hemisphere is the Southern
Hemisphere Annular Mode (SAM), which describes the strength
of the circumpolar zonal winds. Observations and models have
linked stratospheric polar ozone depletion with trends in
SAM.
However, the general circulation models used in the
Intergovernmental Panel on Climate Change assessment can
only investigate how ozone influences atmospheric
circulation, not vice versa. In the United States,
scientists from Earth System Research Laboratory (ESRL) of
the National Oceanic & Atmospheric Administration and
Goddard Space Flight Centre of the National Aeronautics and
Space Administration analysed records dating from 1962 to
2004 to investigate the two-way ozone-SAM relationship. They
found a significant correlation between the austral spring
total column ozone above the South Pole and SAM, with delay
times of up to four months.
The austral spring SAM is also linked to polar ozone
concentrations into the early summer. The ozone-SAM
relationship is then investigated in a coupled chemistry
climate model (CCM). Led by Dr. Ryan L. Fogt of ESRL, the
scientists have shown that the observed relationship can be
represented in the CCMs, suggesting CCMs are important tools
to investigate future Southern Hemisphere climate change
involving ozone recovery and greenhouse gas increases.
Source:
www.sciencemode.com |
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Rocket launches may need
regulation to prevent ozone loss |
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The global market for rocket
launches may need more stringent regulation in order to
prevent significant damage to Earths stratospheric ozone
layer in the decades to come, according to a new study by
researchers in the United States. Future ozone losses from
unregulated rocket launches will eventually exceed ozone
losses due to chlorofluorocarbons (CFCs), said Dr. Martin Ross
from The Aerospace Corporation and the chief author of the
study. The study, with participation from the University of
Colorado at Boulder (UCB) and Embry-Riddle Aeronautical
University, provides a market analysis for estimating future
ozone layer depletion based on the expected growth of the
space industry and known impacts of rocket launches.
If left unregulated, rocket launches by the year 2050 could
result in more ozone destruction than was ever realized by
CFCs, warned Prof. Darin Toohey of UCBs atmospheric and
oceanic sciences department. Since some proposed space efforts
would require frequent launches of large rockets over extended
periods, the new study was designed to bring attention to the
issue in the hope of sparking additional research.
Current global rocket launches deplete the ozone layer by no
more than a few hundredths of 1 per cent annually, said Prof.
Toohey. But as the space industry grows and other
ozone-depleting chemicals decline in the Earths stratosphere,
the issue of ozone depletion from rocket launches would move
to the forefront. Just a handful of space shuttle launches by
the United States National Aeronautics and Space
Administration release more ozone-depleting substances in the
stratosphere than the entire annual use of CFC-based medical
inhalers used to treat asthma and other diseases in the United
States and which are now banned, said Prof. Toohey.
Highly reactive trace-gas molecules known as radicals dominate
stratospheric ozone destruction a single radical in the
stratosphere can destroy up to 10,000 ozone molecules.
Microscopic particles, including soot and aluminium oxide
particles emitted by rocket engines, provide chemically active
surface areas that increase the rate such radicals leak from
their reservoirs and contribute to ozone destruction, said
Prof. Toohey.
The research team is optimistic that a solution to the problem
exists. We have the resources, we have the expertise, and we
now have the regulatory history to address the issue in a very
powerful way, he said.
Source:
www.sciencedaily.com
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