1.3.2. Ozone
WHO
states: "Chamber studies may
show thresholds
for mean effects of ozone on lung
function and airway $ but a few individuals
show these responses below these levels.
As mentioned previously, a particular
threshold in a particular experimental
situation does not necessarily contradict
a finding of effects below these levels
in other situations.
The time-series results
often have insufficient data to distinguish
between a linear and non-linear model
with confidence. In addition, the statistical
analyses applied to investigate thresholds
in datasets on particles have not been
applied to the same extent to datasets
on ozone. There remain uncertainties in
interpreting the shape of exposure-response
relationships in epidemiological studies
due to different patterns of confounding
by other pollutants and correlations with
personal exposure across the range of
ozone concentrations. Although there is
evidence that associations exist below
the current guideline value, our confidence
in the existence of associations with
health outcomes decreases as concentrations
decrease.
The answer and rationale
refer to acute effects of ozone, as this
is most important for health impact assessment
of the effects of ozone.
Rationale:
Clinical experimental
studies
Experimental clinical studies have the
advantage that it is possible to set experimental
conditions to test a specific hypothesis.
Particular subject groups can be selected
(provided ethical considerations are met),
ozone can be studied without the presence
of other pollutants and ozone concentrations
can be experimentally controlled. These
studies may give clearer information about
a threshold
for a specific measure of effect in particular
circumstances. Such results can be used
to test conclusions from other studies
such as ecologic air pollution studies.
However, the applicability of this information
to the whole of the general population
is limited as the studies usually have
a small sample size and only study healthy
or mildly ill subjects and milder health
outcomes.
Human clinical studies
do not provide convincing evidence for
an absolute level below which no effects
are observed. There is evidence that prolonged
(6.6 hours) single exposures to ozone
at concentrations of 160 µg/m3
(80 ppb), with prolonged “moderate”
exercise, cause decrements in pulmonary
function, airway injury, and increased
non-specific airways responsiveness. Although
the magnitude of the mean effects at this
exposure level is generally small, some
individuals show clinically important
responses.
McDonnell et al. (1995)
developed a predictive model for changes
in the forced expiratory volume in 1 second
(FEV1) based on the 6.6-hour ozone exposure
studies performed by the US Environmental
Protection Agency. This model found that
the lowest level of exposure, expressed
as concentration x time for which the
90% confidence interval excluded 0, was
0.4 mg/m3-hour (0.2 ppm-hour).
This model suggests that significant declines
in FEV1 would be seen with exercising
exposures to ozone concentrations of 400
µg/m3 (200 ppb) for one
hour, or 50 µg/m3 (25
ppb) for eight hours. This result is consistent
with the epidemiological and panel studiesfinding
effects on lung
function with ozone concentrations
below the WHO Air Quality Guidelines of
120 µg/m3 (60 ppb) for
eight hours.
It must be kept in mind
that human subjects show highly variable
responsiveness to ozone effects (see also
answer to Question 3). This may be the
result of genetic differences as described
in the epidemiological studies section
below. Clinical studies have generally
used relatively small numbers of unselected
subjects. Relying on mean changes for
the whole subject group may underestimate
the clinical significance of larger changes
in a small number of subjects. If a clinical
study were to be performed with pre-selected
“responders” to ozone, in
terms of pulmonary function, it is likely
that the observed response thresholds
for such groups are lower than that for
a healthy, unselected group. Thus the
human clinical data on lung
function changes are not sufficient
to indicate a threshold below which no
effects are expected to occur for all
people.
With regard to indices
of airway inflammation
and injury, fewer data are available than
for the studies of lung
function effects. However, the report
by Devlin et al. (1991) shows that 6.6
hours of exposure, with exercise, to 160
µg/m3 (80 ppb) ozone
caused statistically significant increases
in inflammatory cells in bronchoalveolar
lavage fluid, and increases in indicators
of epithelial injury. The degree of change
was less than that generally seen with
higher concentrations, and some significant
changes at higher concentrations were
not seen with exposure to 160 µg/m3.
However, two study subjects exposed to
160 µg/m3 ozone experienced
greater than 10-fold increases in polymorphonuclear
leukocytes in bronchoalveolar lavage (BAL)
fluid, suggesting an increased sensitivity
to ozone inflammatory effects in these
subjects. It is possible that the effect
threshold
for inflammatory changes in such sensitive
subjects may be well below 160 µg/m3.
Epidemiological studies
Observational epidemiological studies
examine whole populations including susceptible
groups (even if these are unidentified).
However, as the population is being observed
in real life, it is not possible to choose
perfect experimental conditions. The ideal
case where only the ozone concentration
is changed is not possible because, in
actuality, changes in ozone concentrations
occur at the same time as changes in the
weather and concentrations of other pollutants.
In addition, the study has to work with
whatever range of ozone concentrations
happen to occur in a particular place.
Time-series results often
have insufficient data to distinguish
between a linear and non-linear model
with confidence. This can result from
factors including too few data points
overall, too few data points near a possible
threshold and a restricted range of data.
It is possible to perform a statistical
test for any significant deviation from
linearity but this has only been performed
in a minority of studies on ozone (e.g.
Schwartz et al., 1994; Hoek et al., 1997).
In addition, the sophisticated statistical
analyses applied to specifically address
the question of thresholds in datasets
on particles (e.g., Daniels et al., 2000)
have not been applied to datasets on ozone
to the same extent. A recent paper (Kim
et al., 2004) applied a linear model,
a natural spline model and a threshold
model to a dataset in Seoul and found
that the threshold model, with a threshold
at 56 µg/m3 (28 ppb)
1 hour average, gave the best fit. However,
the slope above the threshold was steeper
than in the linear model so the threshold
model did not necessarily predict a lower
health impact. Further studies of this
type are needed. Currently, many studies
on ozone do not explicitly describe the
shape of the exposure-response function
at all.
The atmospheric chemistry
of ozone has some unique features which
make the interpretation of the shape of
exposure-response relationships particularly
complex. Formation of ozone is temperature-dependent
so that the high end of the exposure-response
relationship will be based on hot sunny
summer days and the lower end on winter
days. Unfortunately, this may mean that
factors other than the ozone concentration
are varying across the range of the exposure-response
relationship. For example, it is known
that ozone is often positively correlated
with particles in the summer and negatively
correlated with particles in the winter
(Sarnat et al., 2001). Ozone can be particularly
low in cold inversion conditions when
other pollutants accumulate. As these
other pollutants can have the same health
effects as ozone, this can give the perverse
impression that health effects increase
(or fail to drop) as ozone concentrations
decrease. This may appear to suggest a
change in slope in a single pollutant
model exposure-response relationship that
does not truly reflect the effect of ozone
itself. Although the use of multi-pollutant
models may help to disentangle this somewhat,
there may be other factors involved as
well. For example, variations in the total
oxidant burden in the different polluted
environments in which ozone occurs may
influence the health response to ozone.
Ozone levels are very
low indoors. This means that people’s
exposure to ozone varies according to
how much they are outdoors. It is likely
that people spend less time outdoors on
the winter days contributing to the lower
end of the exposure-response relationship
– another factor complicating interpretation.
The low level of ozone indoors means that
personal exposure to ozone and ambient
concentrations of ozone are not well correlated
(Sarnat et al., 2001; Avol et al., 1998).
Brauer et al. (2002) demonstrated, using
simulations, that surrogate metrics that
are not highly correlated with personal
exposures obscure the presence of thresholds
in epidemiological studies of larger populations.
This would apply when ambient ozone concentrations
are used as a surrogate for personal exposure
to ozone.
Bearing in mind the above
difficulties in interpretation, individual
studies that examined the shape of exposure-response
relationships are described below. Emphasis
is given to studies on all cause mortality,
respiratory hospital admissions and respiratory
symptoms, the endpoints
most likely to be used in health impact
assessment. Panel studies that examine
effects on lung
function at a similar range of ozone
concentrations are also considered as
these may lend plausibility to the occurrence
of the other health outcomes in the same
range.
Several studies of ozone
and all-cause mortality in single pollutant
models suggest thresholds at 40 to 100
µg/m3 (20–50 ppb)
8 hour average (Anderson et al., 1996;
Hong et al., 1999; Wong et al 2001); 50
µg/m3 to less than 120
µg/m3 1 hour average
(Kim et al., 2004; Simpson et al., 1997;
Morgan et al., 1998/2002) or 36 to 50
µg/m3 24 hour average
(Diaz et al., 1999; Goldberg et al., 2001).
Morgan et al. (2002) found a linear association
when using the GAM rather than GEE model.
Galan Labacca et al. (1999) found a U-shaped
relationship and Toulomi et al. (1997)
found a flatter slope at high concentrations.
However, for the reasons given in the
paragraphs above, it may not be possible
to take these shapes at face value.
Fairley et al. (2003)
found a suggestion of a stronger relationship
of all cause mortality with daily ozone
ppb-hours above 120 µg/m3
after adjustment for PM2.5.
Kim et al. (2004) found that there was
a steeper slope above 52 to 56 µg/m3
1 hour average in several different multi-
pollutant models. Although Moolgavkar
et al. (1995) only found a significant
association, adjusted for SO2
and TSP, in the highest quintile (above
96 µg/m3 24 hour average),
there was a linear increase across quintiles.
Borja-Aburto et al. (1997) found no relationship
after adjustment for TSP. Only Hoek et
al. (1997) used a multi-pollutant model
(with TSP/24 hour average ozone and a
formal test for non-linearity –
the test for non-linearity was not significant.
The relative risk remained similar even
after all days above 40 µg/m3
ppb 24 hour average were removed.
For single pollutant models
of respiratory hospital admissions, Ponce
de Leon et al. (1996) found a suggestion
of a threshold
around 100 µg/m3 8 hour
average; Thurston et al. (1994) found
increased relative risks in the two upper
quartiles above 90 µg/m3
1 hour average and Schwartz et al. (1994)
found an increase in risk above 50 µg/m3
24 hour average. Other studies found a
flat association (Atkinson et al., 1999,
8 hour) or a linear association (Burnett
et al., 1994; Burnett et al., 2001, 1
hour). Burnett et al. (1997) found an
upturn at 50 µg/m3 12-hour
average but a chi- squared test for non-linearity
was not significant. None of the studies
examined the shape of the exposure-response
in a multi-pollutant model.
Mortimer et al. (2002)
found that a significant association with
lower
respiratory symptoms remained below
160 µg/m3 8 hour average.
This was also found for an asthma
symptom score although only in asthmatics
not on medication (Delfino et al., 1998).
Schwartz et al. (1994) found a flattening
of the relationship with lower respiratory
symptoms above 80 µg/m3
24 hour average but considered this implausible
shape was due to confounding. The relationship
for cough, after control for PM10,
was linear (p=0.31 in test for non-linearity).
Thurston et al. (1997) (1 hour) and Ostro
et al. (1993) (1 hour) also found linear
relationships.
Several panel studies
of lung
function have used censoring of days
above a certain concentration to investigate
thresholds. Higgins et al. (1990) found
no significant effect on lung function
in children after removal of days above
about 240 µg/m3 1 hour
average, although there are many studies
which have shown effects on lung function
below this level. Spektor et al. (1988)
found a significant association with lung
function in active children remained after
removal of all days above 120 µg/m3
1 hour average. Brunekreef et al. (1994)
found that, in vigorously exercising cyclists,
significant associations with lung function
remained after removal of all days above
100 µg/m3 1 hour average
but became non-significant after removal
of all days above 80 µg/m3.
Similarly, Brauer et al. (1996) found
a significant association with lung function
was maintained in active farm workers
with removal of all days above 80 µg/m3
1 hour average but not with removal of
all days above 60 µg/m3.
It should be noted that censoring days
above a certain concentration also involves
reducing the total days in the analysis
and thus a loss of statistical power.
This may itself result in a loss of statistical
significance.
Bergamaschi et al. (2001)
found a linear relationship (R2=0.484)
between 2 hour average ozone in the range
60 to 220 µg/m3 and changes
in serum CC16 (a marker of increased epithelial
permeability) in subjects with wild type
NADPH quinone reductase and null glutathione-S-
transferase μ1. This was not found
in subjects bearing other genotypes. (The
former genotype is a proposed susceptible
group in terms of oxidative stress). Correlations
with decreased FEV1 and the forced expiratory
vital capacity (FVC) were also found mainly
in this susceptible group. This genotype
is present in 30% of the population. Other
candidates for genetic susceptibility
to ozone, from evidence in mice, include
the tumour necrosis factor Tnf and toll-like
receptor 4 Tlr4 gene (Kleeberger et al.,
2001). In communities with the lowest
ozone concentrations, variant TNF genotypes
were associated with a higher risk of
wheezing outcomes (Gilliland et al., 2003).
Thus, there are indications that subjects
with particular genotypes are responding
to ozone at lower concentrations than
the general population. This needs to
be taken into account when considering
thresholds.
Several studies have compared
associations with ozone by season and
often find greater associations in the
summer when ozone levels are higher (e.g.
Anderson et al., 1996; Simpson et al.,
1997; Sunyer et al., 1996). This might
appear to provide support for a threshold.
However, the studies often divide the
year into two six month periods for which
the ozone concentrations overlap for the
majority of the exposure range (e.g. Simpson
et al 1997). In other studies (e.g. Sunyer
et al., 1996 in Barcelona), the ozone
range in winter/spring is no lower than
the full year range in other places where
significant associations have been found
such as London (Anderson et al., 1996).
Hoek et al. (1997) adjusted for TSP and
did not find a greater association of
all- cause mortality with 24 hour average
ozone in the summer. In contrast, Moolgavkar
et al. (1995) with a good contrast in
24 hour average ozone concentrations and
adjustment for
sulphur dioxide and TSP did find a
greater association in the summer. The
non-significant associations found in
many studies in the cool season may be
due to the different patterns of confounding
by other pollutants, of personal exposure
and of the chemistry of the polluted environment
in different seasons, rather than to the
small differences in ozone concentrations.
Seasonal differences may therefore be
less informative about thresholds than
might be expected.
Another approach is to
examine the results from places where
ozone concentrations are low (<160
µg/m3 8 hour average
or <180 µg/m3 1 hour
average). Although not all studies show
significant associations (Bremner et al.,
1999; Zmirou et al., 1996; Hong et al.,
1999), positive and significant associations
with all-cause mortality have been found
in Brisbane with a maximum ozone concentrations
of 126 µg/m3 8 hour average
(Simpson et al., 1997), in Vancouver with
maximum ozone concentration of 150 µg/m3
1 hour average (Vedal et al., 2003) and
in London with a maximum ozone concentration
of 148 µg/m3 8 hour average
(Anderson et al., 1996). These associations
were stable to adjustment for other pollutants.
Some studies have found
positive and statistically significant
associations with respiratory hospital
admissions, for example, in Brisbane with
a maximum 8 hour average concentration
of 130 µg/m3 (Petroeschevsky
et al., 2001) and in London with a 95th
percentile 8 hour average concentration
of 74 µg/m3 (Ponce de
Leon et al., 1996). Another study in London
with a maximum 8 hour average ozone concentration
of 160 µg/m3 was positive
but not significant (Atkinson et al.,
1999). A positive and significant association
was found in a meta-analysis of results
from 16 Canadian cities with a 99th percentile
of 174 µg/m3 1 hour average
(Burnett et al., 1997).
Given the above results,
it would be difficult to rule out the
possibility of an association at ozone
concentrations below 120 to 160 µg/m3
8 hour average. In fact, if there was
a threshold it could well be below this,
as it is unlikely that a single day or
a few days close to the maximum concentration
would be sufficient to drive a significant
association alone. The 90th percentiles
in these studies (where given) are around
60 to 80 µg/m3.
Studies of non-asthmatics
in areas with maximum ozone concentrations
up to 228 µg/m3 1 hour
average, 186 µg/m3 8
hour average or 82 µg/m3
24 hour average did not find statistically
significant associations with lower
respiratory symptoms (Hoek et al.,
1999; Declercq et al., 2000; Hoek et al.,
1995; Ward et al., 2002). The only exception
was a study in vigorously exercising cyclists
with a maximum 1 hour average ozone concentration
of 196 µg/m3 (Brunekreef
et al., 1994). On the other hand, increases
in asthma
attacks have been found in severe asthmatics
in Paris with a maximum ozone concentration
of 86 µg/m3 8 hour average
(Desqueyroux et al., 2002).
Some studies found significant
small negative effects on lung
function in places where ozone levels
did not rise above 140 or 160 µg/m3
8 hour average (Korrick et al., 1998;
Cuijpers et al., 1995). Rises in serum
CC16, a marker of lung permeability, have
been shown in cyclists at 2 hour average
ozone concentrations of 120 or 160 µg/m3
(Broeckhart et al., 2000).
Conclusions
Overall, it was not possible for all health
outcomes to confidently define an unequivocal
no- effect threshold
for the whole population. For the reasons
described above, interpretation of the
shape of exposure-response relationships
is very difficult to ascertain for ozone,
particularly at the low end of the ambient
range. However, in some studies associations
with outcomes ranging from mortality to
respiratory symptoms have been reported
from locations where ozone never exceeds
120 to 160 µg/m3 as 8
hour average values. Some panel studies
suggest small effects on lung function
above around 60 to 80 µg/m3
1 hour average. Our confidence in the
existence of associations with health
outcomes decreases at concentrations well
below these levels, as problems with negative
correlations with other pollutants and
lack of correlation with personal exposure
increase, but we do not have the evidence
to rule them out.
Further research
Clear conclusions concerning the shape
of exposure-response relationships in
epidemiological studies will always be
difficult but, given the importance of
this issue, we recommend further research
to explore the shape of the exposure-response
relationship for ozone. Greater understanding
of the different factors which may influence
the shape such as correlation with other
pollutants, correlations with personal
exposure and variations in the total oxidant
burden of different polluted environments,
may help. Recent work has increased understanding
of possible genetic reasons for increased
susceptibility
to ozone, suggesting new types of susceptible
groups, but the implications of this for
the range of responses at different ozone
concentrations have yet to be fully explored."
Source
& © : WHO
Regional Office for Europe Health
Aspects of Air Pollution - answers to
follow-up questions from CAFE (2004),
Section <5.3
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