The deterioration of physical health due to changes in the weather conditions was suggested beginning
from Hippocrates at the 5th century B.C. Climatic characteristics, such as rain, atmospheric
pressure (AP), thunderstorms, temperature, weather phases and wind have been repeatedly
implicated in the pathogenesis of many diseases such as rheumatoid arthritis, SLE,Behcet's disease
Bell's palsy, sudden hearing loss, myocardial infarction, abdominal aortic aneurysm ruptures, asthma
and some showed significant relationship (
1). The clinical impression of many physicians is in the
direction that occurrence of SP is not a random event. Similarly this relationship has been investigated
for spontaneous pneumothorax (SP). The cause of the rupture of blebs or bullae causing SP remains
unclear, but suggestions were concentrated over the presence of a substantial transpulmonary
pressure gradient (
2). The overexpansion of the alveoli due to the trapped air may trigger the occurrence
of SP when the outer pressure falls (
3). It has also been suggested in many series that SP admissions
occurs in clusters (
1,
2,
4,
5,
6).
Atmospheric pressure, temperature changes or correlation with specific weather phases, seasonal
factors and storm were suggested to be precipitating factors in the development of SP (
1,
2,
5,
6,
7).
The results of some series do not support the premise that seasonal factors are involved in precipitating
SP, although certain climatic parameters showed weak associations with the incidence of SP
(
8,
9,
10).
In this issue of the Journal of Thoracic Disease, Bertolaccini et al. report their results of the
study examining the influence of standard meteorological parameter variations and concentrations of
the major air pollutants on the incidence of SP in a highly developed industrial area (Turin, Italy)
(
11). Although the relation between SP and meteorological parameters were examined previously,
this retrospective report is linking SP to atmospheric chemical parameters like atmospheric particles
(eg. PM10), ozone and nitrogen dioxide levels. This original study by Bertolaccini et al. suggests that
the occurrence of SP might be facilitated by higher and less dispersed values of daily mean nitrogen
dioxide, by lower and more dispersed values of ozone, and by less dispersed temperature and wind
speed values. The other examined correlations like, large carbon dioxide maxima and during cold
and windy days, appeared less significant.
Their current retrospective study consisted of a total 591 SP admissions and, 363 days with admissions
(19% of the total) to two hospitals between 2002 and 2007 in Turin, Italy. The patients with
documented primary SP was included to the study where traumatic and secondary pneumothoraces
were excluded. They took into account only the variables recorded one day before SP occurrence
pointing that the nature of SP is severe and disabling. A pneumothorax patient may became symptomatic
within several days and because of the retrospective character of the patient history study, the
day that SP developed was not considered to be reliable enough, so other investigators compared the measured meteorological values of the 2 to 4 consecutive days prior
to admission as well as the actual day of admission (
1,
5,
6,
9).
In the current study the climatic variable measurements were
AP, temperature, relative humidity, wind speed, and as mentioned
in the introduction section some atmospheric chemical parameters
which were absent in the previous SP, but asthma exacerbations
studies, were solar global radiation, precipitation, NO, NO2, SO2,
PM10, C6H6, C7H8, ozone, carbon monoxide and carbon dioxide.
Mean, maximum and minimum daily values, daily standard deviations,
average daily anomalies and several daily variations were
calculated. The study results are in agreement that SP patients are
admitted in clusters, which strongly supports the hypothesis that
the meteorological conditions could play a role in the mechanism
responsible for development of SP (
1,
2,
4-6). The incidence of SP
had no seasonal or monthly correlation in this study. Similarly no
seasonal or monthly predominance of clusters could be identified
in some studies (
1,
2,
5,
6). Slight spring preponderance and a significant
increase in the rate of SP in May and December and another
one in summer and in July was demonstrated (
9,
12). In this
study no correlations between SP and variations in AP was found.
Alifano et al. found a significant correlation with wider differences
in AP mean between the index day and the previous day and between
the AP minimum and the AP maximum of the previous day
(
6). Bense found that a fall in AP of at least 10 millibars followed
by increased SP admissions (
7). Similarly in our study clusters of
SP episodes were significantly associated with falls and wider differences
in AP. We suggest that transpulmonary pressure gradient
due to falls in AP may be enough to cause SP in some patients (
1).
Although the exact mechanism by which a fall in AP may cause SP
remains unknown two suggestions are reasonable. First when the
air inside the blebs or bullae is trapped due to bronchospasm, a
rapid equilibration of the pressure gradient with the atmosphere
could not be achieved, second like in asthma there may be a relation
between inflammation and weather conditions; thus a check
valve mechanism may result in SP (
2,
6). The authors mentioned
that the only significant meteorological variable correlated with the
onset of SP is the minimum wind speed.
In the current study, the results suggest that, occurrence of SP
appears to be facilitated by higher and less dispersed values of daily
mean nitrogen dioxide, by lower and more dispersed values of ozone
and by less dispersed temperature and wind speed values. Other correlations, as those with large carbon dioxide maxima and
during cold and windy days stated to appear less significant. This
study shows unique external contributing factors for the onset of
SP which are promising and warrant further investigation. Other
population studies in different countries based on similar designs
should be developed to further confirm and detail the influences of
meteorological variables on SP occurrence. And limitations of the
studies, the presence of comorbid illnesses or respiratory disease,
cigarette smoking, different climatic conditions, nonhomogenous
distribution of cases must be taken into account.