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Heart Online First, published on July 23, 2014 as 10.1136/heartjnl-2014-306160
Editorial
The hazard of rounding Cape Horn:
is it changing?
Pietro Amedeo Modesti1,2
…he who goes the oftenest round Cape
Horn goes the most circumspectly.
Herman Melville, “White-Jacket”, 1850
Notwithstanding the range of strategies to
help one cope with the cold weather, most
countries experience mortalities in excess
of 5–30% in winter, brought on mainly by
cerebrovascular events.1 This variability is
mainly attributed to the population being
able to keep themselves warm, both
indoors and outdoors, necessitated by the
mean cold temperature. Policies and
measures to increase efficient use of energy
indoors, coupled with advice to citizens
suggesting to wear adequate warm protective clothing and to keep themselves active
when out in the open, have been thus
promoted. The elderly are aware of the
risks, and traditionally perceive winter as a
rounding of Cape Horn.
Consequently, the result of exposure to
acute cold may trigger vasoconstriction,
with a rise in blood pressure (BP), and
myocardial ischaemia in patients with coronary artery disease. This acute response is
considered in all guidelines on BP measurement which recommend the importance of standardised room temperature
when assessing BP values. However, a
negative relationship between outdoor
temperature and BP values was consistently observed even when measurements
were taken in comfortably warm rooms.2
In the French Three-City study3 that prospectively investigated 8801 participants
over the age of 65 years, average systolic
BP was 5 mm Hg higher in winter than in
summer. This variation was independent
of anthropometric data and baseline BP
values, but rather related to the subjects’
age. Variations in BP were greater in subjects 80 years of age or older, than in
younger participants. In the reanalysis of
data collected in the World Health
Organization Monica Project (monitoring
trends and determinants in cardiovascular
1
Department of Clinical and Experimental Medicine,
University of Florence, Florence, Italy; 2Centre for Civil
Protection and Risk Studies, University of Florence
(CESPRO), Florence, Italy
Correspondence to Professor Pietro Amedeo
Modesti, Department of Clinical and Experimental
Medicine, University of Florence, Largo Brambilla 3,
Florence 50134, Italy; pamodesti@unifi.it
disease) risk factors surveys,4 including 25
populations in 16 countries (115 434 participants aged 35–64 years) the effect of
outdoor temperature remained after controlling for indoor temperature, as a 1°C
increase in outdoor temperature reducing
BP values by 0.14 mm Hg (95% Cl −0.23
to −0.05, adjusted for indoor temperature). Conversely, the effects of the winter
season disappeared after controlling for
outdoor temperature, suggesting that a
major component of the seasonal change
in BP was the direct result of temperature.4
As physicians, we often have to deal
with the effects of temperature in treating
hypertensive
patients
even
during
summer, when we encounter the potential
implications of falls or acute renal failure
caused by a marked reduction in BP
especially in the elderly. As a consequence,
(although not considered in hypertension
guidelines) physicians often resort to seasonal adaptation of antihypertensive drugs
in their clinical practice.
The influence of temperature, or at
least seasonality, is conversely less considered in epidemiological studies investigating the burden of risk factors in
populations. The importance of conducting an epidemiological study throughout a
whole year, or at least to declare the exact
timing of the study in the final report, is
indeed not always given due importance.
A recent large epidemiological survey
aimed at assessing hypertension burden at
the population level, BP is the main factor
guiding cardiovascular (CV) risk stratification, including the measurement of temperature as one of the parameters
investigated.5 In the Hypertension and
Diabetes in Yemen (HYDY) study, an
increase of 1°C in air temperature reduced
hypertension with an OR of 0.98 (95%
confidence limits: 0.96–0.99) at logistic
regression analyses adjusted for age,
gender, education and average air temperature at the two survey visits.5
The elegant study by Marti-Soler et al6
shows that, beside systolic BP levels, which
were, on average, 3.5 mm Hg lower in
summer than in winter, other CV risk factor
levels tended to be higher in winter and
lower in summer. In particular, in the
Northern Hemisphere, the estimated seasonal variations were 0.26 kg/m2 for Body
Mass Index, 0.6 cm for waist circumference,
0.02 mmol/L for triglycerides, 0.10 mmol/L
for total cholesterol, 0.01 mmol/L for highdensity lipoprotein cholesterol, 0.11 mmol/L
for low-density lipoprotein cholesterol,
and 0.07 mmol/L for glycaemia. Similar
seasonal variations were found in the
Southern Hemisphere, with the exception
of waist circumference, HDL and LDL
cholesterol.6 Therefore, the resultant estimate of individual CV risk varied depending on the season. As a consequence, at the
patient level, only a low value in winter
can thus be considered a low ‘yearly’
value, whereas a low value in summer does
not mean a low value in winter. At the
population level, seasonal differences may
be important because CV risk estimation
plays a key role in the efficient allocation
of resources.5 This aspect is especially
important for low-income countries, but
any speculation is limited by the small
number of studies carried out in the
Southern Hemisphere, and by the absence
of studies investigating populations from
Asia, Africa and South America.6
As variations in weather patterns and
adaptive abilities are determined by latitude, a differential effect of temperature
on mortality has been found. The temperature of the lowest temperature-associated
mortality observed in a city (minimum
mortality temperature), was shown to vary
by latitude. People who live in cities
located at higher latitudes, have lower
minimum mortality temperatures, while
people who live in cities located at lower
latitudes have higher thresholds in coping
with ambient temperatures. The large
majority of studies included in the analysis6 were conducted in European countries. In this setting, the possibility of
comparing between-countries differences
in the seasonal variations of BP and CV
risk, might give an insight into the range of
distribution of excess winter mortality
across Europe. More precisely, excess
winter mortality was found to be higher in
Southern Europe (Portugal and Spain),
than in Scandinavia and Northern Europe
(Finland and Germany).7 In Europe,
thermal efficiency of housing, as well as
the capability to cope with cold weather,
were indeed found to increase with rising
latitude.8 In the reanalysis of BP data collected within the WHO MONICA
Project,4 the random effects that seasons
had on the main risk factor for CV events
(BP), were latitude-dependent being lower
for countries with colder climates, and
higher for countries with warmer climates.
Conversely, no association between the
estimated amplitude of seasonal BP variations and latitude was observed by
Marti-Soler et al6 (figure 1). The numbers
Modesti PA. Article
Heart Monthauthor
2014 Vol (or
0 No their
0
1
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Editorial
Figure 1 (A) Population-specific
seasonal change in systolic blood
pressure against latitude. Reproduced
from Barnett et al4 with permission of
the publisher. (B) Estimated amplitude
of seasonal changes in blood pressure
by latitude. Reproduced from
Marti-Soler et al6 with permission of
the publisher.
of populations and countries included in
the two studies, are comparable; the
model adopted to estimate seasonal BP
variations is also similar. Nevertheless, the
different representations of extreme latitudes might play a role. The large majority
of studies included by Marti-Soler et al6
were, however, performed after 1997
(only 8 out of the 23 studies were started
before 1997), whereas the collection
period of studies included by Barnett et al4
ranged from 1979 to 1997. In England
and Wales, the association of year-to-year
variation in excess winter mortality with
the number of cold days in winter (<5°C),
evident until mid-1970, has recently disappeared 9 and the link between winter temperature and excess winter mortality is no
longer as strong as before. Historical
trends in excess winter mortality also show
a gradual reduction in deaths between
1980 and 2011. Those changes could
probably be linked to the improved energy
efficiency in homes and the quality of
housing.9
The relationship between weather and
winter mortality is probably altered 9 and the
discrepancies between the two studies might
2
disclose a reduced latitude-dependency of
the influence of winter on BP. Is it the end of
a myth? Probably not. The variability
observed by Marti-Soler et al6 in the distribution of seasonal variation of BP by latitude might also indicate that policy changes
are non-homogeneously occurring in
Europe. Cape Horn is still Cape Horn,
never a place to be treated lightly.
2
3
4
5
Competing interests None.
Provenance and peer review Commissioned;
internally peer reviewed.
To cite Modesti PA. Heart Published Online First:
[please include Day Month Year] doi:10.1136/heartjnl2014-306160
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Modesti PA. Heart Month 2014 Vol 0 No 0
Downloaded from heart.bmj.com on August 19, 2014 - Published by group.bmj.com
The hazard of rounding Cape Horn: is it
changing?
Pietro Amedeo Modesti
Heart published online July 23, 2014
doi: 10.1136/heartjnl-2014-306160
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