Climate Change and Switzerland 2050 - OcCC - SCNAT
Climate Change and Switzerland 2050 - OcCC - SCNAT
Climate Change and Switzerland 2050 - OcCC - SCNAT
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70 <strong>Climate</strong> <strong>Change</strong> <strong>and</strong> Switzerl<strong>and</strong> <strong>2050</strong> | Health<br />
tions in architecture <strong>and</strong> in the planning of<br />
industrial <strong>and</strong> office buildings, is not only important<br />
with regard to work conditions but also in<br />
terms of other structural engineering issues.<br />
Water management<br />
The frequency of floods will be influenced by<br />
flood control measures. Floods <strong>and</strong> drinking<br />
2. Heat waves<br />
water supply also have an important impact on<br />
water management.<br />
Following is a presentation of the different areas<br />
in which effects of climate change are expected.<br />
The order reflects the decreasing relevance of<br />
the expected changes to health.<br />
In Switzerl<strong>and</strong>, the likely increase in heat waves by <strong>2050</strong> will be the most important climatically<br />
induced change with regard to health. The 1000 additional deaths caused by the heat-wave<br />
summer of 2003 demonstrated the sensitivity of the population. From <strong>2050</strong> onwards, similar<br />
conditions may occur every few years. Short-term measures include informing the population<br />
<strong>and</strong> introducing early warning systems. In the long term, adapted construction methods <strong>and</strong><br />
city planning may enhance well-being. It is unclear how quickly the population is able to adapt<br />
to new climatic conditions.<br />
Heat <strong>and</strong> mortality<br />
An increase in heat waves is an undisputed<br />
result of the increase in mean temperature.<br />
When the mean temperature rises, the probability<br />
of events that are rare today rises as well.<br />
It is not yet clear whether the distribution of<br />
the temperatures merely shifts in parallel to the<br />
mean temperatures, or whether the variance of<br />
single years also increases, as some studies suggest.<br />
1,2<br />
Mortality shows a clear dependency on temperature.<br />
Mortality rises considerably when the temperature<br />
threshold of a specific region is exceeded.<br />
Fig. 1 illustrates the relationship between<br />
mortality <strong>and</strong> wind-chill factor on the northern<br />
<strong>and</strong> southern side of the Alps within the period<br />
1990–2003. The regional difference is clearly<br />
evident: The “optimum” temperature with the<br />
lowest mortality rate is about 3.5 °C higher on<br />
the southern side than on the northern side of<br />
the Alps. That means that people adapt to generally<br />
higher ambient air temperatures physically<br />
as well as by attitude changes <strong>and</strong> technical<br />
measures. In order to consider the effects of<br />
climate change, the question therefore arises<br />
how quickly adaptation takes place. Based on<br />
the experiences of 2003, changes in behaviour<br />
could already be observed in 2005 (sunscreen,<br />
cooling, etc.).<br />
The heat-wave summer of 2003 clearly showed<br />
that severe heat waves can cause considerable<br />
health problems <strong>and</strong> additional deaths. Direct<br />
consequences are, for instance, heat-related cardiovascular<br />
problems, heat stroke, dehydration<br />
(drying-up of the body) <strong>and</strong> hyperthermia (overheating).<br />
Elderly people <strong>and</strong> those in care are<br />
most often affected.<br />
In 2003, heat waves resulted in a significant<br />
increase in the mortality rate in the affected<br />
regions in Central Europe (France, Southern<br />
Germany, Switzerl<strong>and</strong>, Northern Italy <strong>and</strong><br />
Spain) 3 , in particular in cases where information<br />
<strong>and</strong> care of risk groups was absent. Europe-wide,<br />
the number of additional deaths was estimated<br />
at ca. 35,000.<br />
In the summer of 2003, mean temperatures<br />
were about 4 to 5.5 °C above the long-term average.<br />
This lies approximately within the upper<br />
threshold of the expected temperature increase<br />
by <strong>2050</strong>. In this case, assuming that the vari-