12.05.2015 Views

Zmena klímy – možný dopad (nielen) na obyvateľstvo - Prohuman

Zmena klímy – možný dopad (nielen) na obyvateľstvo - Prohuman

Zmena klímy – možný dopad (nielen) na obyvateľstvo - Prohuman

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

methods have become indispensable. But as far as climatic changes are concerned,<br />

they still serve as auxiliary techniques. Furthermore, their constant development<br />

and improvement of accuracy and precision, the varying object to measure, evoke<br />

worry that they, to a greater extent, will be affected by the problem of homogeneity.<br />

It also must be realized that even though the atmospheric processes are relatively<br />

well-understood and the existing measurement and research techniques,<br />

including supercomputers and modelling procedures, are highly developed,<br />

weather forecasting for time period longer than a couple of days is still problematic.<br />

Predicting climate changes in the nearest 10 or 100 years, not to mention<br />

greater time span, is then incomparably more complicated. What we have now<br />

are only doubtful sce<strong>na</strong>rios, with still little-understood basics and all kinds of<br />

feedbacks. What if we make just a tiny mistake in our studies? Then the outcome<br />

will be completely altered. Therefore every authoritative and firm statements of<br />

individual researchers must be questioned, especially if they are uncritically expressed<br />

by politicians and decision-makers.<br />

Climate change sce<strong>na</strong>rio – projection or fiction?<br />

Modern approach to the climate change forecasting relies on General Circulation<br />

Models (GCMs) which simulate the climate system. They are based on basic<br />

physical laws and use hydrody<strong>na</strong>mic and thermody<strong>na</strong>mic equations. The numerical<br />

global circulation models are complex and expensive; as a result, only a few<br />

research centres around the world are able develop them. The horizontal spatial<br />

resolution of the contemporary models reaches 100 km, which is a huge step forward<br />

if compared to first attempts in modelling that were made twenty years ago.<br />

Equally important is the growing number of applied variables.<br />

In addition to numerical models, the climate change sce<strong>na</strong>rios employ also<br />

predictions of greenhouse gasses emission as well as other pollutants connected<br />

with both socio-economic development of the world and the ecology actions. In<br />

the Special Report on Emission Sce<strong>na</strong>rios (SRES 2001) an exceptio<strong>na</strong>l interest is<br />

given to sustai<strong>na</strong>ble development, which allows to design sce<strong>na</strong>rios in which the<br />

greenhouse gasses emission will have become stable by 2050 (sce<strong>na</strong>rio B1 and B2).<br />

Depending on what model and which sce<strong>na</strong>rio is taken into account, the future<br />

climatic changes may be calculated, but they generally do not reach beyond the<br />

year 2100. The outcome of such projections are often referred to and discussed<br />

in the literature of climatology. For example, it is worth familiarizing oneself with<br />

the Fourth (IPCC 2007) and, currently in development, Fifth Assessment Report of<br />

the IPCC. The raise of average global temperature presented in them is relatively<br />

pessimistic: even if the assumed temperature raise for the 2020–2029 decade will<br />

106

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!