Climate change  

         

Air

Climate change
Indicators
International Commitments
Emissions of greenhouse effect gases
Increase in air temperatures
Changes in the water level of the Baltic Sea
Use of renewable energy resources

Ozone depletion

Transboundary air pollution

Air quality

Temperatures on Earth are determined by the natural greenhouse effect - part of the solar radiation reaching the Earth's surface is absorbed, and part is reflected to the atmosphere as infrared radiation. Water vapour and greenhouse effect gases (carbon dioxide, methane, sulphur dioxide, ozone, and others) do not hinder the path of solar radiation through the atmosphere, but they absorb the reflected infrared radiation. The mean temperature on the surface would be about -18°C without this absorption, but is about +14°C with the absorption.

An increase in the atmospheric concentration of greenhouse effect gases causes increased absorption of infrared radiation, raising the temperatures. This causes an additional greenhouse effect.

Anthropogenic gases which disrupt the heat exchange equilibrium include: carbon dioxide (CO2), methane (CH4), nitrogen oxide (N2O), hydrofluorocarbons (HFC), perfluorocarbons (PFC), and sulphur hexafluoride (SF6). These gases create a layer around Earth which does not allow heat to dissipate to the cosmos, and causes various changes: increase in global temperatures, raising sea level, changes in species composition, and others.