| | The climatic effects of water vapour |
| | 0,35 | | MB |
| | 5 | | stron |
| | 2379 | | ID | National Institute for Space Research |
| | 2003 | | rok |
| | EXTREME variations in local weather and the seasons make it easy for people to mutter |
| | “greenhouse effect”, and blame everything on carbon dioxide. Along with other man-made gases, |
| | such as methane, carbon dioxide has received a bad press for many years and is uniformly cited |
| | as the major cause of the greenhouse effect. This is simply not correct. While increases in carbon |
| | dioxide may be the source of an enhanced greenhouse effect, and therefore global warming, the |
| | role of the most vital molecule in our atmosphere – water – is rarely discussed. Indeed, water |
| | barely rates a mention in the hundreds of pages of the 2001 report by the Intergovernmental Panel |
| | on Climate Change. |
| | Many aspects of the seemingly simple water molecule conspire to make it difficult to model its |
| | effect on our climate. Unlike most other atmospheric gases, the distribution of water in the |
| | atmosphere varies strongly with time, location and altitude (figure 1).Water is also unique among |
| | atmospheric molecules because it changes phase at terrestrial temperatures.This means that it can |
| | transfer energy from its frozen form at the poles to its liquid and vapour forms in the atmosphere. |
| | Once in the atmosphere, water moves with the winds and can even diffuse up to the stratosphere, |
| | where it is responsible for destroying the ultraviolet-shielding ozone layer. |
| | The atmosphere plays a crucial role in the Earth’s radiation budget because it absorbs both the |
| | incoming radiation from the Sun and the outgoing radiation that is reflected from the planet’s |
| | surface. However, the radiation in each of these processes has very different wavelengths. The |
| | Sun radiates approximately as a black body with a temperature of 5800K, which peaks in the optical |
| | region at a wavelength of about 0.6 µm. The reflected radiation profile, on the other hand, is much |
| | closer to a black body at a temperature of 275 K, and has a peak at much longer infrared |
| | wavelengths (about 11 µm). The physical processes that lead to the absorption of radiation in the |
| | two regions are different, but water vapour plays the dominant role in both. |