L’appauvrissement de l’ozone et les changements climatiques
L’appauvrissement de l’ozone et les changements climatiques sont deux problèmes distincts mais ils ont tous deux un effet sur les cycles
terrestres, il n’est pas possible de les séparer totalement. Il reste encore de nombreuses incertitudes au sujet des relations entre les
deux processus.
26 May 2010 - by UNEP/GRID-Arendal
Production déclarée totale de substances appauvrissant l’ozone
Veuillez noter qu’au fur et à mesure que de nouveaux pays ratifient le Protocole de Montréal, les chiffres de la production déclarée totale augmentent. De ce fait, la production ne correspond pas au même nombre de pays en 1990 et en 2007.
26 May 2010 - by UNEP/GRID-Arendal
Pays donateurs et pays bénéficiaires du Fonds multilatéral
Les pays reçoivent des fonds en fonction de leurs besoins pour se conformer au Protocole. C’est-à-dire qu’ils reçoivent des fonds correspondant à l’élimination de quantités spécifiques de SAO en production et en consommation. Les pays producteurs et les grands consommateurs de SAO reçoivent davantage de fonds car ils ont de plus grands besoins. Cependant, tous les pays en voie de développement qui sont parties au Protocole de Montréal ont reçu de...
26 May 2010 - by UNEP/GRID-Arendal
Major mineral fuel resources in Europe, Caucasus and Central Asia
Mineral fuels for electricity and heat generation take primarily two forms: fossil fuels in the form of oil, natural gas and coal, and uranimum ore for nuclear power. Oil and gas are distributed in different belts, primarily in the North Sea, Caucasus and Northern Russia. Coal in different forms is still an important fuel resource and resources are distributed over the region. Uranium resources are primarily in Ukraine and Central Asia.
20 Jul 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
Solar insolation
Solar insolation, the quantification of energy per surface area on the ground, can be used as an indicator for the potential for solar energy. This graphic presents solar insolation, calculated to annual averages from monthly averages 1983 - 1993.
20 Jul 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
Hydropower potential (theoretical possitibility for electricity generation)
xHydropower, generating electricity through turbines, represents a clean and renewable energy source, but not without problems. Dams and reservoirs disrupt the natural flow, and may increase siltation and evaporation, in addition to severe impacts for wildlife, for instance migrating fish. The gross theoretical capability, presented in this map, represents a calculation based on the topography and precipitation in the countries, and is the amount...
20 Jul 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
tourismstats_see
About tourismstats_see
20 Jul 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
political_see
About political_see
20 Jul 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
The expansion of the European Union, political map 1957, 1987, 1997 and 2007
The political map and landscape in Europe has changed drastically in the period of 1957-2007. In the aftermath of the Second World War, the European Communities was formed in 1957 by the treaty of Rome, with six signatories. This was a time with considerable poltical tension between the Eastern Bloc (Warsaw pact, COMECON and associated countries) on one side, and NATO on the other. Through time, the communities expanded with the associated EFTA c...
20 Jul 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
Trends in permafrost temperatures in the central and northern Mackenzie Valley, 1984-2006
Temperature monitoring in Canada indicates a warming of shallow permafrost over the last two to three decades. Since the mid-1980s, shallow permafrost (upper 20-30 m) has generally warmed in the Mackenzie Valley. The greatest increases in temperature were 0.3 to 1°C per decade in the cold and thick permafrost of the central and northern valley. In the southern Mackenzie Valley, where permafrost is thin and close to 0°C, no significant trend in pe...
01 Jun 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
World ocean thermohaline circulation (alternative version)
The global conveyor belt thermohaline circulation is driven primarily by the formation and sinking of deep water (from around 1500m to the Antarctic bottom water overlying the bottom of the ocean) in the Norwegian Sea. When the strength of the haline forcing increases due to excess precipitation, runoff, or ice melt the conveyor belt will weaken or even shut down. The variability in the strength of the conveyor belt will lead to climate change in...
01 Jun 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
Historical trends in carbon dioxide concentrations and temperature, on a geological and recent time scale
The most recent geological history, in the last hundred thousand years, has been characterised by cycles of glaciations, or ice ages. The historic temperatures, through these times, have been low, and continental ice sheets have covered large parts of the world. Through ancient air, trapped in tiny bubbles in the Antarctic ice, we have been able to see what the temperature cycle was at that time, and also the concentration of carbon dioxide (CO2)...
01 Jun 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
Arctic sea ice minimum extent in September 1982, 2005 and 2007
The red line indicates the median minimum extent of the ice cover for the period 1979–2000. This figure compares the Arctic sea ice extent in September for the years 1982 (the record maximum since 1979), 2005 and 2007 (the record minimum). The ice extent was 7.5 million km2 in 1982 and only 5.6 million km2 in 2005 and down to 4.3 million km2 in 2007. As has been observed in other recent years, the retreat of the ice cover was particularly pronoun...
18 Apr 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
Increases in annual temperatures for a recent five-year period, relative to 1951-1980
Warming is widespread, generally greater over land than over oceans, and the largest gains in temperatures for the planet are over the North American Arctic, north central Siberia, and on the Antarctic Peninsula. These recent increases in temperature are confirmed by changes in other features: loss of sea ice, shift of tundra to shrub vegetation, and migration of marine and terrestrial ecosystems to higher latitudes.
18 Apr 2007 - by Hugo Ahlenius, UNEP/GRID-Arendal
Ringed seal pupping lair, with the pup in the lair and the female approaching the haul-out hole from the water
Ringed seals are the 'classic' Arctic seal in many regards, being found as far north as the Pole because of their ability to keep breathing holes open in ice that can reach 2 metres in depth. This species is certainly one of the most vulnerable of the high-Arctic seals to the declines in the extent or quality of sea ice because so many aspects of their life-history and distribution are tied to ice. Ringed seals also require sufficient snow cover...
01 Nov 2007 - by Robert Barnes, UNEP/GRID-Arendal