Climate and environmental change in the Mediterranean Basin - current situation and risks for the future. First Mediterranean assessment report union for the Mediterranean
| Autor: | Cramer, Wolfgang, Guiot, Joël, Marini, Katarzyna, Azzopardi, Brian, Balzan, Mario V., Cherif, Semia, Doblas-Miranda, Enrique, Dos Santos, Maria, Drobinski, Philippe, Fader, Marianela, Hassoun, Abed El Rahman, Giupponi, Carlo, Koubi, Vassiliki, Lange, Manfred, Lionello, Piero, Llasat, Maria Carmen, Moncada, Stefano, Mrabet, Rachid, Paz, Shlomit, Savé, Robert, Snoussi, Maria, Toreti, Andrea, Vafeidis, Athanasios T., Xoplaki, Elena |
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| Jazyk: | angličtina |
| Rok vydání: | 2020 |
| Předmět: | |
| Popis: | Virtually all sub-regions of the Mediterranean Basin, on land and in the sea, are impacted by recent anthropogenic changes in the environment. The main drivers of change include climate (temperature, precipitation, atmospheric circulation, extreme events, sea-level rise, sea water temperature, salinity and acidification), population increase, pollution, unsustainable land and sea use practices and non-indigenous species. In most areas, both natural ecosystems and human livelihoods are affected. Due to global and regional trends in the drivers, impacts will be exacerbated in the coming decades, especially if global warming exceeds 1.5 to 2°C above the pre-industrial level. Significantly enhanced efforts are needed in order to adapt to inevitable changes, mitigate change drivers and increase resilience. Due to anthropogenic emissions of greenhouse gases, climate is changing in the Mediterranean Basin, historically and projected by climate models, faster than global trends. Annual mean temperatures on land and sea across the Mediterranean Basin are 1.5°C higher than during pre-industrial times and they are projected to rise until 2100 by an additional 3.8 to 6.5°C for a high greenhouse gas concentration scenario (RCP8.5) and 0.5 to 2.0°C for a scenario compatible with the long-term goal of the UNFCCC Paris Agreement to keep the global temperature well below +2°C above the pre-industrial level (RCP2.6). On land and in the sea, heat waves will intensify in duration and peak temperatures. Despite strong regional variations, summer rainfall will likely be reduced by 10 to 30% in some regions, increasing existing water shortages, desertification and decreasing agricultural productivity. peer-reviewed |
| Databáze: | OpenAIRE |
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