Projeção das mudanças no regime anual de chuvas até o fim do século XXI. As zonas mais azuis devem receber mais chuvas, e as mais alaranjadas devem experimentar a maior redução. O mapa mostra que praticamente toda a área de produção agropecuária do Brasil, e grandes biomas úmidos que dependem vitalmente de água e chuva abundantes, como o Pantanal e a Mata Atlântica, estão sob ameaça de tornarem significativamente mais secos. Outros que naturalmente têm menos precipitação, como o Cerrado e a Caatinga, também devem ter seu equilíbrio afetado negativamente. A Caatinga, que é naturalmente a região mais seca do Brasil, poderá receber até 50% menos de chuvas nas projeções mais pessimistas (6 °C de aquecimento). O Pampa, por outro lado, poderá ter sua precipitação aumentada em até 40%. Em ambos os casos, as mudanças que isso provocará no equilíbrio dos biomas provavelmente serão significativas.[119] Vários estudos preveem a savanização de grandes áreas da Floresta Amazônica e a desertificação de outros ecossistemas brasileiros, com extensa perda de biodiversidade e impacto socioeconômico.[120][121][122][123][124][125][126] Portugal todo deve ficar sob influência semelhante.
English: Based on NOAA (2007) public-domain source: This world map shows the change in annual average precipitation projected by the GFDL CM2.1 model for the 21st century. The change is in response to increasing atmospheric concentrations of greenhouse gases and aerosols based on a "middle of the road" estimate of future emissions. Future emissions are based on the "A1B" emissions scenario, taken from the Special Report on Emissions Scenarios. For the "A1B" emissions scenario, atmospheric carbon dioxide levels are projected to increase from 370 to 717 ppm. The plotted precipitation differences were computed as the difference between the 2081 to 2100 twenty year average minus the 1951 to 2000 fifty year average. Blue areas are projected to see an increase in annual precipitation amounts. Brown areas are projected to receive less precipitation in the future. (Note the irregular color bar intervals.)Warming of the global climate is expected to be accompanied by a reduction in rainfall in the subtropics and an increase in precipitation in subpolar latitudes and some equatorial regions. This pattern can be described in broad terms as the wet getting wetter and the dry getting drier, since subtropical land regions are mostly semi-arid today, while most subpolar regions currently have an excess of precipitation over evaporation. Though clearly a feature of a warming global climate, this characterization of the changing precipitation pattern cannot be applied to every locale, but should instead be thought of as a large-scale tendency that can be modified by local conditions in some cases. As seen in the map below, the drying is projected to be strongest near the poleward margins of the subtropics (for example, South Africa, southern Australia, the Mediterranean, and the south-western U.S.), a pattern that can be described as a poleward expansion of these semi-arid zones.This large-scale pattern of change is a robust feature present in nearly all of the simulations conducted by the world's climate modeling groups for the 4th Assessment of the Intergovernmental Panel on Climate Change (IPCC), including those conducted at NOAA’s Geophysical Fluid Dynamics Laboratory (GFDL). It is also evident in observed 20th century precipitation trends.In the map, changes are measured in inches of liquid water per year, ranging from +60 to -60. As described above, changes are not uniform globally. Most areas which see increases in precipitation are in the range of +1 to +30. Most areas which see decreases are in the range of -1 to -45.References: NOAA, February 2007: GFDL Climate Modeling Research Highlights: Will the wet get wetter and the dry drier? (PDF), vol. 1, no. 5, revision 10/15/2008, 4:47:16 PM. The National Oceanic and Atmospheric Administration (NOAA) Geophysical Fluid Dynamics Laboratory (GFDL) - Princeton, NJ, USA