chapter - Atmospheric and Oceanic Science
chapter - Atmospheric and Oceanic Science
chapter - Atmospheric and Oceanic Science
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12.6.1. Baseline scenarios<br />
It is convenient to define a baseline scenario or observed climate with regard<br />
to which the changes in the different climate scenarios can be referred. The election<br />
of this baseline or reference period is frequently determined by the availability of<br />
climatic information. Most of the impact assessment studies aim to determine the<br />
effects of the change with respect to current conditions, <strong>and</strong> so they used recent<br />
base periods such as 1961-90. It is important to have in mind that no matter whatever<br />
the baseline period is, there are differences between climatic averages based<br />
on long periods of time (for instance, 100 years) <strong>and</strong> those considering shorter subperiods.<br />
Moreover, different 30-years periods show differences in regional annual<br />
mean temperatures of ±0.5°C <strong>and</strong> of ±15% in annual precipitation (Hulme <strong>and</strong> New<br />
1997; Visser et. al. 2000). Thus small regional changes in future climate scenarios<br />
cannot be consider significant.<br />
12.6.2. Global scenarios<br />
Climate scenarios<br />
Scenario A2 proposed by the IPCC implies that in less than a century, carbon<br />
dioxide concentrations will reach more than three times pre-industrial levels,<br />
methane concentration will be more than 5 times <strong>and</strong> those of nitrous oxide will<br />
almost double. It is important to highlight that these values have never been reached<br />
at least in the last 20 millions years.<br />
For year 2060, GCM project an increase of the global surface temperature of<br />
1.3 to 2.5°C depending on the socio-economic scenario, with higher warming at<br />
high latitudes <strong>and</strong> in winter. This warming would not be uniform; in the continental<br />
areas of the northern hemisphere there would be regions where temperature<br />
would raise more than 8ºC. Table 12.2 shows mean projections of temperature rise<br />
for different decades up to 2100 with respect to the period 1961-90 for different scenarios.<br />
Beyond that date the increase of the temperatures could be much higher,<br />
critically depending on the future evolution of the GHG emissions.<br />
Table 12.2. Increase in the surface mean global temperature (ºC) for different<br />
socio-economic scenarios.<br />
SCENARIOS<br />
A1 A2 B1 B2<br />
2000 0,15 0,15 0,15 0,15<br />
2020 0,50 0,50 0,50 0,60<br />
2040 1,20 1,00 0,90 1,10<br />
2060 2,50 1,80 1,30 1,60<br />
2100 4,50 3,80 2,00 2,70<br />
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