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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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