A comparative study of large-scale atmospheric circulation in the context of a future scenario (RCP4. 5) and past warmth (mid-Pliocene)
The mid-Pliocene warm period (~ 3.3–3.0 Ma) is often considered as the last sustained
warm period with close enough geographic configurations compared to the present one
associated with atmospheric CO2 concentration (405±50 ppm) higher than the modern
level. For this reason, this period is often considered as a potential analogue for the future
climate warming, with the important advantage that for mid-Pliocene many marine and
continental data are available. To investigate this issue, we selected the RCP4. 5 scenario …
warm period with close enough geographic configurations compared to the present one
associated with atmospheric CO2 concentration (405±50 ppm) higher than the modern
level. For this reason, this period is often considered as a potential analogue for the future
climate warming, with the important advantage that for mid-Pliocene many marine and
continental data are available. To investigate this issue, we selected the RCP4. 5 scenario …
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