step three. ITCZ changes and get across-equatorial atmospheric temperatures transportation change because of anthropogenic and you can paleoclimatic pressuring
step three. ITCZ changes and get across-equatorial atmospheric temperatures transportation change because of anthropogenic and you can paleoclimatic pressuring The relationship between PPenny and AHTEQ in the observations is coplotted with the slab ocean aquaplanet simulations in Fig. 8. The slope found in the observations is very close to that of the dos4-m depth run [...]