step three. ITCZ shifts and you will get across-equatorial atmospheric temperatures transportation transform due to anthropogenic and you may paleoclimatic forcing
step three. ITCZ shifts and you will get across-equatorial atmospheric temperatures transportation transform due to anthropogenic and you may paleoclimatic forcing The relationship between PCent 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