Not exact matches
Taking factors such as sea surface temperature, greenhouse gases and natural aerosol particles into consideration, the researchers determined that changes in the concentration of black carbon could be the primary
driving force behind the observed alterations to the
hydrological cycle in the region.
In turn, the rate of evaporation
drives the entire
hydrological cycle by altering the size and latitudinal positions of the air circulation systems and thus the rate of energy transfer from surface to space.
The temporal relationship between the Suess solar
cycle and particularly significant 210 yr oscillations in the speleothem δ18O records therefore supports the notion that solar variability played a significant role in
driving centennial - scale changes in the
hydrological cycle in the subtropics during the Holocene.