Characterizing and understanding the multidecadal variations of
the continental hydrological cycle is a challenging issue given the limitation of observed data sets.
Not exact matches
These shifts to wetter summers correspond with periods on enhanced
continental runoff as expressed by the abundance of freshwater indicators such as the algae Pediastrum and the dinocyst taxon Bosedinia and areconsistent with enhanced
hydrological cycling prior to, and during the PETM interval.The marked increase in WMMT and WMMP puts a new perspective on environ - 15 mental precursors to the injection of carbon during the PETM.
All of these simulations exhibit a strongly damped
hydrological cycle relative to that of the modern climate, with less evaporation over the oceans and
continental - scale drying over land.