Holocene Hydroclimate

 

Global pattern of aridity, drought, precipitation and evapotranspitation have changed from the mid Holocene to the late the Holocene, i.e., the last some 8000 years. The global pattern of hydroclimate and possible extreme values like prolonged drought shall be calculated from the transient Holocene simulations with the MPI-ESM and, if possible, be compared with proxy data.

 

Contact: Martin Claußen, Geomatikum 1619, martin.claussen@we dont want spammpimet.mpg.de