a sensitivity study to separate the effect of changes in land surface (including lakes and vegetation) and changes in atmosphere-ocean conditions on changes in Saharan dust emission and North Atlantic dust deposition between mid-Holocene and pre-industrial times. Four equilibrium simulations with variant land surface/ atmosphere-ocean conditions for mid-Holocene and pre-industrial, each 30 years
[1] DOIEgerer, S.; Claussen, M.; Reick, C.; Stanelle, T. (2016). The link between marine sediment records and changes in Holocene Saharan landscape: simulating the dust cycle. doi:10.5194/cp-12-1009-2016