The purpose of the project DEKLIM-EEM is to reconstruct past interglacials based on proxy data and to understand the processes that are responsible for climatic changes during these interglacials by applying
The purpose of the project DEKLIM-EEM is to reconstruct past interglacials based on proxy data and to understand the processes that are responsible for climatic changes during these interglacials by applying
The purpose of the project DEKLIM-EEM is to reconstruct past interglacials based on proxy data and to understand the processes that are responsible for climatic changes during these interglacials by applying
Simulation of the last interglacial climate with the MPI/UW model. This simulation has been performed for comparison with the preindustrial climate run MPI/UW_MM_ATM_CTL_P. In this simulation the incoming
Simulation of the last interglacial climate with the MPI/UW model. This simulation has been performed for comparison with the preindustrial climate run MPI/UW_MM_ATM_CTL_M. In this simulation the incoming
MPI/UW_MM_ATM_HOL Holocene (10 - 0 kyrBP) DKRZ storage: /dxul/ut/m/m211003/echamlsg/21181ctrl
Simulation of the Holocene climate with the MPI/UW model. This simulation has been performed for comparison
Simulation of the last interglacial climate with the MPI/UW model. This simulation has been performed for comparison with the time transient climate runs MPI/UW_MM_ATM_HOL_acc_M, MPI/UW_MM_ATM_EEM_acc_M.
Simulation of the last interglacial climate with the MPI/UW model. This simulation has been performed for comparison with the preindustrial climate run MPI/UW_MM_ATM_CTL_P. In this simulation the incoming
Simulation of the last interglacial climate with the MPI/UW model. This simulation has been performed for comparison with the preindustrial climate run MPI/UW_MM_ATM_CTL_M. In this simulation the incoming
MPI/UW_MM_ATM_EEM (129 - 109 kyrBP), DKRZ storage: /dxul/ut/m/m211021/echamlsg/21176ctrl
Simulation of the last interglacial climate with the MPI/UW model. This simulation has been performed for comparison
Simulation of the climate of the Eemian interglacial at 125000 years before present. Boundary conditions are the same as in the control run (EH4_HOPE_T30-CTL), apart from the concentration of anthropogenic
Simulation of the climate of the Eemian interglacial at 125000 years before present. Boundary conditions are the same as in the control run (EH4_HOPE_T30-CTL), apart from the concentration of anthropogenic