Warm Paleocene/Eocene climate as simulated in ECHAM5/MPI-OM
We investigate the late Paleocene/early Eocene (PE) climate using the coupled atmosphere-ocean-sea ice model ECHAM5/MPI-OM. The surface in our PE control simulation is on average 297 K warm and ice-free, despite a moderate atmospheric CO<sub>2</sub> concentration of 560 p...
Main Authors: | M. Heinemann, J. H. Jungclaus, J. Marotzke |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2009-12-01
|
Series: | Climate of the Past |
Online Access: | http://www.clim-past.net/5/785/2009/cp-5-785-2009.pdf |
Similar Items
-
Numerical evidence against reversed thermohaline circulation in the warm Paleocene/Eocene ocean
by: Bice, Karen L., et al.
Published: (2001) -
Could changing ocean circulation have destabilized methane hydrate at the Paleocene/Eocene boundary?
by: Bice, K.L, et al.
Published: (2002) -
Global mean surface temperature and climate sensitivity of the early Eocene Climatic Optimum (EECO), Paleocene–Eocene Thermal Maximum (PETM), and latest Paleocene
by: G. N. Inglis, et al.
Published: (2020-10-01) -
Changing European storm loss potentials under modified climate conditions according to ensemble simulations of the ECHAM5/MPI-OM1 GCM
by: J. G. Pinto, et al.
Published: (2007-01-01) -
ENSO combination mode and its influence on seasonal precipitation over southern China simulated by ECHAM5/MPI-OM
by: Shengjie YI, et al.
Published: (2019-05-01)