The atmospheric general circulation model ECHAM 5. PART I: Model description

By E. Roeckner, G. Bäuml, Luca Bonaventura, R. Brokopf, M. Esch, Marco A. Giorgetta, Stefan Hagemann, I. Kirchner, L. Kornblueh, E. Manzini and 4 more. 2003

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Subfields: Atmospheric Science

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Citations in the corpus

The influence of a weakening of the atlantic meridional overturning circulation on ENSO (2006, methodology): “The global salt balance is satisfied by uniformly removing freshwater from the remaining ocean surface. d. MPI-OM1 The Max Planck Institute Ocean Model (MPI-OM1) coupled model consists of the atmosphere/land component ECHAM5 (Roeckner et al. 2003) and the ocean/ sea ice model MPI-OM (Marsland et al.”
Meridional transport and deposition of atmospheric 10 Be (2008, background): “A complete description of the ECHAM5 GCM is given in Roeckner et al. (2003).”
On Constraining Estimates of Climate Sensitivity with Present-Day Observations through Model Weighting (2011, background): “…sensitivity for a more practical reason: in current ensembles of climate models, global measures of error are not systematically related to climate sensitivity or the underlying feedbacks (Knutti et al. 2006; Murphy et al. 2004; Piani et al. 2005; Sanderson et al. 2008; Collins et al. 2011).”
The aerosol-climate model ECHAM5-HAM (2004, methodology): “Further, as shown byTimmreck and Schulz(2004) based on a study with the ECHAM4 GCM and theBalkanski et al. (2004) emission scheme, the application of the nudging technique influences the wind statistics and spatial distribution, Atmos.”
SALSA – a Sectional Aerosol module for Large Scale Applications (2007, methodology): “Phys., 8, 2469–2483, 2008 www.atmos-chem-phys.net/8/2469/2008/ ECHAM5 (Roeckner et al., 2003): 2400 s (T31L19), 1800 s (T42L19), 1200 s (T42L31 and T63L19), 900 s (T84L19), 720 s (T63L31 and T106L19), 480 s (T85L31), and 360 s (T106L31).”
Ocean Circulation and Tropical Variability in the Coupled Model ECHAM5/MPI-OM (2006, methodology): “Secondly, the relative motion between the lowest atmospheric layer and the ocean surface is used in the calculation of the drag coefficient (and other turbulent mixing coefficients) assuming a law-of-the-wall formulation (Roeckner et al., 2003).”
Efficient MCMC for Climate Model Parameter Estimation: Parallel Adaptive Chains and Early Rejection (2012, methodology): “J¨arvinen et al. (2010) applied an adaptive MCMC method for estimating the joint posterior probability density of a small number ( n = 4) of closure parameters appearing in the ECHAM5 climate model (see Roeckner et al. 2003, for model description).”
Classifications of Atmospheric Circulation Patterns (2008, neutral): “46, SLP ﬁelds from a coupled atmosphere– ocean model [ECHAM5/MPI-OM at T63L31 resolution in the framework of the 4 th Intergov-ernmental Panel on Climate Change (IPCC) assessment report 132 , 156 , 157 ] are evaluated us-ing ERA-40 reanalysis data for 1961–2000.”
GCM intercomparison of global cloud regimes: present-day evaluation and climate change response (2007, background): “…(all are atmosphere—mixed-layer ocean configurations of the model) Model Resolution Nature of cloud scheme Main references ECHAM5 T63 L32 Prognostic Roeckner et al. (2003) HadSM3 N48 L19 Diagnostic Pope et al. (2002); Williams et al (2001) HadSM4 N48 L38 Ddiagnostic Webb et al. (2001) HadGSM1 N96…”