Process-level improvements in CMIP5 models and their impact on tropical variability, the Southern Ocean, and monsoons
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Published:2018-01-16
Issue:1
Volume:9
Page:33-67
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ISSN:2190-4987
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Container-title:Earth System Dynamics
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language:en
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Short-container-title:Earth Syst. Dynam.
Author:
Lauer AxelORCID, Jones Colin, Eyring VeronikaORCID, Evaldsson Martin, Hagemann Stefan, Mäkelä JarmoORCID, Martin GillORCID, Roehrig Romain, Wang Shiyu
Abstract
Abstract. The performance of updated versions of the four earth system models (ESMs)
CNRM, EC-Earth, HadGEM, and MPI-ESM is assessed in comparison to their
predecessor versions used in Phase 5 of the Coupled Model Intercomparison
Project. The Earth System Model Evaluation Tool (ESMValTool) is applied to
evaluate selected climate phenomena in the models against observations. This
is the first systematic application of the ESMValTool to assess and document
the progress made during an extensive model development and improvement
project. This study focuses on the South Asian monsoon (SAM) and the West African monsoon (WAM),
the coupled equatorial climate, and Southern Ocean clouds and
radiation, which are known to exhibit systematic biases in present-day ESMs. The analysis shows that the tropical precipitation in three out of four
models is clearly improved. Two of three updated coupled models show an
improved representation of tropical sea surface temperatures with one
coupled model not exhibiting a double Intertropical Convergence Zone (ITCZ).
Simulated cloud amounts and cloud–radiation interactions are
improved over the Southern Ocean. Improvements are also seen in the
simulation of the SAM and WAM, although systematic biases remain in regional
details and the timing of monsoon rainfall. Analysis of simulations with
EC-Earth at different horizontal resolutions from T159 up to T1279 shows
that the synoptic-scale variability in precipitation over the SAM and WAM
regions improves with higher model resolution. The results suggest that the
reasonably good agreement of modeled and observed mean WAM and SAM rainfall
in lower-resolution models may be a result of unrealistic intensity distributions.
Funder
European Commission
Publisher
Copernicus GmbH
Subject
General Earth and Planetary Sciences
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