Autor: |
Madeleine, J.-B. Hourdin, F. Grandpeix, J.-Y. Rio, C. Dufresne, J.-L. Vignon, E. Boucher, O. Konsta, D. Cheruy, F. Musat, I. Idelkadi, A. Fairhead, L. Millour, E. Lefebvre, M.-P. Mellul, L. Rochetin, N. Lemonnier, F. Touzé-Peiffer, L. Bonazzola, M. |
Jazyk: |
angličtina |
Rok vydání: |
2020 |
Předmět: |
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Popis: |
The cloud parameterizations of the LMDZ6A climate model (the atmospheric component of the IPSL-CM6 Earth system model) are entirely described, and the global cloud distribution and cloud radiative effects are evaluated against the CALIPSO-CloudSat and CERES observations. The cloud parameterizations in recent versions of LMDZ favor an object-oriented approach for convection, with two distinct parameterizations for shallow and deep convection and a coupling between convection and cloud description through the specification of the subgrid-scale distribution of water. Compared to the previous version of the model (LMDZ5A), LMDZ6A better represents the low-level cloud distribution in the tropical belt, and low-level cloud reflectance and cover are closer to the PARASOL and CALIPSO-GOCCP observations. Mid-level clouds, which were mostly missing in LMDZ5A, are now better represented globally. The distribution of cloud liquid and ice in mixed-phase clouds is also in better agreement with the observations. Among identified deficiencies, low-level cloud covers are too high in mid-latitude to high-latitude regions, and high-level cloud covers are biased low globally. However, the cloud global distribution is significantly improved, and progress has been made in the tuning of the model, resulting in a radiative balance in close agreement with the CERES observations. Improved tuning also revealed structural biases in LMDZ6A, which are currently being addressed through a series of new physical and radiative parameterizations for the next version of LMDZ. ©2020. The Authors. |
Databáze: |
OpenAIRE |
Externí odkaz: |
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