Tropical and Subtropical Cloud Transitions in Weather and Climate Prediction Models: The GCSS/WGNE Pacific Cross-Section Intercomparison (GPCI)
By João Paulo Ramos Teixeira, S. Cardoso, M. Bonazzola, Jason C. Cole, A. Delgenio, C. DeMott, C. Franklin, C. Hannay, C. Jakob, Y. Jiao and 28 more. 2011
146 citations recorded by the source corpus.
AbstractA model evaluation approach is proposed in which weather and climate prediction models are analyzed along a Pacific Ocean cross section, from the stratocumulus regions off the coast of California, across the shallow convection dominated trade winds, to the deep convection regions of the ITCZ—the Global Energy and Water Cycle Experiment Cloud System Study/Working Group on Numerical Experimentation (GCSS/WGNE) Pacific Cross-Section Intercomparison (GPCI). The main goal of GPCI is to evaluate and help understand and improve the representation of tropical and subtropical cloud processes in weather and climate prediction models. In this paper, a detailed analysis of cloud regime transitions along the cross section from the subtropics to the tropics for the season June–July–August of 1998 is presented. This GPCI study confirms many of the typical weather and climate prediction model problems in the representation of clouds: underestimation of clouds in the stratocumulus regime by most models with the co...
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/a3b83e020da1baf662023a3bdf9a7035005c764b
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In Atmospheric Science
- F. Brient
- Axel Von Engeln
- João Paulo Ramos Teixeira
- Sandrine Bony
- Stephen A. Klein
- M. Zelinka
- Chris Bretherton
- M. Webb
In Global and Planetary Change
- F. Brient
- Axel Von Engeln
- João Paulo Ramos Teixeira
- Sandrine Bony
- Stephen A. Klein
- M. Zelinka
- Chris Bretherton
- M. Webb
Citations in the corpus
- Interpretation of the positive low-cloud feedback predicted by a climate model under global warming (2013, background): “CGILS focuses on three cases of boundary-layer clouds occurring along a transect ranging from California to Hawaii (Teixeira et al. 2011) and representative of stratus, stratocumulus and shallow cumulus cloud types (Karlsson et al. 2010).”
- A Planetary Boundary Layer Height Climatology Derived from ECMWF Reanalysis Data (2013, background): “These results naturally confirm previous studies of the evolution of PBL and cloud-top height in this transition region (e.g., von Engeln et al. 2005; Karlsson et al. 2010; Teixeira et al. 2011).”