CAS FGOALS-f3-L Model Datasets for CMIP6 Historical Atmospheric Model Intercomparison Project Simulation
By B. He, Q. Bao, Xiaocong Wang, Linjiong Zhou, Xiaofei Wu, Yimin Liu, Guoxiong Wu, Kangjun Chen, Sicheng He, Wenting Hu and 7 more. Advances in Atmospheric Sciences, 2019
160 citations recorded by the source corpus.
The outputs of the Chinese Academy of Sciences (CAS) Flexible Global Ocean-Atmosphere-Land System (FGOALS-f3-L) model for the baseline experiment of the Atmospheric Model Intercomparison Project simulation in the Diagnostic, Evaluation and Characterization of Klima common experiments of phase 6 of the Coupled Model Intercomparison Project (CMIP6) are described in this paper. The CAS FGOALS-f3-L model, experiment settings, and outputs are all given. In total, there are three ensemble experiments over the period 1979–2014, which are performed with different initial states. The model outputs contain a total of 37 variables and include the required three-hourly mean, six-hourly transient, daily and monthly mean datasets. The baseline performances of the model are validated at different time scales. The preliminary evaluation suggests that the CAS FGOALS-f3-L model can capture the basic patterns of atmospheric circulation and precipitation well, including the propagation of the Madden-Julian Oscillation, activities of tropical cyclones, and the characterization of extreme precipitation. These datasets contribute to the benchmark of current model behaviors for the desired continuity of CMIP.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/ef7635eba36ec25c889177f9fdfa09b3754e9e30
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
In Global and Planetary Change
Citations in the corpus
- Emergent constraints on equilibrium climate sensitivity in CMIP5: do they hold for CMIP6? (2020, background): “, 2010; Hirota et al., 2011). This index is defined as the climatological annual mean precipitation bias averaged 290 over the south-eastern Pacific (30°S – 0°, 150°W – 100°W). The southern ITCZ index is calculated in mm day and dominated by the so-called double ITCZ, a common problem in many CMIP5 ”