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Research Article

CAS FGOALS-f3-L model dataset descriptions for CMIP6 DECK experiments

CAS FGOALS-f3-L 参加CMIP6 DECK 试验数据介绍

, , , , , , , , , , , , , & show all
Pages 582-588 | Received 04 Apr 2020, Accepted 09 May 2020, Published online: 07 Jul 2020

Figures & data

Table 1. Model configurations of CAS FGOALS-f3-L

Table 2. Experiment designs

Table 3. External forcing settings in piControl, abrupt-4×CO2, and 1pctCO2

Figure 1. (a) Time series of global mean TOA net radiation (units: W m−2) for piControl from model-year 600 to 1160 with a global mean value of 0.31 W m−2, standard deviation of 0.37 W m−2 and climate trend of −0.03 W m−2/100 yr. (b) Time series of global mean SST for piControl from model-year 600 to 1160 with a global mean value of 16.45°C, standard deviation of 0.11°C and climate trend of 0.03°C/100 yr

Figure 1. (a) Time series of global mean TOA net radiation (units: W m−2) for piControl from model-year 600 to 1160 with a global mean value of 0.31 W m−2, standard deviation of 0.37 W m−2 and climate trend of −0.03 W m−2/100 yr. (b) Time series of global mean SST for piControl from model-year 600 to 1160 with a global mean value of 16.45°C, standard deviation of 0.11°C and climate trend of 0.03°C/100 yr

Figure 2. Climate mean distribution of SST (units: °C): (a) observation (1871–1900 mean); (b) FGOALS-f3-L (600–1160 mean)

Figure 2. Climate mean distribution of SST (units: °C): (a) observation (1871–1900 mean); (b) FGOALS-f3-L (600–1160 mean)

Figure 3. Climate mean distribution of precipitation (units: mm d−1): (a) observation (1979–2014); (b) FGOALS-f3-L (600–1160 mean)

Figure 3. Climate mean distribution of precipitation (units: mm d−1): (a) observation (1979–2014); (b) FGOALS-f3-L (600–1160 mean)

Table 4. Surface air temperature responses to abrupt quadrupling of CO2 and 1% yr−1 CO2 increase at 150 model years

Figure 4. Time series of global mean surface air temperature anomalies (units: °C; relative to piControl) for ensemble means of abrupt-4×CO2 and 1pctCO2, respectively. The dashed lines are the three ensemble members, respectively

Figure 4. Time series of global mean surface air temperature anomalies (units: °C; relative to piControl) for ensemble means of abrupt-4×CO2 and 1pctCO2, respectively. The dashed lines are the three ensemble members, respectively

Figure 5. Climate sensitivity of CAS FGOALS-f3-L estimated from the 160-year integrations from abrupt-4×CO2 and associated piControl simulations. The abscissa is the surface air temperature anomaly (units: °C) and the vertical axis is the TOA net radiation anomaly (units: W m−2). The blue dashed lines are the extension lines of the regression lines. (a) r1i1p1f1; (b) r2i1p1f1; (c) r3i1p1f1; (d) ensemble mean

Figure 5. Climate sensitivity of CAS FGOALS-f3-L estimated from the 160-year integrations from abrupt-4×CO2 and associated piControl simulations. The abscissa is the surface air temperature anomaly (units: °C) and the vertical axis is the TOA net radiation anomaly (units: W m−2). The blue dashed lines are the extension lines of the regression lines. (a) r1i1p1f1; (b) r2i1p1f1; (c) r3i1p1f1; (d) ensemble mean

Data availability statement

The data that support the findings of this study are available from https://esgf-node.llnl.gov/projects/cmip6/