ALBERT

Description: [1]  The climatology, seasonality, and intraseasonal to interannual variability of the temperature field near the cold-point tropopause (CPT) are examined using the state-of-the-art climate models that participated in the Coupled Model Intercomparison Project Phase 5 (CMIP5). Both historical simulations and future projections based on the Representative Concentration Pathway (RCP) 8.5 scenario are used to evaluate model performance and to identify potential changes in the CPT temperature, which is estimated using both the 100-hPa and zero-lapse-rate (ZLR) temperatures. It is found that historical simulations successfully reproduce the spatio-temporal structure of the CPT temperature in comparison to reanalysis data. The interannual variability associated with El Niño-Southern Oscillation and intraseasonal variability associated with equatorial waves are also reasonably well captured. However, the models show non-negligible biases in several aspects: 1) most models have a warm bias around the CPT; 2) large inter-model differences occur in the amplitude of the seasonal cycle in 100-hPa temperature; 3) several models overestimate lower stratospheric warming in response to volcanic aerosols; 4) temperature variability associated with the quasi-biennial oscillation and Madden-Julian oscillation is absent in most models; 5) equatorial waves near the CPT exhibit a wide range of variations among the models with unrealistically persistent Kelvin waves in several models. In the RCP 8.5 scenario, the models predict robust warming both at the 100-hPa and ZLR levels, but cooling at the 70-hPa level. A weakened seasonal cycle in the temperature is also predicted in most models at both the 100- and 70-hPa levels. These findings may have important implications for cross-tropopause water vapor transport and related global climate change and variability.