Abstract

Reproducibility of precipitation distribution over the tropical oceans for the recent dataset of the Coupled Model Intercomparison Project phase 5 (CMIP5) is investigated and compared to CMIP3. The Taylor skill score for the reproducibility of the CMIP5 multi-model ensemble mean (0.64) is slightly higher than that of CMIP3 (0.60), but the difference is not statistically significant. Still, there is some evidences that the double intertropical convergence zone (ITCZ) bias is mitigated from CMIP3 to CMIP5, whereas the cold tongue bias remains similar. An inter-model empirical orthogonal function analysis shows that these two biases are closely related to the dominant inter-model discrepancies of precipitation patterns. The two biases are attributed to two factors, respectively. In the CMIP5 models with the prominent double ITCZ, the deep convection is not sensitive enough to environmental air humidity at the lower-mid troposphere, as is in CMIP3. Thus, the deep convection is not suppressed even over the dry subsidence region of the southeastern Pacific, forming the double ITCZ bias. Conversely, models with the severe cold tongue bias have lower ocean model resolution with too strong equatorial trades. Therefore, proper representation of the sensitivity of deep convection to humidity and higher resolution of the ocean models with better equatorial trades are important for reducing the double ITCZ and the cold tongue biases.

Highlights

  • Since the Coupled Model Intercomparison Project (CMIP) was launched in 1995, coupled ocean-atmosphere general circulation models developed in dozens of research centers around the world (e.g., Table 1) have been compared and analyzed extensively

  • There is some evidences that the double intertropical convergence zone (ITCZ) bias is mitigated from CMIP3 to Coupled Model Intercomparison Project phase 5 (CMIP5), whereas the cold tongue bias remains similar

  • The inter-model empirical orthogonal function (EOF) analysis indicates that two dominant discrepancies of precipitation distribution among the CMIP5 models are closely related to severity of the double ITCZ and the cold tongue biases

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Summary

Introduction

Since the Coupled Model Intercomparison Project (CMIP) was launched in 1995, coupled ocean-atmosphere general circulation models developed in dozens of research centers around the world (e.g., Table 1) have been compared and analyzed extensively. Zheng et al (2012) analyzed ocean heat budget for the CMIP3 models and showed that overly negative horizontal and vertical heat advection contribute to the cold SST bias. They examined equatorial ocean circulations and thermal structures in models and suggested that these errors in horizontal advection are caused by too strong westward surface currents, and that in vertical advection are associated with excessive upwelling and vertical temperature gradients over the central to eastern Pacific.

Data and method
Precipitation reproducibility in CMIP5 and CMIP3
Findings
Discussion
Summary
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