The purpose of this study was to explore the relationship between teachers' perception of organizational justice and organizational citizenship behavior and to reveal the mediating role of teacher job burnout between teachers' perception of organizational justice and organizational citizenship behavior. This study used a questionnaire to collect data from 857 teachers in 21 secondary schools in Chongqing, China. Through a series of hierarchical regression analyses, mediating effects tests, structural equation modeling tests, and dominance analyses, the findings consistently indicated that procedural justice was a positive predictor of organizational citizenship behavior, while teacher’s job burnout was a negative predictor of organizational citizenship behavior. In addition, the study results also indicated that job burnout had a significant mediating effect on the relationship between teachers' perceptions of organizational justice and organizational citizenship behaviors, particularly with the passion burnout and burnout of professional self-effectiveness.

Two coupled climate models which participated the CMIP6 project (Coupled Model Intercomparison Project Phase 6), the Earth System Model of Chinese Academy of Sciences version 2 (CAS-ESM2-0) and the Nanjing University of Information Science and Technology Earth System Model version 3 (NESM3), were assessed in terms of the impact of four new sea ice parameterization schemes. These four new schemes are related to air-sea heat flux, radiation penetration and absorption, melt ponds, ice-ocean flux, respectively. To evaluate the effectiveness of these schemes, key sea ice variables with and without these new schemes, such as sea ice concentration (SIC) and sea ice thickness (SIT), were compared against observation and reanalysis product from 1980 to 2014. The simulations followed the design of historical experiments within the CMIP6 framework. The results revealed that both models demonstrated improvements in simulating Arctic SIC and SIT when the new parameterization schemes were implemented. The model bias of SIC in some marginal sea ice zones of Arctic was reduced, especially during March. The SIT was increased and the transpolar gradient of SIT was reproduced. The changes of spatial pattern of SIC and SIT after adding new schemes bear similarities between the two coupled models. This suggests that the new schemes have potential for broad application in climate models, especially for those with underestimated SIT.