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Performance of decadal prediction in Coupled Model Intercomparisson Project Phase 5 (CMIP5) on projecting climate in tropical area

机译:在热带地区突出的耦合模型中偶联型截面项目第5(CMIP5)中的分型预测性能

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Skill of BCC-CSM1.1, MPI-ESM-LR and IPSL-CM5A-LR (climate models which are collected together in Coupled Model Intercomparison Project Phase 5) on projecting precipitation, air temperature and sea surface temperature (SST) in tropical region were analyzed during December-January-February (DJF) and June-July-August (JJA) using Empirical Orthogonal Functions (EOF), climatology, bias and Root Mean Square Error (RMSE) parameters. These models were compared with the reanalysis/observation data. The results showed that dominant modes (EOF1) of all models for air temperature were similar with the mode of reanalysis data. In general, EOF1 of all models for precipitation are similar with mode of the observation which is dominated by positive (negative) anomaly in northern (southern) equator. Climatology of precipitation, air temperature and sea surface temperature showed that high values were located in southern equator during DJF and shifted to the north during JJA. The highest air temperature bias was located in Africa (around 6°C during DJF and JJA) for MPI-ESM-LR. In addition all models captured the ITCZ signal. The highest RMSE and bias of precipitation (> 9 and 5 mm/day) were located in western Pacific in BCC-CSM1.1 during DJF and IPSL-CM5A-LR during JJA. BCC-CSM1.1 had higher RMSE (> 9 mm/day) in projecting precipitation in Papua and Borneo, MPI-ESM-LR detected higher bias in Sumatra, Java, Nusa Tenggara, while IPSL-CM5A-LR in Sumatra. The highest RMSE for SST (more than 2°C) was located in the eastern Pacific.
机译:BCC-CSM1.1,MPI-ESM-LR和IPSL-CM5A-LR的技能(在耦合型号相互熟悉的项目第5阶段收集的气候模型)在热带地区突出,空气温度和海表面温度(SST)在12月至2月(DJF)和6月至8月(JJA)的分析了使用经验正交功能(EOF),气候学,偏见和均方根误差(RMSE)参数。将这些模型与再分析/观察数据进行比较。结果表明,所有用于空气温度模型的主导模式(EOF1)与再分析数据的模式相似。通常,沉淀的所有模型的EOF1与观察模式类似的模式,其由北部(南部)赤道的正(负)异常主导。降水,空气温度和海面温度的气候学表明,在DJF期间,高值位于南部赤道中,并在JJA期间转移到北部。最高的空气温度偏置位于非洲(DJF和JJA期间约6°C),用于MPI-ESM-LR。此外,所有型号均捕获ITCZ信号。在JJA期间,在DJF和IPSL-CM5A-LR期间,沉淀(> 9和5mm /天)的最高RMSE和偏差(> 9和5 mm /天)位于BCC-CSM1.1。 BCC-CSM1.1具有更高的RMSE(> 9毫米/天)在巴布亚和婆罗洲的突出沉淀方面,MPI-ESM-LR检测到苏门答腊,Java,Nusa Tenggara的更高偏见,而IPSL-CM5A-LR在苏门答腊省。 SST(超过2°C)的最高RMSE位于太平洋东部。

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