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Regional climate change scenarios over South Asia in the CMIP5 coupled climate model simulations

机译:CMIP5耦合气候模型模拟中南亚区域气候变化情景

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This paper evaluates the performance of a suite of state-of-art coupled atmosphere-ocean general circulation models (AOGCMs) in their representation of regional characteristics of hydrological cycle and temperature over South Asia. Based on AOGCM experiments conducted for two types of future greenhouse gas emission scenarios (RCP4.5 and RCP8.5) extending up to the end of 21st century, scenarios of temperature and hydrological cycle are presented. The AOGCMs, despite their relatively coarse resolution, have shown a reasonable skill in depicting the hydrological cycle over the South Asian region. However, considerable biases do exist with reference to the observed hydrological cycle and also inter-model differences. The regional climate change scenarios of temperature (T), atmospheric water balance components, precipitation, moisture convergence and evaporation (P, C and E) up to the end of the 21st century based on CMIP5 modeling experiments conducted for (RCP4.5 and RCP8.5) indicate marked increase in both rainfall and temperature into the 21st century, particularly becoming conspicuous after the 2050s. The monsoon rainfall and atmospheric water balance changes under RCP4.5 and RCP8.5 scenarios are discussed in detail in this paper. Spatial patterns of rainfall change projections indicate maximum increase over South Asia in most of the models. Model simulations under scenarios of increased greenhouse gas concentrations suggests that the intensification of the hydrological cycle is driven mainly by the increased moisture convergence due to increase in the water holding capacity of the atmosphere in a warmer environment, the intensification of the hydrological cycle is greater for RCP8.5 compared to RCP4.5, also fewer models indicate increased variance of temperature and rainfall in a warmer environment. While the scenarios presented in this study are indicative of the expected range of rainfall and water balance changes, it must be noted that the quantitative estimates still have large uncertainties associated with them. Five best model mean reveals the general consensus among the AOGCM results and gives the best estimate of the future projection over the South Asian monsoon region.
机译:本文评估了一套最先进的大气-海洋通用环流模型(AOGCM)在代表南亚水文循环和温度区域特征方面的性能。基于对21世纪末之前的两种未来温室气体排放情景(RCP4.5和RCP8.5)进行的AOGCM实验,提出了温度和水文循环情景。尽管AOGCM的分辨率相对较粗糙,但它们在描述南亚地区的水文循环方面显示出合理的技巧。但是,参考观测的水文循环以及模型间差异确实存在相当大的偏差。根据针对(RCP4.5和RCP8)进行的CMIP5建模实验,到21世纪末为止的温度(T),大气水平衡成分,降水,水分收敛和蒸发(P,C和E)的区域气候变化情景.5)表示进入21世纪的降雨量和温度均显着增加,尤其是在2050年代之后变得明显。本文详细讨论了RCP4.5和RCP8.5情景下的季风降雨和大气水平衡变化。降雨变化预测的空间格局表明,在大多数模型中,南亚的增幅最大。在温室气体浓度增加的情况下的模型模拟表明,水文循环的加剧主要是由于在较温暖的环境中大气持水量增加而导致的水分汇聚增加所致,水文循环的强化更大。与RCP4.5相比,RCP8.5的模型也更少,这表明在温暖的环境中温度和降雨的变化增加。尽管本研究中提出的方案表明了降雨和水平衡变化的预期范围,但必须注意的是,定量估计仍具有很大的不确定性。五个最佳模型均值揭示了AOGCM结果之间的普遍共识,并给出了对南亚季风区域未来预测的最佳估计。

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