Met Office Hadley Centre, Fitzroy Road, Exeter, UK.
Met Office Hadley Centre, Fitzroy Road, Exeter, UK.
Sci Total Environ. 2019 Feb 10;650(Pt 1):1499-1520. doi: 10.1016/j.scitotenv.2018.08.376. Epub 2018 Aug 29.
Climate impacts and adaptation studies often use output from impact models that require data representing future climates at a resolution greater than can be provided by Global Climate Models (GCMs). This paper describes the use of Regional Climate Model (RCM) simulations to generate high-resolution future climate information for assessing climate impacts in the Ganges-Brahmaputra-Meghna (GBM) and Mahanadi deltas as part of the DECCMA project. In this study, three different GCMs (HadGEM2-ES, CNRM-CM5 and GFDL-CM3), all using a single scenario for future greenhouse forcing of the atmosphere (RCP 8.5), were downscaled to a horizontal resolution of 25 km over south Asia using the HadRM3P RCM. These three GCMs were selected based on ability to represent key climate processes over south Asia and ability to sample a range of regional climate change responses to greenhouse gas forcing. RCM simulations of temperature, precipitation, and lower level (850 hPa) atmospheric circulation in the monsoon season (June, July, August, September - JJAS) were compared with observational datasets and their respective driving GCMs to ensure large-scale consistency. Although there are some biases in the RCM simulations, these comparisons indicate that the RCMs are able to simulate realistically aspects of the observed climate of South Asia, such as the monsoon circulation and associated precipitation that are key for informing downstream impacts and adaptation studies. Simulated future temperature and precipitation changes on seasonal and daily timescales suggest increases in both temperature and precipitation across all three models during the monsoon season, with an increase in the amount of extremely heavy precipitation over the GBM and Mahanadi basins. Despite different driving conditions, these results are consistent across all three RCM simulations, providing a level of confidence in the magnitudes and spatial characteristics of temperature and precipitation projections for South Asia.
气候影响和适应研究通常使用需要代表未来气候的数据的影响模型,这些数据的分辨率超过了全球气候模式(GCMs)所能提供的分辨率。本文描述了使用区域气候模式(RCM)模拟来生成高分辨率的未来气候信息,以评估在 Ganges-Brahmaputra-Meghna(GBM)和 Mahanadi 三角洲的气候影响,这是 DECCMA 项目的一部分。在这项研究中,使用 HadRM3P RCM 将三个不同的 GCM(HadGEM2-ES、CNRM-CM5 和 GFDL-CM3)全部使用未来大气温室强迫的单一情景(RCP 8.5)下推到南亚的水平分辨率为 25km。选择这三个 GCM 是基于它们在南亚代表关键气候过程的能力和对温室气体强迫的区域气候变化响应的范围进行抽样的能力。季风季节(6 月、7 月、8 月、9 月-JJAS)的温度、降水和低层(850 hPa)大气环流的 RCM 模拟与观测数据集及其各自的驱动 GCM 进行了比较,以确保大尺度一致性。尽管 RCM 模拟存在一些偏差,但这些比较表明,RCM 能够真实地模拟南亚观测到的气候的某些方面,例如季风环流和相关的降水,这些对于通知下游影响和适应研究是关键的。模拟的未来季节和日时间尺度的温度和降水变化表明,在季风季节,所有三个模型的温度和降水都有所增加,而 GBM 和 Mahanadi 流域的极重度降水增加。尽管驱动条件不同,但这三个 RCM 模拟的结果是一致的,为南亚的温度和降水预测的幅度和空间特征提供了一定程度的信心。