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Assessment of two versions of regional climate model in simulating the Indian Summer Monsoon over South Asia CORDEX domain

机译:评估两种版本的区域气候模型,模拟印度夏季风对南亚CORDEX域的影响

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摘要

This study assess the performance of two versions of Regional Climate Model (RegCM) in simulating the Indian summer monsoon over South Asia for the period 1998 to 2003 with an aim of conducting future climate change simulations. Two sets of experiments were carried out with two different versions of RegCM (viz. RegCM4.2 and RegCM4.3) with the lateral boundary forcings provided from European Center for Medium Range Weather Forecast Reanalysis (ERA-interim) at 50 km horizontal resolution. The major updates in RegCM4.3 in comparison to the older version RegCM4.2 are the inclusion of measured solar irradiance in place of hardcoded solar constant and additional layers in the stratosphere. The analysis shows that the Indian summer monsoon rainfall, moisture flux and surface net downward shortwave flux are better represented in RegCM4.3 than that in the RegCM4.2 simulations. Excessive moisture flux in the RegCM4.2 simulation over the northern Arabian Sea and Peninsular India resulted in an overestimation of rainfall over the Western Ghats, Peninsular region as a result of which the all India rainfall has been overestimated. RegCM4.3 has performed well over India as a whole as well as its four rainfall homogenous zones in reproducing the mean monsoon rainfall and inter-annual variation of rainfall. Further, the monsoon onset, low-level Somali Jet and the upper level tropical easterly jet are better represented in the RegCM4.3 than RegCM4.2. Thus, RegCM4.3 has performed better in simulating the mean summer monsoon circulation over the South Asia. Hence, RegCM4.3 may be used to study the future climate change over the South Asia.
机译:这项研究评估了两个版本的区域气候模式(RegCM)在模拟1998年至2003年南亚印度夏季风的性能,目的是进行未来的气候变化模拟。使用两种不同版本的RegCM(即RegCM4.2和RegCM4.3)进行了两组实验,并从欧洲中距离天气预报重新分析中心(ERA-interim)以50 km的水平分辨率提供了横向边界强迫。与较早版本的RegCM4.2相比,RegCM4.3的主要更新是包括测量的太阳辐照度,以代替硬编码的太阳常数和平流层中的附加层。分析表明,在RegCM4.3中,印度夏季风的降雨,水分通量和地表净下行短波通量要比RegCM4.2模拟更好。 RegCM4.2模拟中阿拉伯海北部和印度半岛上过多的水气通量导致对半岛西部西高止山脉地区降雨的高估,因此,印度的全部降雨都被高估了。 RegCM4.3在整个印度及其四个降雨同质带方面表现良好,能够再现平均季风降雨和年际降雨变化。此外,RegCM4.3比RegCM4.2更好地代表了季风爆发,低空的索马里急流和热带的东风急流。因此,RegCM4.3在模拟南亚夏季平均季风环流方面表现更好。因此,RegCM4.3可用于研究南亚未来的气候变化。

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