CMIP6 HighResMIP 模型在模拟东非极端降水方面表现如何?

Hassen Babaousmail, B. Ayugi, K. T. C. Lim Kam Sian, Herijaona Hani‐Roge Hundilida Randriatsara, Richard Mumo
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摘要

这项研究评估了九个耦合模式相互比较项目第六阶段(CMIP6)高分辨率模式相互比较项目(HighResMIP)模式及其集合平均值再现 1995-2014 年期间东非极端降水的能力。模型数据集根据两个观测数据集进行评估:CHIRPS和GPCC。考虑的降水指数包括 CDD、CWD、R1mm、R10mm、R20mm、SDII、R95p、PRCPTOT 和 Rx1day。总体结果表明,HighResMIP 模式较好地再现了年变率;但是,HighResMIP 模式之间存在某些一致的偏差,即倾向于高估 CWD 和 R1mm,低估 CDD 和 SDII。利用泰勒图和泰勒技能得分对 HighResMIP 模式进行了排序。结果表明,这些模式合理地模拟了 PRCPTOT、R1mm、R10mm、R95p 和 CDD 等指数,但对 SDII CWD、SDII 和 R20mm 的模拟普遍较差。它们是 CMCC-CM2-VHR4、HadGEM31-MM、HadGEM3-GC31-HM 和 GFDL-CM4。相反,MPI-ESM1-2-XR 和 MPI-ESM1-2-HR 在模拟 OND 季节方面表现出色,但低估了 MAM 季节。比较分析表明,在模拟各种指数方面,多模式模拟的准确性优于单个模式。本研究的结果对于确定 HighResMIP 数据再现东非极端降水事件的能力非常重要,从而有助于决策。然而,鉴于在再现平均降水量方面观察到的总体弱点,在解释基于东非个别 CMIP6 模式的研究结果时应谨慎。
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How do CMIP6 HighResMIP Models Perform in Simulating Precipitation Extremes over East Africa?
This work assesses the ability of nine Coupled Model Intercomparison Project phase 6 (CMIP6) High-Resolution Model Intercomparison Project (HighResMIP) models and their ensemble mean to reproduce precipitation extremes over East Africa for the period 1995–2014. The model datasets are assessed against two observation datasets: CHIRPS and GPCC. The precipitation indices considered are CDD, CWD, R1mm, R10mm, R20mm, SDII, R95p, PRCPTOT, and Rx1day. The overall results show that HighResMIP models reproduce annual variability fairly well; however, certain consistent biases are found across HighResMIP models, which tend to overestimate CWD and R1mm and underestimate CDD and SDII. The HighResMIP models are ranked using the Taylor diagram and Taylor Skill Score. The results show that the models reasonably simulate indices, such as PRCPTOT, R1mm, R10mm, R95p, and CDD; however, the simulation of SDII CWD, SDII, and R20mm is generally poor. They are CMCC-CM2-VHR4, HadGEM31-MM, HadGEM3-GC31-HM, and GFDL-CM4. Conversely, MPI-ESM1-2-XR and MPI-ESM1-2-HR show remarkable performance in simulating the OND season while underestimating the MAM season. A comparative analysis demonstrates that the MME has better accuracy than the individual models in the simulation of the various indices. The findings of the present study are important to establish the ability of HighResMIP data to reproduce extreme precipitation events over East Africa and, thus, help in decision making. However, caution should be exercised in the interpretation of the findings based on individual CMIP6 models over East Africa given the overall weakness observed in reproducing mean precipitation.
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