几内亚海岸极端降雨指数的平均值和变率的未来变化以及大西洋赤道模态的作用

K. Worou, T. Fichefet, H. Goosse
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引用次数: 2

摘要

摘要。极端气候的发生可能对农业、供水和能源生产等各个部门产生巨大影响。本研究旨在了解几内亚海岸极端降雨指数的部分变异性,这可能与大西洋赤道模态(AEM)有关,其正相位与降雨事件的强度和频率增加有关。本文利用6个观测降水数据库计算的6个极端指数,以及参与CMIP6第6期耦合模式比对项目(CMIP6)的24个一般环流模式(GCMs)的历史和SSP5-8.5模拟,研究了7 - 9月几内亚海岸极端降水事件的变化。在当前条件下,我们发现当前的gcm明显高估了潮湿事件的频率和连续潮湿日数的最大值。模拟的其他极端指数的幅度都在观测值的范围内,而且分布很大。我们的结果证实了现有的研究。然而,对不同气候条件下与AEM相关的模拟极端降雨的评估关注较少,而AEM的变率预计将在未来减少,并对极端事件产生潜在的重大影响。在这里,我们使用六(1)观测到的降雨(海面温度)数据和24个GCM输出来研究AEM与几内亚海岸极端降雨事件之间的当前、近期、中期和长期未来联系。对AEM的极端降雨响应的偏差在不同的模式和观测中有很大的差异。对于长期未来(2080-2099年),预计降雨事件的频率会降低,强度会增加。例如,连续5个湿润日(rx5天)的多模式集合中位数(EnsMedian)最大降雨量将比当前条件下高21%。此外,预计几内亚海岸上大多数极端指数的变率将增加(长期未来rx5天增加48%)。相比之下,在温暖的气候中,AEM变异性的减少导致几内亚海岸与AEM相关的降雨极端响应的减弱。在目前的条件下,AEM解释了enth中位数rx5天变化的18%,到21世纪末,这一值将减少到8%。因此,在绝对情况下,大多数极端降雨指数的总变率预估会增加,但在未来变暖的气候中,AEM对这种变率的贡献会减弱。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Future changes in the mean and variability of extreme rainfall indices over the Guinea coast and role of the Atlantic equatorial mode
Abstract. The occurrence of climate extremes could have dramatic impacts on various sectors such as agriculture, water supply, and energy production. This study aims to understand part of the variability in the extreme rainfall indices over Guinea coast that can be related to the Atlantic equatorial mode (AEM), whose positive phases are associated with an increase in the intensity and frequency of rainfall events. We use six extreme indices computed from six observed rainfall databases and historical and SSP5-8.5 simulations from 24 general circulation models (GCMs) that participate in the sixth phase of the Coupled Model Intercomparison Project (CMIP6) to study changes in extreme rainfall events over Guinea coast during July–September. Under present-day conditions, we found that current GCMs clearly overestimate the frequency of wet events and the maximum number of consecutive wet days. The magnitude of the other extreme indices simulated is within the range of the observations which, moreover, present a large spread. Our results confirm the existing studies. However, less attention has been paid to the evaluation of the modelled rainfall extremes associated with the AEM under different climate conditions, while the variability of the AEM is expected to decrease in the future, with a potentially significant impact on the extreme events. Here, we use six (one) observed rainfall (sea surface temperature) data and 24 GCM outputs to investigate the present-day, near-term, mid-term, and long-term future links between the AEM and the extreme rainfall events over the Guinea coast. The biases in the extreme rainfall responses to the AEM are subject to a large spread across the different models and observations. For the long-term future (2080–2099), less frequent and more intense rainfall events are projected. As an illustration, the multimodel ensemble median (EnsMedian) maximum rainfall during 5 consecutive wet days (RX5day) would be 21 % higher than under present-day conditions. Moreover, the variability of the majority of the extreme indices over the Guinea coast is projected to increase (48 % for RX5day in the long-term future). By contrast, the decreased variability of the AEM in a warmer climate leads to a reduced magnitude of the rainfall extreme responses associated with AEM over the Guinea coast. While under present-day conditions the AEM explains 18 % of the RX5day variance in the EnsMedian, this value is reduced to 8 % at the end of 21st century. As a consequence, in absolute, there is a projected increase in the total variability of most of the extreme rainfall indices, but the contribution of the AEM to this variability weakens in a warmer future climate.
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