尼日利亚几内亚和苏丹-萨赫勒生态区极端降雨指数预估

A. Salihu, A. Abdulkadir, G. N. Nsofor, M. Y. Otache
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摘要

干旱和洪水是极端降雨事件的双重后果。极端降雨事件的负面影响使得了解其在未来气候变化下的行为成为区域规划的必要条件。因此,本研究的目的是预测几内亚和尼日利亚苏丹-萨赫勒生态区的极端降雨指数。采用5天最大降雨量(Rx5day)、强降雨日数(R10mm)、连续湿日数(CWD)和连续干日数(CDD) 4个极端降雨指标。数据和计算使用KNMI气候探索者完成。根据1959-1988年和1989-2018年的基线,对2019-2048年的短期、2049-2078年的中期和2079-2100年的长期进行了预测。采用典型浓度路径(rcp) 2.6、4.5和8.5下的耦合模式比对项目5 (CMIP5)的多模式集合平均值。采用Mann-Kendal统计检验,在0.05显著水平上分析极端降雨指数变化趋势。结果表明,整个几内亚和苏丹-萨赫勒生态区作为最大5天降雨量区域,在所有3个区域均呈现显著的正趋势。对于强降水,RCP2.6相对于所考虑的三个预估期没有显著的正趋势,而RCP4.5和RCP8.5相对于2049 ~ 2078和2079 ~ 2100期有显著的正趋势。CDD的增加和CWD的减少在0.05的置信水平上均不显著。因此,预计这项研究将有助于指导人们了解降雨和与降雨有关的极端事件的持续变化以及可能的变化。这对几内亚和尼日利亚的苏丹-萨赫勒生态区的水资源管理和农业的未来规划也很重要。
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Projected extreme rainfall indices in Guinea and Sudano-sahelian Ecological Zones, Nigeria
Drought and Flood episodes are twin issues that are consequences of extreme rainfall events. The negative impact of extreme rainfall events makes understanding their behaviour under the future climate change necessary for regional planning. Hence, the objective of the study is to project extreme rainfall indices in Guinea and Sudano-Sahelian ecological zones, Nigeria. A set of four extreme rainfall indices namely: maximum 5-day rainfall (Rx5day), heavy rainfall days (R10mm), consecutive wet days (CWD) and consecutive dry days (CDD) were adopted. The data and computation were done using KNMI Climate Explorer. Projections were produced for the near-term 2019-2048, mid-term 2049-2078 and long-term 2079-2100 periods with reference to the 1959-1988 and 1989-2018 baselines. The multi-model ensemble mean of couple model intercomparison project 5 (CMIP5) under representative concentration pathways (RCPs) 2.6, 4.5, and 8.5 were used. Mann-Kendal statistical test was adopted to analyze the trends in extreme rainfall indices at the 0.05 significance level. Based on the results, it can be deduced that there is a significant positive trend in the whole Guinea and Sudano-Sahelian ecological zone as a region for maximum 5-day rainfall with respect to all the three RCPs. As for heavy rainfall, itreveals that there is no significant positive trend for RCP2.6 with respect to the three projected periods under consideration but significant positive trends with respect to 2049-2078 for RCP4.5 as well as RCP8.5 with respect to 2049-2078 and 2079-2100 periods. Increase in CDD, as well as a decrease in CWD, were both not significant at the 0.05 confidence level. Therefore, it is expected that this study will aid guidance to the understanding of the ongoing changes as well as possible changes in rainfall and rainfall-related extremes. It is also important for future planning of water resources management and agriculture in Guinea and Sudano-Sahelian ecological zones of Nigeria.
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