布基纳法索努豪分盆地的气候预测和未来降雨趋势分析。

Noba Wendkuni, Ghislain, Damiba Lucien, Doumounia Ali, Zongo Inoussa, Zougmoré François
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引用次数: 0

摘要

气候变化是生物圈发生变化的指标。对其进行监测,将有助于预测应对由此产生的灾害的行动。在布基纳法索努瓦霍次盆地开展的这项研究概述了近期、中期和长期的降雨情况。它建立在地区气候模型的基础上,而地区气候模型是全球气候模型降尺度后的气候预测。这些模型是根据温室气体排放和辐射强迫等情景生成的,称为区域浓度路径(RCP)。本研究选择了 RCP 4.5 和 RCP 8.5 两种情景,从而确定了一种降雨区域气候模型,其输出结果根据努豪次盆地观测数据进行了修正,突出显示了次盆地未来降水量的变化。在三种定义的正常情况下,即正常 1(2021-2050 年)、正常 2(2051-2080 年)和正常 3(2071-2100 年),累积年降雨量均值在 RCP 4.5 情景下呈下降趋势,而在 RCP 8.5 情景下呈上升趋势。在 RCP 4.5 情景下,标准化降水指数(SPI)显示,正常 1 开始的年份非常潮湿,然后在正常 2 和正常 3 的年份中,降水量接近正常水平。在 RCP 8.5 情景下,SPI 显示正常年份 1 以干旱年份为主。在正常年份 2 和 3 中,湿润和非常湿润的年份重新占据主导地位。同时,未来降雨的空间动态显示,在 RCP 4.5 情景下,年降雨总量在纬度上向该次流域的东南部移动,而在 RCP 8.5 情景下则向西北部移动。因此,气候预测突显了该次流域未来降水量可能发生的变化。考虑到这一点,可以为该地区实施气候变化适应战略奠定基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Climate projection and future rainfall trends analysis in the Nouhao sub-basin in Burkina Faso.
Climate change is an indicator of changes happening in the biosphere. Monitoring it, will anticipating actions against the resulting disasters. This study, undertaken in Burkina Faso Nouaho sub basin, gives an overview of rainfall in the near, medium and long terms. It is built on regional climates models which are climates projections from global climate models downscaling. These models are generated basis on scenarios like greenhouse gas emissions and radiative forcing called Regional Concentration Pathways (RCP). The two scenarios RCP 4.5 and RCP 8.5 chosen in this study, have enabled to identify a rainfall regional climate model whose output corrected basis on Nouhao sub-basin observation data, highlight changes in sub-basin future precipitation. Over the three defined normal, i.e. normal 1 (2021-2050), normal 2 (2051-2080) and normal 3 (2071-2100), cumulative annual rainfall mean shows a downward trend under the RCP 4.5 scenario, and an upward trend under the RCP 8.5 scenario. The Standardized Precipitation Index (SPI) for the RCP 4.5 scenario shows very wet years at the start of normal 1, before giving way to alternating years close to normal rainfall, in normal 2 and 3. In the RCP 8.5 scenario, the SPI shows a dominance of dry years in normal 1. In normal 2 and 3, wet and very wet years return to dominate. The spatial dynamics of future rainfall, meanwhile, show a latitudinal shift in annual rainfall totals towards the south-east of the sub-basin under the RCP 4.5 scenario, and towards the north-west under the RCP 8.5 scenario. The climate projection thus highlights possible future changes in precipitation in the sub-basin. Its consideration could form the basis for the implementation of climate change adaptation strategies in the area.
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