评估全球气温上升1.5°C对牙买加洪水的影响:以Hope流域为例研究

A. Mandal, Tannecia S. Stephenson, Jayaka Campbell, Michael Taylor, Shavel Watson, L. Clarke, David Smith, Junior Darsan, Matthew D. Wilson
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引用次数: 3

摘要

气候变化模型预测,到本世纪末,加勒比盆地内的降雨强度可能会增加,尽管该地区总体上预计会更加干燥。这可能会影响牙买加和加勒比小岛屿发展中国家发生洪水的频率和严重程度。我们以牙买加流域为例,研究了全球平均地表温度比工业化前水平升高1.5、2.0和2.5°C对洪水灾害的影响。分析了PRECIS区域气候模式对加勒比地区的降雨预估。来自模型预测量化不确定性(AENWH, AEXSA, AEXSC, AEXSK, AEXSL和AEXSM)的六名成员利用水文和水力模型为不同的全球变暖水平绘制了希望河的100年洪水淹没图。模型运行预测,升温2.0、2.5和1.5°C时的峰值流量高于历史记录中对流域部分造成破坏的事件的流量。水力模型的预测显示,1.5°C时,流动面积、深度和范围增加,随后温度上升2.0°C和2.5°C。这些结果表明,该流域脆弱地区的洪水风险持续存在。本文是“发展有弹性的能源系统”主题问题的一部分。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
An assessment of the impact of 1.5 versus 2 and 2.5°C global temperature increase on flooding in Jamaica: a case study from the Hope watershed
Climate change models project that, within the Caribbean basin, rainfall intensity is likely to increase toward the end of this century, although the region is projected to be drier overall. This may affect the frequency and severity of floods in Jamaica and the Caribbean Small Island Developing States. We investigate how flood hazards may be affected by increases in global mean surface temperature of 1.5, 2.0 and 2.5°C above pre-industrial levels using a case study of a Jamaican watershed. Rainfall projections from the PRECIS regional climate model for the Caribbean are analysed. Six members from the Quantifying Uncertainty in Model Predictions (AENWH, AEXSA, AEXSC, AEXSK, AEXSL and AEXSM) were used to create 100-year flood inundation maps for the Hope river for different global warming levels using hydrological and hydraulic models. Model runs projected peak discharges at 2.0, 2.5 and 1.5°C warming that were higher than discharges in the historical record of events that damaged sections of the watershed. Projections from the hydraulic model show increased flow area, depth and extent for 1.5 followed by 2.0 and 2.5°C rises in temperature. These results imply continued flood risk for the vulnerable areas of the watershed. This article is part of the theme issue 'Developing resilient energy systems'.
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