肯尼亚水塔对未来气候变化的脆弱性:为流域管理决策提供信息的评估

K. Mwangi, Anthony M. Musili, Viola A. Otieno, H. S. Endris, G. Sabiiti, M. Hassan, A. T. Tsehayu, Artan Guleid, Z. Atheru, A. C. Guzha, Thomas De Meo, N. Smith, D. Makanji, J. Kerkering, B. Doud, E. Kanyanya
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引用次数: 8

摘要

最近的趋势表明,在未来几十年,由于人为和自然压力因素,肯尼亚的自然资源将继续面临巨大压力,这将对包括粮食安全和生计在内的社会经济发展产生更大的负面影响。了解这些压力源的影响是在各个层面制定应对和适应策略的重要一步。肯尼亚水塔在提供供水、木材和非木材林产品等生态系统服务以及调节气候和水的数量和质量等服务方面发挥着关键作用。为了评估水塔对气候变化的脆弱性,本研究采用了IPCC第4次评估报告框架,该框架将脆弱性定义为暴露、敏感性和适应能力的函数。降水历史趋势表明,3 - 4 - 5月(MAM)主雨季降水呈减少趋势,10 - 11 - 12月(OND)短雨季降水呈增加趋势。温度模式与区域一致,具有共同的上升趋势,速率在0.3 ~ 0.5℃/ 10年。预测分析考虑了三种排放情景:低排放(缓解)情景(RCP2.6)、中等水平排放情景(RCP4.5)和高排放(一切照旧)情景(RCP8.5)。高排放情景的结果表明,与1970-2000年的基准期相比,到2050年代(2036-2065年),水塔上空的年温度可能上升3.0°C至3.5°C,到2070年代(2055-2085年未提供结果),温度可能上升3.6°C至4.8°C。研究结果表明,水塔的暴露程度、敏感性和适应能力在大小和空间上都存在差异。这反映在水塔的空间可变脆弱性指数上。水塔的整体脆弱性将增加,导致暴露的生态系统和依赖这些景观提供的生态系统服务的社区的恢复能力受到侵蚀。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Vulnerability of Kenya’s Water Towers to Future Climate Change: An Assessment to Inform Decision Making in Watershed Management
Recent trends show that in the coming decades, Kenya’s natural resources will continue to face significant pressure due to both anthropogenic and natural stressors, and this will have greater negative impacts on socio-economic development including food security and livelihoods. Understanding the impacts of these stressors is an important step to developing coping and adaptation strategies at every level. The Water Towers of Kenya play a critical role in supplying ecosystems services such as water supply, timber and non-timber forest products and regulating services such as climate and water quantity and quality. To assess the vulnerability of the Water Towers to climate change, the study adopted the IPCC AR4 framework that defines vulnerability as a function of exposure, sensitivity, and adaptive capacity. The historical trends in rainfall indicate that the three Water Towers show a declining rainfall trend during the March-April-May (MAM) main rainy season, while the October-November-December (OND) short rainy season shows an increase. The temperature patterns are consistent with the domain having a common rising trend with a rate in the range of 0.3°C to 0.5°C per decade. Projection analysis considered three emissions scenarios: low-emission (mitigation) scenario (RCP2.6), a medium-level emission scenario (RCP4.5), and a high-emission (business as usual) scenario (RCP8.5). The results of the high-emission scenario show that the annual temperature over the Water Towers could rise by 3.0°C to 3.5°C by the 2050s (2036-2065) and 3.6°C to 4.8°C by the 2070s (2055-2085 results not presented), relative to the baseline period 1970-2000. The findings indicate that exposure, sensitivity, and adaptive capacity vary in magnitude, as well as spatially across the Water Towers. This is reflected in the spatially variable vulnerability index across the Water Towers. Overall vulnerability will increase in the water towers leading to erosion of the resilience of the exposed ecosystems and the communities that rely on ecosystem services these landscapes provide.
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