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Glacier loss and hydro-social risks in the Peruvian Andes

机译:秘鲁安第斯山脉的冰川损失和水社会风险

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Accelerating glacier recession in tropical highlands and in the Peruvian Andes specifically is a manifestation of global climate change that is influencing the hydrologic cycle and impacting water resources across a range of socio-environmental systems. Despite predictions regarding the negative effects of long-term glacier decline on water availability, many uncertainties remain regarding the timing and variability of hydrologic changes and their impacts. To improve context-specific understandings of the effects of climate change and glacial melt on water resources in the tropical Andes, this article synthesizes results from long-term transdisciplinary research with new findings from two glacierized Peruvian watersheds to develop and apply a multi-level conceptual framework focused on the coupled biophysical and social determinants of water access and hydro-social risks in these settings. The framework identifies several interacting variables hydrologic transformation, land cover change, perceptions of water availability, water use and infrastructure in local and regional economies, and water rights and governance to broadly assess how glacier change is embedded with social risks and vulnerability across diverse water uses and sectors. The primary focus is on the Santa River watershed draining the Cordillera Blanca to the Pacific. Additional analysis of hydrologic change and water access in the geographically distinct Shullcas River watershed draining the Huaytapallana massif towards the city of Huancayo further illuminates the heterogeneous character of hydrologic risk and vulnerability in the Andes.
机译:特别是热带高地和秘鲁安第斯山脉的冰川衰退加速,是全球气候变化的一种表现,它正在影响整个社会环境系统中的水文循环并影响水资源。尽管有关于冰川长期减少对水供应的负面影响的预测,但关于水文变化的时间和变异性及其影响仍然存在许多不确定性。为了更好地了解气候变化和冰川融化对热带安第斯山脉水资源的影响,根据上下文的不同,本文综合了长期跨学科研究的结果以及两个冰川化的秘鲁流域的新发现,以开发和应用多层次概念该框架的重点是在这些环境中水获取和水社会风险的生物物理和社会决定因素。该框架确定了几个相互影响的变量,水文改造,土地覆盖变化,对水的可利用性的认识,地方和区域经济中的水利用和基础设施以及水权和治理,以广泛评估冰川变化如何在各种水利用中嵌入社会风险和脆弱性和部门。主要重点是圣诞老人河分水岭,将科迪勒拉·布兰卡排到太平洋。在地理上独特的舒尔卡斯河流域中,将Huaytapallana地块排入Huancayo市的水文变化和取水情况的进一步分析进一步阐明了安第斯山脉水文风险和脆弱性的异质性。

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