Glacier loss and hydro-social risks in the Peruvian Andes

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 eff...

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Published inGlobal and planetary change Vol. 159; pp. 61 - 76
Main Authors Mark, Bryan G., French, Adam, Baraer, Michel, Carey, Mark, Bury, Jeffrey, Young, Kenneth R., Polk, Molly H., Wigmore, Oliver, Lagos, Pablo, Crumley, Ryan, McKenzie, Jeffrey M., Lautz, Laura
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.12.2017
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Abstract 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. •Glacierized hydro-social systems in the Andes are being transformed by global change.•Risks to water access in these systems are heterogeneous, dynamic, and interlinked.•Coupled biophysical and social dimensions mediate and amplify these risks.•A transdisciplinary approach elucidates interactions and feedbacks across dimensions.•A conceptual framework for analyzing these risk dynamics across scales is presented.
AbstractList 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.
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. •Glacierized hydro-social systems in the Andes are being transformed by global change.•Risks to water access in these systems are heterogeneous, dynamic, and interlinked.•Coupled biophysical and social dimensions mediate and amplify these risks.•A transdisciplinary approach elucidates interactions and feedbacks across dimensions.•A conceptual framework for analyzing these risk dynamics across scales is presented.
Author Mark, Bryan G.
French, Adam
Carey, Mark
McKenzie, Jeffrey M.
Lautz, Laura
Polk, Molly H.
Baraer, Michel
Crumley, Ryan
Wigmore, Oliver
Lagos, Pablo
Bury, Jeffrey
Young, Kenneth R.
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Keywords Coupled human-natural systems
Climate change
Transdisciplinary research
Peru
Glacier recession
Water resources
Language English
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Snippet Accelerating glacier recession in tropical highlands and in the Peruvian Andes specifically is a manifestation of global climate change that is influencing the...
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SubjectTerms Andes region
Climate change
Coupled human-natural systems
Glacier recession
glaciers
highlands
hydrologic cycle
infrastructure
land cover
melting
Peru
prediction
risk
rivers
Transdisciplinary research
uncertainty
Water resources
water rights
water utilization
watersheds
Title Glacier loss and hydro-social risks in the Peruvian Andes
URI https://dx.doi.org/10.1016/j.gloplacha.2017.10.003
https://www.proquest.com/docview/2010227188
Volume 159
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