Toward hydro-social modeling: Merging human variables and the social sciences with climate-glacier runoff models (Santa River, Peru)

被引:84
作者
Carey, Mark [1 ]
Baraer, Michel [2 ]
Mark, Bryan G. [3 ,4 ]
French, Adam [5 ]
Bury, Jeffrey [5 ]
Young, Kenneth R. [6 ]
McKenzie, Jeffrey M. [7 ]
机构
[1] Univ Oregon, Robert D Clark Honors Coll, Eugene, OR 97403 USA
[2] Univ Quebec, Ecole Technol Super, Ste Foy, PQ G1V 2M3, Canada
[3] Ohio State Univ, Dept Geog, Columbus, OH 43210 USA
[4] Ohio State Univ, Byrd Polar Ctr, Columbus, OH 43210 USA
[5] Univ Calif Santa Cruz, Dept Environm Studies, Santa Cruz, CA 95064 USA
[6] Univ Texas Austin, Dept Geog & Environm, Austin, TX 78712 USA
[7] McGill Univ, Montreal, PQ H3A 2T5, Canada
基金
美国国家科学基金会; 加拿大自然科学与工程研究理事会;
关键词
Glacial melt; Climate change; Glacier runoff modeling; Social-ecological systems; Cordillera Blanca; Tropical Andes; CORDILLERA-BLANCA; WATER-RESOURCES; MELTWATER CONTRIBUTION; HUMAN VULNERABILITY; STREAM DISCHARGE; NORTH-AMERICA; ALPINE BASINS; RECESSION; FUTURE; SIMULATION;
D O I
10.1016/j.jhydrol.2013.11.006
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Glacier shrinkage caused by climate change is likely to trigger diminished and less consistent stream flow in glacier-fed watersheds worldwide. To understand, model, and adapt to these climate-glacier-water changes, it is vital to integrate the analysis of both water availability (the domain of hydrologists) and water use (the focus for social scientists). Drawn from a case study of the Santa River watershed below Peru's glaciated Cordillera Blanca mountain range, this paper provides a holistic hydro-social framework that identifies five major human variables critical to hydrological modeling because these forces have profoundly influenced water use over the last 60 years: (1) political agendas and economic development; (2) governance: laws and institutions; (3) technology and engineering; (4) land and resource use; and (5) societal responses. Notable shifts in Santa River water use-including major expansions in hydroelectricity generation, large-scale irrigation projects, and other land and resource-use practices did not necessarily stem from changing glacier runoff or hydrologic shifts, but rather from these human variables. Ultimately, then, water usage is not predictable based on water availability alone. Glacier runoff conforms to certain expected trends predicted by models of progressively reduced glacier storage. However, societal forces establish the legal, economic, political, cultural, and social drivers that actually shape water usage patterns via human modification of watershed dynamics. This hydro-social framework has widespread implications for hydrological modeling in glaciated watersheds from the Andes and Alps to the Himalaya and Tien Shan, as well as for the development of climate change adaptation plans. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:60 / 70
页数:11
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