Abstract

Cimarron County, Oklahoma and Union County, New Mexico, neighboring counties in the Southern High Plains, are part of a vital agricultural region in the United States. This region experiences extended periods of cyclical drought threatening its ability to produce, creating an incentive for extensive center pivot irrigation (CPI). Center pivots draw from the rapidly depleting High Plains Aquifer System. As a result, the prospect of long-term sustainability for these agricultural communities is questionable. We use Remote Sensing and Geographic Information Systems to quantify growth in land irrigated by CPI between the 1950s and 2014, and key informant interviews to explore local perspectives on the causes and impact of such growth. In Cimarron County, OK, CPI increased by the mid-1980s, and has continually increased since. Results suggest adaptation to drought, a depleting aquifer, high corn prices, and less rigid groundwater regulations contribute to CPI growth. Conversely, CPI in Union County, NM, increased until 2010, and then declined. Results also suggest that drought-related agricultural changes and more aggressive well drilling regulations contribute to this decrease. Nevertheless, in both counties, there is a growing concern over the depleting aquifer, the long-term sustainability of CPI, and the region’s economic future.

Highlights

  • The decline of the High Plains Aquifer System is considered one of the greatest water management and agricultural concerns currently facing the United States [1]

  • Literature on water governance, vulnerability and resilience is reviewed; second, we provide a description of the study area and comparative study site, as well as the data sources and methods used; third, we present our results from our mixed methods approach; we discuss implications of the results, and conclude that governance plays a major role in influencing center pivot irrigation (CPI) growth and community vulnerability

  • Since the introduction of center pivot irrigation to the High Plains Aquifer System in the mid-20th

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Summary

Introduction

The decline of the High Plains Aquifer System is considered one of the greatest water management and agricultural concerns currently facing the United States [1]. Given the extensive socio-economic implications of groundwater depletion, research that evaluates current groundwater governance policies and explores possible consequences of those policies is expansive [1,3,4,5]. More so, how these consequences contribute to community and agricultural vulnerability, has lead to increasing research on vulnerability, resilience and the role of water governance and politics on sustainable groundwater use [6,7,8,9]. We utilize remote sensing (aerial photograph interpretation) and Geographic Information

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