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|Storage:||The size of this collection is 710 bytes|
|Created:||Apr 19, 2016 at 2:21 a.m.|
|Last updated:|| Oct 05, 2016 at 2:52 p.m.
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A large imbalance between recharge and water withdrawal has caused vital regions of the High Plains Aquifer (HPA) to experience significant declines in storage. A new predevelopment map coupled with a synthesis of annual water levels demonstrates that aquifer storage has declined. This collection gives the 1935 to 1937 groundwater levels in the HPA. This dataset, produced using methods described in Haacker, E. M., Kendall, A. D., & Hyndman, D. W. (2015).
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Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
High Plains Aquifer
|High Plains Aquifer 1935 Groundwater Levels||Resource||Tian Gan||Public & Shareable|
|High Plains Aquifer 1936 Groundwater Levels||Resource||Tian Gan||Public & Shareable|
|High Plains Aquifer 1937 Groundwater Levels||Resource||Tian Gan||Public & Shareable|
|This resource is described by||Haacker, E. M. K., Kendall, A. D. and Hyndman, D. W. (2016), Water Level Declines in the High Plains Aquifer: Predevelopment to Resource Senescence. Groundwater, 54: 231–242. doi:10.1111/gwat.12350|
How to Cite
Haacker, E. M., A. D. Kendall, D. W. Hyndman (2016). High Plains Groundwater Levels, HydroShare, http://www.hydroshare.org/resource/89a37c54bcae4a499351a39b4797998a
This resource is shared under the Creative Commons Attribution CC BY.http://creativecommons.org/licenses/by/4.0/
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