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|Storage:||The size of this collection is 71 bytes|
|Created:||Apr 19, 2016 at 2:21 a.m.|
|Last updated:|| Oct 31, 2023 at 10:38 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).
|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|
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This resource is shared under the Creative Commons Attribution CC BY.http://creativecommons.org/licenses/by/4.0/