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. 2021 Apr 1;5(4):e2020GH000350. doi: 10.1029/2020GH000350

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© 2021. The Authors.

This is an open access article under the terms of the http://creativecommons.org/licenses/by/4.0/ License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.

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Correlation of intermittent stream flows in the Honouliuli Stream to water levels in the T41 Kunia well and the Ewa Shaft during the latter half of 2016. The well and shaft locations are documented in Figure 1A. Modified from Rosa (2017).