Seepage-run discharge measurements, June 2, 2022, South Hālawa Stream, North Hālawa Stream, and Hālawa Stream, Oʻahu, Hawaiʻi
Dates
Time Period
2022-06-02
Publication Date
2023-07-17
Citation
Nakama, R.K., Rochester, R.A., Kunishige, V.E., Brunetto, T.R., Rosa, S.N., Pagaduan, L.D., and Stack, J.K., 2023, Seepage Runs of Hālawa Stream, Oʻahu, Hawaiʻi: December 2021 - June 2022: U.S. Geological Survey data release, https://doi.org/10.5066/P9T8W1IM.
Summary
This data release contains a comma-delimited ascii file of six same-day, discrete discharge measurements made at sites along selected reaches of South Hālawa Stream, North Hālawa Stream, and Hālawa Stream, Oʻahu, Hawaiʻi on June 2, 2022. These discrete discharge measurements form what is commonly referred to as a “seepage run.” The intent of the seepage run is to quantify the spatial distribution of streamflow along the reach during fair-weather, low-flow conditions, generally characterized by negligible direct runoff within the reach. The measurements can be used to characterize the net seepage of water into (water gain) or out of (water loss) the stream channel between measurement sites provided that the measurements were made during [...]
Summary
This data release contains a comma-delimited ascii file of six same-day, discrete discharge measurements made at sites along selected reaches of South Hālawa Stream, North Hālawa Stream, and Hālawa Stream, Oʻahu, Hawaiʻi on June 2, 2022. These discrete discharge measurements form what is commonly referred to as a “seepage run.” The intent of the seepage run is to quantify the spatial distribution of streamflow along the reach during fair-weather, low-flow conditions, generally characterized by negligible direct runoff within the reach. The measurements can be used to characterize the net seepage of water into (water gain) or out of (water loss) the stream channel between measurement sites provided that the measurements were made during stable, nonchanging flow conditions (or, in some cases, were made simultaneously during transient flow conditions) and external surface inflows (for example, a tributary) or outflows (for example, a diversion) of water to the reach are quantified and accounted for in the computation of net seepage.
Click on title to download individual files attached to this item.
SR20220602_Halawa.xml Original FGDC Metadata
View
14.84 KB
application/fgdc+xml
SR20220602_Halawa.csv
799 Bytes
text/csv
SR20220602_Halawa.jpg
1.27 MB
image/jpeg
Purpose
The purpose of this data release is to describe measurement methods used and results of six same-day, discrete discharge measurements made at sites along the selected stream reach.