Relative-gravity differences from the 2014 Minute 319 Pulse Flow in the Colorado River Delta

Data are drift-corrected relative gravity differences between stations. Drift correction was carried out by modeling drift as a continuous function of time using polynomial or locally-weighted scatterplot smooth (lowess) curves. The process and software for carrying out drift correction is described in the USGS Arizona Water Science Center QA/QC plan for relative gravity data collection.

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  "010:12"
]

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  "geospatial"
]