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.
Complete Metadata
| accessLevel | public |
|---|---|
| bureauCode |
[
"010:12"
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|
| contactPoint |
{
"fn": "Jeffrey Kennedy",
"@type": "vcard:Contact",
"hasEmail": "mailto:jkennedy@usgs.gov"
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|
| description | 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. |
| distribution |
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| identifier | http://datainventory.doi.gov/id/dataset/USGS_56e9e4b7e4b0f59b85d81a70 |
| keyword |
[
"Hydrology",
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|
| modified | 2020-08-07T00:00:00Z |
| publisher |
{
"name": "U.S. Geological Survey",
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|
| spatial | -114.84558105371, 32.458421888315, -114.72473144435, 32.652882499534 |
| theme |
[
"Geospatial"
]
|
| title | Relative-gravity differences from the 2014 Minute 319 Pulse Flow in the Colorado River Delta |
