| Dep. | Preferred Method | Stream | DD | FD | SG | EG | Gaps | GD | TS | Rate (s) | Pressure Comp. | Time Order | Valid Data | Missing Data | Data Comp. | Missing Coords. | Review |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 1 | recovered_host | / | Complete | ||||||||||||||
| 2 | recovered_host | 361 | 361 | 0 | 0 | 0 | 0 | 1,436,076 | 12 / | 1 | 2 | 3 | Complete | ||||
| 3 | recovered_host | 445 | 441 | 0 | 0 | 7 | 9 | 1,722,250 | 12 / | 1 | 2 | 3 | Complete |
| Deployment: | 1 | 2 | 3 |
|---|---|---|---|
| 100% | 99% |
| Deployment: | 1 | 2 | 3 |
|---|---|---|---|
| 2 | 0.00 | ||
| 3 | 11.91 | 0.00 |
| Metadata | Start Date | End Date | Comment |
|---|---|---|---|
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GA01SUMO-RID16-01-OPTAAD000 Stream: optaa_dj_dcl_instrument |
3/15/15, 5:25 PM |
Per vendor feedback, the first 1-2 min of each AC-S instrument sampling period should be considered suspect. Signal drift can occur as the instrument warms up, flushes with seawater, and the filter wheel spins up. Id: 1797 By: swhite |
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GA01SUMO-RID16-01-OPTAAD000 Stream: optaa_dj_dcl_instrument_recovered |
3/15/15, 5:25 PM |
Per vendor feedback, the first 1-2 min of each AC-S instrument sampling period should be considered suspect. Signal drift can occur as the instrument warms up, flushes with seawater, and the filter wheel spins up. Id: 1798 By: swhite |
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GA01SUMO |
3/15/15, 5:25 PM | 11/26/15, 5:08 AM |
Deployment 1: Buoy log files showed that seawater was first detected inside the buoy well on 3/26/2015. Both leak detectors showed increasing presence of water over the period of deployment. Upon recovery of the mooring, no external damage was visible and the buoy did not appear to be floating lower than normal. Id: 653 By: lgarzio |
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GA01SUMO-RID16-01-OPTAAD000 |
3/15/15, 5:25 PM | 11/26/15, 5:08 AM |
Deployment 1: Upon recovery, both flow channels were detached from the unit (one was missing entirely). Id: 659 By: lgarzio |
| Metadata | Start Date | End Date | Comment |
|---|---|---|---|
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GA01SUMO-RID16-01-OPTAAD000 |
According to Roesler and Barnard (Optical proxy for phytoplankton biomass in the absence of photophysiology: Rethinking the absorption line height, Methods in Oceanography, 2013), “absorption meters are highly prone to biofouling, particularly biofilms which not only attenuate the collimated beam but also impact the scattering properties of the optical surfaces and tubes. In productive coastal waters biofouling can have significant impacts (i.e. 10% of the signal) within one to two weeks”. By Lori Garzio, on 6/27/19 |
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GA01SUMO-RID16-01-OPTAAD000 |
There is no pressure variable in the .nc files. This should be a coordinate. By Lori Garzio, on 6/27/19 |
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GA01SUMO-RID16-01-OPTAAD000 Deployment: 1 |
In one of the deployment 1 recovered_host netcdf files (in the location attached), the wavelength dimension is an array of -9999999. The wavelength dimension in the other 2 files from that deployment is an index from 0-86. By Lori Garzio, on 6/26/19 |
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GA01SUMO-RID16-01-OPTAAD000 Deployment: 2 |
wavelength_a and wavelength_c are arrays of fill values for this deployment. These variables should contain the measurement wavelengths. By Lori Garzio, on 6/27/19 |
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GA01SUMO-RID16-01-OPTAAD000 Deployment: 3 |
Approximately 90% of the data for beam_attenuation and optical_absorption for this deployment are nans, fill values, outside of global ranges or outliers (+/- 5 SD) By Lori Garzio, on 6/27/19 |