Metadata | Start Date | End Date | Comment |
---|---|---|---|
CP04OSSM-RID27-01-OPTAAD000 |
There is no pressure variable in the .nc files. This should be a coordinate. By Lori Garzio, on 6/28/19 |
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CP04OSSM-RID27-01-OPTAAD000 Deployment: 1 |
recovered_host data aren't expected - according to the ingest csv the raw data files are blank. This dataset should be annotated. By Lori Garzio, on 6/28/19 |
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CP04OSSM-RID27-01-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 6/28/19 |
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CP04OSSM-MFD37-01-OPTAAD000 Deployment: 6 |
99% of the beam_attenuation values for this deployment are nans, outside of global ranges, or outliers (+/-5 SD). By Lori Garzio, on 6/28/19 |
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CP04OSSM-MFD37-01-OPTAAD000 Deployment: 1 |
beam_attenuation and optical_absorption are arrays of fill values for this deployment. By Lori Garzio, on 6/28/19 |
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CP04OSSM-MFD37-01-OPTAAD000 Deployment: 5 |
wavelength_a and wavelength_c are arrays of fill values for this deployment. These variables should contain the measurement wavelengths. By Lori Garzio, on 6/28/19 |
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CP04OSSM-MFD37-01-OPTAAD000 Deployment: 2 |
recovered_host data aren't available for download for this deployment. According to the ingest csv, the raw data files are available. These files should be ingested or the dataset should be annotated. By Lori Garzio, on 6/28/19 |
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CP04OSSM-MFD37-01-OPTAAD000 |
There is no pressure variable in the .nc files. This should be a coordinate. By Lori Garzio, on 6/28/19 |
||
CP04OSSM-MFD37-01-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 6/28/19 |
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CP03ISSM-RID27-01-OPTAAD000 Deployment: 7 |
47% and 68% of the beam_attenuation and optical_absorption values for this deployment are nans, fill values, outside of global ranges, or outliers (+/-5 SD). By Lori Garzio, on 6/28/19 |
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CP03ISSM-RID27-01-OPTAAD000 Deployment: 4 |
38%-44% of the beam_attenuation and optical_absorption values for this deployment are nans, fill values, outside of global ranges, or outliers (+/-5 SD). By Lori Garzio, on 6/28/19 |
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CP03ISSM-RID27-01-OPTAAD000 Deployment: 2 |
97% of the optical_absorption values for this deployment are nans, fill values, outside of global ranges, or outliers (+/-5 SD). By Lori Garzio, on 6/28/19 |
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CP03ISSM-RID27-01-OPTAAD000 Deployment: 1 |
optical_absorption is an array of fill values for this deployment. By Lori Garzio, on 6/28/19 |
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CP03ISSM-RID27-01-OPTAAD000 |
There is no pressure variable in the .nc files. This should be a coordinate. By Lori Garzio, on 6/28/19 |
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CP03ISSM-RID27-01-OPTAAD000 Deployment: 5 |
In one of the deployment 5 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 0-88. By Lori Garzio, on 6/27/19 |
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CP03ISSM-RID27-01-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 6/28/19 |
||
CP03ISSM-MFD37-01-OPTAAD000 Deployment: 2 |
98% of the beam_attenuation and optical_absorption values for this deployment are nans, fill values, outside of global ranges, or outliers (+/-5 SD). By Lori Garzio, on 6/28/19 |
||
CP03ISSM-MFD37-01-OPTAAD000 Deployment: 6 |
wavelength_a and wavelength_c are arrays of fill values for this deployment. These variables should contain the measurement wavelengths. By Lori Garzio, on 6/28/19 |
||
CP03ISSM-MFD37-01-OPTAAD000 |
There is no pressure variable in the .nc files. This should be a coordinate. By Lori Garzio, on 6/28/19 |
||
CP03ISSM-MFD37-01-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 6/28/19 |