Metadata | Start Date | End Date | Comment |
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GI05MOAS-GL485-02-DOSTAM000 |
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GI05MOAS-GL485-04-CTDGVM000 |
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RS01SUM2-MJ01B-12-ADCPSK101 Deployment: 1 |
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RS01SUM2-MJ01B-12-ADCPSK101 Deployment: 1 |
Approximately 50% of the seawater velocities for deployment 1 are NaNs, outside of global ranges, or outliers (+/- 5 SD) By Lori Garzio, on 12/18/19 |
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RS01SUM2-MJ01B-12-ADCPSK101 Deployment: 1 |
The .nc files for deployment 1 are missing the coordinates pressure, lat and lon. By Lori Garzio, on 12/18/19 |
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RS03AXBS-LJ03A-10-ADCPTE303 |
40-70% of seawater velocities for deployments 1-3 are NaNs, outside of global ranges, or outliers (+/- 5 SD). By Lori Garzio, on 12/16/19 |
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RS03AXBS-LJ03A-10-ADCPTE303 |
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RS03AXBS-LJ03A-10-ADCPTE303 |
The .nc files for deployments 1-3 are missing the coordinates pressure, lat and lon. By Lori Garzio, on 12/16/19 |
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RS03AXBS-LJ03A-10-ADCPTE303 Deployment: 1 |
Missing data for deployment 1 should be annotated. By Lori Garzio, on 12/16/19 |
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RS01SLBS-LJ01A-10-ADCPTE101 |
40-55% of seawater velocities for deployments 1-3 are NaNs, outside of global ranges, or outliers (+/- 5 SD). By Lori Garzio, on 12/16/19 |
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RS01SLBS-LJ01A-10-ADCPTE101 |
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RS01SLBS-LJ01A-10-ADCPTE101 |
The .nc files for deployments 1-3 are missing the coordinates pressure, lat and lon. By Lori Garzio, on 12/16/19 |
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RS03AXBS-LJ03A-11-OPTAAC303 Deployment: 3 |
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RS03AXBS-LJ03A-11-OPTAAC303 Deployment: 2 |
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RS03AXBS-LJ03A-11-OPTAAC303 |
Missing data at the end of deployments 2 and 3 should be annotated. By Lori Garzio, on 12/13/19 |
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RS03AXBS-LJ03A-11-OPTAAC303 |
There is no pressure variable in the .nc files. This should be a coordinate. By Lori Garzio, on 12/13/19 |
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RS03AXBS-LJ03A-11-OPTAAC303 |
The .nc files for deployments 1-4 are missing the coordinates pressure, lat and lon. By Lori Garzio, on 12/13/19 |
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RS03AXBS-LJ03A-11-OPTAAC303 |
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 12/13/19 |
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RS01SLBS-LJ01A-11-OPTAAC103 Deployment: 3 |
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RS01SLBS-LJ01A-11-OPTAAC103 Deployment: 2 |