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Full text: A methodology to uncertainty quantification of essential ocean variables

Naldmann et al. 
tests vary depending on the scientific party providing the data. 
Additionally, definitions for the used codes vary, although there 
are a number of similarities between the used conventions. For 
example, flagging schemes based on OceanSITES (OceanSITES, 
2020), ARGO (Wong et al., 2022), Copernicus (Copernicus, 
2020), and SeaDataNet (2010) follow the convention that “no 
quality test performed” is defined as flag=“0”, while schemes 
based on GO-SHIP (Swift, 2010) use flag=1 and (UNESCO, 
2013) and I0OS (Bushnell, 2020) use flag=2 for the same. This 
causes major efforts regarding the mapping of flag information 
between the data providers. Interpretation of quality flags 
coming along with data from different data providers can thus 
be very time consuming for the user. Another issue can occur in 
the case of a lack of information about the results of individual 
quality tests when data meant for a specific purpose do not meet 
chese predefined quality criteria and are excluded although they 
may be useful for other scientific questions under consideration. 
Data flagging is therefore highly useful as a plausibility filter 
to exclude wrong data from datasets without a detailed 
knowledge of the specific sensor characteristics and 
{unctionality as well as without a specific knowledge on the 
later scientific question. Data flagging however cannot replace a 
quality assurance procedure providing statistically robust 
Juantitative information on the data’s uncertainty at a 
specified confidence range. 
Another contribution to the overall uncertainty budget can 
be extracted from the sensor specifications determined in the 
manufacturer laboratory at the time of production and 
zalibration that also should find entry into the metadata 
description of measured data. Most sensor manufacturers 
provide initial accuracy and precision values for their sensors 
and sometimes also information about the stability or drift over 
:ime. Even though this information is exactly the type of 
metadata required to calculate a sensor’s uncertainty or 
confidence, one has to keep in mind that these manufacturer 
metadata are laboratory values referring to a brand-new or re- 
calibrated sensor and therefore do not take the sensor lifetime 
and environmental conditions during storage, transportation 
and/or deployment into account. Furthermore, it must be 
zonsidered that manufacturers sometimes provide only 
information for their sensors describing a typical accuracy 
and/or precision for a sensor but not for a specific sensor 
instance. Better qualified sensor specific metadata are only 
available if the manufacturer provides a sensor specific 
zalibration sheet with detailed information on the serial 
number of the respective sensor or if a recalibration will be 
carried out by another calibration laboratory. Therefore, we have 
to consider different levels of availability and reliability of given 
sensor accuracies indicating the demand for proper 
documentation of sensor metadata. 
As mentioned before, flags are markers for data plausibility 
and provide workflow transparency. They do not include 
detailed information about the significance or robustness of a 
Zrontiers ın Marıne Science 
ji 
10.3389/fmars.2022.1002153 
single data point/measurement. The manufacturers quality 
parameters of a sensor’s data provide this information but 
cannot be easily applied to the operational phase of a 
measurement program. From the scientific point of view the 
knowledge of both information, realistic uncertainty in the 
operational phase of an experiment as well as flags determined 
‘rom plausibility tests, would be helpful to prevent scientists 
‘rom misinterpretation of data. However, while flags can be 
assigned to data points independent from the operational phase 
and status of a measurement, a way to assign uncertainty 
information on sensor measurements in the operational phase 
seem to be largely unknown and not yet widespread in 
ocean sciences. 
Experimental set-'.o 
The experimental setup was designed to be as close as 
possible to a normal monitoring program that would be 
conducted in a coastal area with a duration of several months. 
A balanced experimental approach with six different multi- 
parameter probes [CTD: three Sea & Sun Technology 
(Sea&Sun, 2022) and three Sea-Bird Scientific (Seabird, 2022)] 
(see also Supplementary Materials, Appendix 1, Table Al for 
more details) from four different marine institutes in Germany 
were chosen. These six probes were deployed in the MarGate 
underwater test site (Wehkamp et al., 2013) off Helgoland in the 
southern North Sea from July 20° to November 25", 2020. This 
underwater experimental field is jointly operated by the two 
Helmholtz institutes, Alfred-Wegener-Institute Helmholtz 
Centre for Polar- and Marine Research (AWI) and the 
Helmholtz Institute HEREON (formerly HZG) as an 
.nternational monitoring and test facility for marine observing 
components. It has been part of the EU project Jerico-Next 
Jerico-Next, 2019) where international cooperating partners 
could apply for the financial cover of time slots to evaluate 
marine sensors for scientific purposes. 
The experimental area has a cable connected underwater 
aode with ten submersed ports for continuous power and high- 
speed data connection for the remote-controlled operation of 
underwater sensor systems (Fischer, 2019). 
The underwater field is continuously monitored for the main 
essential ocean variables such as temperature, conductivity, 
oxygen saturation, chlorophyll-a, turbidity, photosynthetic 
active radiation (PAR), current and wave height, as well as 
additional variables as pCO2 and methane concentration. 
Experiments in the so called MarGate field are supported year- 
round by specifically trained scientific divers who are responsible 
for sensor maintenance, repairing and replacing of sensors and 
new experimental set up. The area provides a highly demanding 
environment with average wind speed peaks of more than 6 bft 
(10.8-13.8 m/s) on more than 200 days a year and tidal currents 
up to 1 m/s. 
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