Naldmann et al.
from different sources can occur because of improper definition
and inadequate uncertainty assignment.
Outloo!
The presented approach to quantify uncertainties of
measured EOVs in a practical manner has been presented on
che basis of temperature measurements. The parameter can be
directly measured using a single datum that can immediately be
zalibrated with a temperature standard. Moreover, temperature
sensors show good long-term stability. The collected time series
have shown that measurement results of all sensors are matching
well even after some months. Other EOVs are however more
challenging. Their numerical value has to be calculated from
Jifferent parameters, all having their own uncertainties. Salinity,
for instance, is derived from temperature, conductivity and
pressure measurements. The respective calibration procedure
is relatively elaborate and due to the fact that correlations
between involved parameters exist, the uncertainty calculations
are not straightforward. Moreover, the stability of the sensors is
strongly affected by environmental effects, ie., biofouling. In a
subsequent paper the collected salinity data of the measurement
series will discuss the effect of stability issues and multi-
parameter measurements on the uncertainty quantification of
measured ocean variables.
Other contributions to uncertainty quantifications have to
ve considered as well. One example would be the pressure
sensitivity of temperature in profiling observations, such as
shipboard CTD and Deep ARGO observations (Uchida et al.,
2015)). Checking the time drift of temperature sensors in
profiling float observations (Oka, 2005), would be another
important topic, as profiling floats are not usually recovered
and therefore post-observation calibrations for the temperature
sensors are not possible.
Similar initiatives to enable the quantification of
ancertainties had been started like the US CLIVAR Working
group on Ocean Uncertainty Quantification (US-CLIVAR,
2020) and the International Quality-Controlled Ocean
Database (Cowley, 2021). In the publication of Cowley et al.
an additional aspect is mentioned that is described as the
“Representativeness Errors”. This aspect is putting the
uncertainty assessment in the framework of what processes
shall be observed and what type of fluctuations can be
expected. Because here assumptions have to be made that are
-rontiers in Marine Science
IE
10.3389/fmars.2022.1002153
telated to the used models this contribution to the uncertainty
will probably change over time.
With this study a contribution to the UN Decade for Ocean
Sciences shall be made. It will be a unique opportunity to use
established platforms like the IODE Ocean Best Practice System
(IODE, 2022) to disseminate the ideas and methods developed
here. A close interaction with expert groups within WMO is
already ongoing and will provide an additional impulse bridging
the existing gap between ocean and meteorological practices.
Data availability statemer.t
The datasets presented in this study can be found in online
repositories. The names of the repository/repositories and
accession number(s) can be found below: PANGAEA - https://
doi.,pangaea.de/10.1594/PANGAEBA.942643.
Author contributions
CW, PF, and HB conceptualized the experiment, SS was
overseeing and contributed to the systematic application of
metrological principles, MK and J-GF did the oceanographic
evaluation of the complete data set, MB designed the
experimental set-up and evaluated the sensor performance
during the lifetime of the study, SW carried out all calibration
tasks. RH was contributing to the data management description.
CW wrote an initial draft of this manuscript. All authors
contributed to the article and approved the submitted version.
Fundirng
The project named DAUNE was carried out using existing
junding resources of all involved institutions.
Acknowledgments
The authors very much acknowledge the support by the AWI
Diving Team located on the island of Helgoland who deployed and
safely retrieved all instruments, did the maintenance and repair and
handled all sensor data. We also thank Kai Herklotz from BSH,
Germany, for his support and valuable input.
rrontiersin.org