A. Valente et al.: A compilation of global bio-optical in situ data
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Table 1. The standard variables, nomenclatures, and units in the final table
Variable/column Description and units
'dx
ime
‚at
‚on
depth_water
chla_hplc
chla_fluor
mrs_<band =>
aph_ <band>
adg_<band>
bp_<band>
<d_<band =>
sm
stopol1
chla_hplc_dataset
chla_hplc_subdataset
chla_hple_contributor
chla_fluor_dataset
chla_fluor_subdataset
chla_fluor_contributor
s_dataset
rrs_subdataset
"rs_contributor
aph_dataset
aph_subdataset
aph_contributor
adg_dataset
adg_subdataset
adg_contributor
ıbp_dataset
»bp_subdataset
bp_contributor
<d_dataset
<d_subdataset
<d_contributor
sm_dataset
:sm_subdataset
:sm_contributor
dag_time
flag _chl method
Unique key identifying each row
GMT, <YYYY-MM-DD>T<HH:MM:SS>Z
Decimal degree, —90 : 90, south negative
Decimal degree, — 180: 180, west negative
Sampling depth (m) — all assigned to zero
[otal chlorophyll-a concentration determined from HPLC method (mg m73)
Chlorophyll-a concentration determined from fluorometric or spectrophotometric methods (mg m”)
Remote-sensing reflectance (sr” h
Algal pigment absorption coefficient (m!)
Detrital plus CDOM absorption coefficient m7')
Darticle backscattering coefficient (m h
diffuse attenuation coefficient for downward irradiance (m 7!)
Total suspended matter (g m73)
Water depth from ETOPO1 (m)
Metadata string for “chla_hplc”
Metadata string for “chla_hplc”
Metadata string for “chla_hplc”
Metadata string for “chla_fluor”
Metadata string for “chla_fluor”
Metadata string for “chla_fluor”
Metadata string for “rrs”
Metadata string for “rrs”
Metadata string for “rrs”
Metadata string for “aph”
Metadata string for “aph”
Metadata string for “aph”
Metadata string for “adg”
Metadata string for “adg”
Metadata string for “adg”
Metadata string for “bbp”
Metadata string for “bbp”
Metadata string for “bbp”
Metadata string for “kd”
Metadata string for “kd”
Metadata string for “kd”
Metadata string for “tsm”
Metadata string for “tsm”
Metadata string for “tsm”
“1” if observation without time (set to 12:00:00 UTC)
“1” if observation as unknown chlorophyll method
reprocessed in 2017 (“MOBY R2017 reprocessing”) to
include various improvements in the calibration of the
instrument and post-processing, which include: (1) a new
method to extrapolate the upwelling radiance attenuation
coefficient to the surface (Voss et al., 2017); (2) an increase
in arm depth by 0.234 m; and (3) a single pixel shift in
the data for the red spectrograph collected at a bin factor
of 384. Only the last two changes were included in the
present compilation. The first change uses model results to
improve Lw at wavelengths above 575 nm, by correcting
che diffuse upwelling radiance attenuation coefficient for
inelastic effects. Thus for wavelengths above 575 nm, the
Lw21 product in the Gold directory should be investigated.
As mentioned before, the MOBY data compiled in this work
are sensor-specific. Therefore, attention is necessary to use
the correct MOBY data when validating a particular sensor.
The way MOBY data are stored in the final merged table
is consistent with the original wavelengths; however, these
wavelengths can differ from what is sometimes expected
to be the central wavelength of a given band and sensor.
Irrespective of the wavelength where MOBY data are
stored in the final table, for validation of bands 1—6 of
SeaWiFS, MOBY data stored in the final merged table at
412, 443, 490, 510, 555, and 670 nm, respectively, should
attos://doi.org/10.5194/essd-14-573 /-202:;
Earth Syst. Sei. Data, 14. 5737-5770. 2022