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P. Poli et al.: SVP-BRST: genesis, design, and initial results
Ocean Sci., 15,199-214, 2019
www.ocean-sci.net/15/199/2019/
SST difference (K), Hull minus CT probe
-0.5 -0.1 0.0 0.1 0.5
(a)
Il
a&jfriF -Y:
(c)
: b.
:< i Vi
I ce
1 LU
^ ■ p " ‘ ■ * ■ ]
F. 1
I
Number of points
per 0.01 K difference and
per 1 ° angle
| 1 2 4 7 13 24 45 84 157 294
-0.5 -0.1 0.0 0.1 0.5
SST difference (K), Hull minus CT probe
Number of points
per 0.01 K difference and
per 0.25 ms -1 wind speed
129 257 514
-0.5 -0.1 0.0 0.1
SST difference (K), Hull minus CT probe
Figure 2. Differences between the two SST sensors from all HRSST-
estimates for (b) 10 m wind speed and (c) significant wave height.
reassess sensor accuracy and drift several years after initial
calibration. The buoys were recovered without visible outer
damage. It is not impossible that the sensors may have aged
differently during the various phases of the buoy life cycle:
(a) after calibration and until deployment, (b) at sea, and (c)
after recovery. Unfortunately, it proved impossible to have
the probes calibrated by the same laboratory (Bernie Petó
las, personal communication, 2016). Table 3 shows the re
sults of the calibration verification done by the initial lab
oratory (Measurement Specialties, lab. no. 1 in the table),
and the calibration verifications done by two other laborato-
■2 SVP-BS buoys, as a function of (a) solar elevation angle and ERA5
ries (at different dates), after the buoys were recovered from
shore. Despite the same Metocean interface being used at
all three laboratories, the calibration procedure, being inher
ently laboratory dependent, brings in additional uncertain
ties. For example, the various laboratories involved here did
not use the same verification points. The initial laboratory
used three calibration points (0, 25, 40 °C), i.e., the bare
minimum to compute the three Steinhart-Hart coefficients
per sensor. The same temperatures were then used to as
sess the (residual) calibration error. In the table, lab. no. 2
refers to the Service Hydrographique et Océanographique de