XCTD (eXpendable Conductivity Temperature Depth) probes, developed rec
ently by SIPPICAN Inc., have been used simultaneously with a CTD sonde
in order to test, in the field, their performance and accuracy (inter
preted as +/-2 standard deviations pf the XCTD-CTD differences). We ha
ve taken advantage, during the THETIS-I experiment in March 1992, of b
oth the homogeneous and the stratified areas encountered in winter in
the northern part of the western Mediterranean Sea to differentiate th
e errors due to the experimental conditions from those effectively due
to the sensors. Although some intrinsic problems are evident, so that
only seven out of the nine probes considered for comparison are usabl
e, the accuracy specified by the manufacturer for the temperature (AT=
+/-0.03 degrees C) is reached after standard processing, while the acc
uracies in conductivity, salinity and potential density are AC similar
to+/-0.06 mS/cm (the specified value is AC=+/-0.03 mS/cm), AS similar
to+/-0.04 and A sigma(theta)+/-0.03 kg/m(3). However, when the experi
mental errors (in situ natural variability, relatively rough estimatio
n of the XCTD depth) are considered, it appears that the effective acc
uracies of the XCTD sensors are better than +/-0.02 degrees C and +/-0
.04 mS/cm, that is to say better than and close to the specified value
s of +/-0.03 degrees C and +/-0.03 mS/cm. Occasional offsets in conduc
tivity can further be well corrected for by using a temperature-salini
ty relation in some limited depth range and area where this relation i
s known to hold well; the conductivity-sensor accuracy then significan
tly improves to AC similar to 0.02 mS/cm resulting, for our study area
, in corresponding salinity and potential density accuracies of AS sim
ilar to+/-0.03 and A sigma(theta)similar to+/-0.02 kg/m(3). Thus, such
instruments promise to be useful tools for many experimental studies.
Complementary comparisons, performed with new versions of the XCTD pr
obes under less convenient experimental conditions, are also presented
. Copyright (C) 1996 Elsevier Science Ltd.