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Volltext : The Copernicus Surface Velocity Platform drifter with Barometer and Reference Sensor for Temperature (SVP-BRST)

P.  Poli  et  al.:  SVP-BRST:  genesis,  design,  and  initial  results

207

www.ocean-sci.net/15/199/2019/

Ocean  Sci.,  15,199-214,  2019

0.00  0.05  0.10  0.15  0.20  0.00  0.05  0.10  0.15  0.20
SST  uncertainty  (K)  SST  uncertainty  (K)
(SLSTR  3-channel  nighttime)  (SLSTR  3-channel  nighttime)

Figure  5.  SLSTR  SST  uncertainty  validation  plot  for  (a)  all  drifters
and  (b)  a  subset  of  HRSST-1  and  HRSST-2  drifters,  with  uncertainty ­
  bins  of  0.001  K.  An  uncertainty  of  0.05  K  is  assumed  for  the
drifter  SST.

Also,  when  in  that  situation,  the  float  is  more  likely  to  reach
wave  crests.  There,  the  sky  visibility  is  improved,  reducing
the  GPS  time  to  first  fix  (TTFF),  which  can  serve  as  an  additional ­
  indicator  of  drogue  loss  (Petolas,  2013).
To  investigate  the  influence  of  the  drogue,  the  SVP-BS
data  record  is  revisited.  These  buoys  used  submergence  sensors, ­
  whereas  drifters  nowadays  use  strain  gauges,  e.g.,  as
indicated  by  Rio  (2012),  who  developed  a  advanced  method
to  identify  drogue  loss  using  drifter  currents,  satellite  altimetry, ­
  and  wind  reanalysis  data.  The  submergence  (or  tether
strain  gauge)  readings  are  neither  straightforward  to  interpret ­
  nor  fully  reliable  on  their  own  (Rio,  2012).  Flowever,
the  SVP-BS  drifter  data  considered  here  (available  from  the
Coriolis  In  Situ  Thematic  Assembly  Center)  are  not  found
in  the  drifter  dataset  of  Rio  and  Etienne  (2018),  which  includes ­
  drogue  presence  flags.  Consequently,  for  this  analysis, ­
  we  use  the  submergence  and  GPS  TTFF  data.  A  visual
inspection  indicates  that  10  of  the  20  buoys  in  Table  2  have
lost  their  drogues  during  their  mission.  For  these  buoys,  two
series  of  data  records  are  extracted:  (1)  before  drogue  loss
and  (2)  after  drogue  loss.
During  daytime,  the  median  of  the  differences  between
the  twin  SST  measurements  is  —0.04K  in  (1),  whereas  it  is
—0.03  K  in  (2).  The  reduction  in  differences  may  appear  insignificant, ­
  but  it  is  consistent  with  the  CT  sensor  being  more
often  exposed  to  depths  similar  to  the  sensor  integral  to  the
hull  when  the  drogue  is  lost  than  when  the  drogue  is  present.
Similarly,  the  robust  standard  deviation  of  the  differences  between ­
  the  twin  SST  measurements  is  0.03  K  in  (1),  whereas
it  is  0.01  K  in  (2).  Again,  this  reduction  is  consistent  with
drogue  loss  for  the  same  reasons.
During  nighttime,  no  influence  of  the  drogue  loss  is  expected ­
  if  the  temperatures  are  homogeneous  just  below  the
surface.  This  is  indeed  what  is  observed.  The  median  of  the
differences  is  —0.04K  in  both  (1)  and  (2),  and  the  robust
standard  deviation  of  the  differences  is  0.03  K  in  both  (1)
and  (2).
In  other  terms,  the  SVP-BS  data  record  confirms  the  expectation ­
  that  once  the  drogue  is  lost,  the  SST  probes  on  a
drifter  are  more  likely  to  be  exposed  to  water  immediately

below  the  surface  than  when  the  drogue  is  present,  and  this
effect  is  more  visible  in  the  presence  of  stratification  (e.g.,
during  daytime).  To  keep  track  of  the  drogue  effect  on  SST
measurements,  it  is  important  to  monitor  drogue  loss  as  well
the  immersion  depth  and  its  variations.
2.6  Limited  traceability
Adopting  a  more  general  point  of  view  for  SST  observations,
several  works  have  already  attempted  to  document  the  uncertainties ­
  in  the  various  in  situ  SST  measurement  methods.
The  present  paper  does  not  attempt  to  review  all  these  efforts
but  cites  relevant  results  from  the  comprehensive  review  of
Kennedy  (2014).  While  the  focus  of  this  earlier  work  was  on
the  creation  on  long  time  series,  with  the  largest  issues  identified ­
  at  the  time  of  World  War  II  (transition  on  ships  from
bucket  to  engine-room  intake),  the  quality  of  SST  buoys  was
found  to  be  the  subject  of  several  concerns.  The  first  concern ­
  is  the  spread  in  quality  between  buoys,  depending  on
the  source  of  the  uncertainty  estimate,  with  no  reliable  link
to  the  actual  metrological  reference.  The  second  concern  is  a
suggested  improvement  in  quality  over  time,  though  without
quantified  evidence  or  clear  a  priori  reason  for  it  that  would
be  explained  by  metrological  documentation.  Both  points
stem  from  an  insufficient  knowledge  of  the  sensor  technology, ­
  and  of  the  calibration  procedure  that  was  actually  used,
for  each  drifting  buoy  deployed.  The  results  shown  earlier,
showing  differences  in  SST  quality  between  general  drifters
versus  HRSST  drifters,  reinforce  the  importance  of  enhancing ­
  the  knowledge  of  drifter  metrology  and  metadata.

3  Design  of  the  SVP-BRST
The  HRSST-2  efforts  were  initiated  by  the  cal/val  needs  of
AATSR  SST  retrievals.  With  the  demise  of  this  instrument
after  10  years  of  service  in  2012  (ESA  Communications  Department, ­
  2012),  the  HRSST-2  developments  were  put  to  a
halt,  until  the  replacement  sensor  (SLSTR  on  Sentinel-3)  was
launched.  However,  this  gap  gave  time  to  finish  all  HRSST-2
deployments  and  review  the  lessons  learnt  from  them.  Coupled ­
  with  the  need  to  assert  long  consistent  time  series  of  SST
at  an  accuracy  level  compatible  with  SLSTR  requirements,
sound  bases  were  used  to  imagine  a  novel  sensor  package
for  reference  SST.  The  result  is  the  SVP-BRST,  based  on  the
SVP-B  design  (Sybrandy  et  ah,  2009),  with  a  strain  gauge
to  detect  drogue  loss.  In  addition,  the  HRSST-2  requirements
presented  earlier  are  included,  as  well  as  others,  described
hereafter.
The  first  additional  requirement  is  to  employ  an  additional ­
  HRSST  sensor,  in  addition  to  the  regular  SST  sensor.
The  HRSST  sensor  collects  data  within  the  5  min  before  the
round  hour,  when  the  position  is  updated  by  means  of  GNSS.
The  mean  SST  is  to  be  computed  from  1  Hz  SST  measurements. ­
  In  addition,  the  data  can  be  relayed  at  1  Hz  frequency
            
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