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Is it possible to extract information related to sea-state from an Argo float ?

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HAL Id: hal-02169635

https://hal.sorbonne-universite.fr/hal-02169635

Submitted on 8 Jul 2020

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Is it possible to extract information related to sea-state

from an Argo float ?

Antoine Poteau, Hervé Claustre, F. d’Ortenzio, L Prieur

To cite this version:

Antoine Poteau, Hervé Claustre, F. d’Ortenzio, L Prieur. Is it possible to extract information related

to sea-state from an Argo float ?. 5th Euro-Argo User Workshop, Mar 2015, Brest, France.

�hal-02169635�

(2)

Is  it  possible  to  extract  informa2on  related  to  sea-­‐state  from  an  Argo  float?  

Thanks  to  the  new  genera.on  of  profiling  floats  and  in  par.cular  to  iridium  telemetry,  the  acquisi.on  frequency  can  be  drama.cally  increased.  We  inves.gate  here  the  possibility  to   extract   informa.on   related   to   sea-­‐state   from   the   analysis   of   high-­‐resolu.on   measurements   of   the   pressure   data.   We   par.cularly   focus   on   the   study   of   the   speed   anomaly     as   compared  to  a  nominal  speed  expected  for  a  calm  sea-­‐state.  By  comparison  between  speed  anomaly  of  a  float  in  the  Med  Sea  and  concurrent  seastate  measurements  by  a  weather   buoy  in  the  same  area,  we  suggest  that  float  behaviour  can  be  an  indicator  of  sea-­‐state.  In  the  context  of  remOcean  and  NOAS  projects,  we  set  up  a  high  frequency  mode  (every  2  s)   for  the  sub-­‐surface  layer  and  for  more  than  fourty  floats  deployed  in  various  open  ocean  areas,  we  present  a  preliminary  analysis  of  the  speed  anomaly.  

Poteau

1,2

 A.,  Claustre

1,2

 H.,  D'Ortenzio

1,2

 F.,  Prieur  L.

1,2

 

1  -­‐  Sorbonne  Universités,  UPMC  Univ  Paris  06,  UMR  7093,  LOV,  Observatoire  océanologique,  F-­‐06230,  Villefranche/mer,  France     2  -­‐  CNRS,  UMR  7093,  LOV,  Observatoire  océanologique,  F-­‐06230,  Villefranche/mer,  France    

observa.on  of  float  behavior  :  

Characteris.cs  of  the  NKE  CTS4  float  in  the  upper  layer:     -­‐  when  the  float  passes  10  dbars,  it  does  not  ac.vate  its   pump  for  a  dura.on  of  600  sec    

-­‐  ader  600  sec,  the  float  starts  to  pump  360  sec  to  emerge   -­‐  under  standard  (calm)  weather  condi.ons,  it  takes  90-­‐100   sec  for  the  float  to  rise  the  surface  from  10m.  

-­‐  data  acquisi.on  from  1m  to  0  m:  mean  value  

-­‐  data  acquisi.on  from  10  to  1m  :  raw  data  @  2  sec  (0.5Hz)   -­‐  data  acquisi.on  from  350  to  10m  :  raw  data  @  10  sec   (0.1Hz)  

CTS4,  NKE  

600  s   4.5  m   80  s   0  m   Standard  behavior      

sta.s.c  &  climagraphs  

Non  Standard  behavior  

MOORED  AUTOMATIC   WEATHER  STATIONS  

valida.on  with  weather  mooring  

Time-serie of behavior indicators of two floats compared to meteorological buoy data in the North-Western Mediterranean Sea. Even if the distance of the floats to the mooring are greater than 100 km, the comparison of both time series confirms that float behavior indicators can be used with a certain confidence to track sea-state. These indicators can thus be extracted from all the CTS4 floats we manage to date.

We now envisage to extract similar float behavior indicators from standard Argo profiles and in particular the information related to big event..

big  events  >  10m  re-­‐dive  0.4%  

what  next    

Characteris.cs  of  the  NKE  CTS4   float  in  Indicators  of  float   behavior  in  the  upper  layer   In  this  poster  we  explore  the   idea  that  the  float  behavior  is   related  to  the  sea  state.    

Time  spend    between    10m  and  1m   (s)  proxy  of  speed  anomaly  

Maximum  re−dive     between  10m  and  1m  [m],  

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