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Volltext : An operational oil drift forecasting system for german coastal waters

Die  Kuste,  81  (2014),  255-271

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2.1  Overview
The  numerical  weather  forecast  models  of  the  German  Weather  Service  (DWD),  COS-MO-EU
  (LME)  and  GME,  are  at  die  top  level  of  the  applied  model  chain.  LME  and
GME  provide  the  needed  atmospheric  forcing  for  both  ocean  model  components  on  a
four-times-daily  basis  with  a  forecast  lead  time  of  up  to  7  days.  BSElcmod  is  run  with  a
horizontal  resolution  of  about  5  km  for  the  whole  North  and  Baltic  Sea  area  and  comes
with  a  2-way  nested  grid  increasing  the  resolution  to  about  900  m  in  the  German  Bight
and  western  Baltic  Sea  (DICK  et  al.  2001).  A  further  refinement  of  grid  resolution  up  to
90  m  has  recently  been  achieved  for  die  sub-region  of  die  Elbe  estuary  (MULLER-Navarra
  and  BORK  2012).  Besides  die  atmospheric  forcing,  die  tidal  water  level  at  the
open  boundaries  in  the  North  Sea  and  freshwater  inflow  from  the  largest  rivers  are  driving ­
  forces  of  the  circulation  model.  At  present  BSElcmod  provides  a  three  day  forecast  of
water  level,  current,  temperature,  salinity  and  ice  coverage  once  a  day  in  fully  automatic
fashion.  The  model  output  is  archived  with  a  time  step  of  15  minutes  for  water  level  and
current  and  hourly  for  the  other  variables  together  with  the  atmospheric  forcing.  The
model  data  archive  provides  the  basis  for  all  drift  simulations  and  a  range  of  furdier  applications. ­

To  forecast  die  drift  of  oil,  objects  and  conservative  substances  a  Lagrangian  dispersion ­
  model  is  used.  To  date  an  in-house  developed  Lagrangian  drift  model,  called  BSHdmod.L
  (DICK  and  SOETJE  1990)  is  applied  at  BSH.  BSHdmod.L  uses  the  above  mentioned ­
  archived  BSHcmod  model  fields  and  wind  forecasts  of  LME.  It  was  one  of  die
first  Lagrangian  dispersion  models  operationally  predicting  oil  drift  and  fade  in  Nordi  and
Baltic  Sea  and  has  been  very  successfully  applied  in  die  past  e.g.  during  die  Pallas  wreckage ­
  in  1998  or  die  Baltic  Carrier  collision  in  2001.  Later  on  the  model  code  was  shared
with  neighboring  Nordi  and  Baltic  Sea  countries  like  Denmark  or  Sweden,  where  it  developed ­
  in  parallel.  The  Swedish  Meteorological  and  Hydrological  Institute  (SMHI)  and
the  predecessor  institution  of  die  Forsvarets  Center  for  Operativ  Oceanografi  (FCOO)
used  BSHdmodL  to  upgrade  the  common  HELCOM  modelling  and  drift  forecasting
system  for  oils  and  chemicals  called  SeatrackWeb.  They  continuously  developed  die  drift
model  core  (called  Particle  Advection  and  Dispersion  Model,  PADM),  enhanced  it  with  a
graphical  user  interface  (GLT)  and  made  it  accessible  via  die  internet  (Ambjorn  et  al.
2011 ).
Several  institutes  run  SeatrackWeb  separately  and  in  different  versions.  For  example
SMHI  hosts  die  official  HELCOM  site  (https://stw-helcom.smlii.se/)  and  extra  production ­
  sites  for  special  users  in  Swedish  lakes  and  fjords  (Vanern  and  Brodfjorden)  while
FCOO  hosts  dieir  own  version  for  Danish  users.  BSH  joined  die  SeatrackWeb  developer
group  in  2006  and  adapted  SeatrackWeb  for  BSH  special  requirements  for  example  the
use  of  nested  grids  and  an  extended  model  area.  Recently  SeatrackWeb  runs  in  operational ­
  mode  using  BSHcmod  forcing.  The  BSH  version  of  SeatrackWeb  is  available  under
http://stw.bsh.de/seatrack  .
Mainly  German  authorities,  including  BSH  itself,  are  die  users  of  die  BSH  version  of
SeatrackWeb,  so  die  target  area  of  die  model  is  die  German  Bight  and  die  Western  Baltic
Sea  witii  a  900  m  resolution  of  the  water  current  field  (see  blue  area  in  Fig.l).  Outside  this
area  die  currents  have  a  resolution  of  about  5  km  in  the  North-,  Baltic  Sea  and  in  parts  of
the  English  Channel.
            
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