• Keine Ergebnisse gefunden

Auxiliary  material  for    Global  sea-­‐surface  nitrate  fields  estimated  from  remotely  sensed  sea-­‐surface  temperature,  chlorophyll  and  modeled  mixed  layer  depth    Lionel  Arteaga

N/A
N/A
Protected

Academic year: 2022

Aktie "Auxiliary  material  for    Global  sea-­‐surface  nitrate  fields  estimated  from  remotely  sensed  sea-­‐surface  temperature,  chlorophyll  and  modeled  mixed  layer  depth    Lionel  Arteaga"

Copied!
1
0
0

Wird geladen.... (Jetzt Volltext ansehen)

Volltext

(1)

Auxiliary  material  for    

Global  sea-­‐surface  nitrate  fields  estimated  from  remotely  sensed  sea-­‐surface   temperature,  chlorophyll  and  modeled  mixed  layer  depth  

 

Lionel  Arteaga1,  Markus  Pahlow1,  Andreas  Oschlies  1  

 

1GEOMAR  Helmhlotz  Centre  for  Ocean  Research  Kiel,  Kiel,  Germany    

Geophysical  Research  Letters  [2014GL062363]  

  Introduction  

 

This  auxiliary  material  contains  one  supplementary  Figure  and  one  

supplementary  data  set.  Figure  fs01  shows  the  results  of  the  error  analysis   described  in  section  3.3  Error  analysis.  The  data  set  is  a  netCDF  file,  “ds01.nc”,   that  contains  local  coefficients  obtained  from  the  linear  regression,  βsst,  βMLD,  βChl,  

C,  for  each  oceanic  pixel  on  a  1°  x  1°  resolution  grid.  These  coefficients  can  be   combined  with  data  from  SST,  surface  Chl,  and  MLD  to  estimate  surface  nitrate   concentrations  in  the  global  ocean  following  Equation  2.  

  Data  

1.  ds01.nc:  netCDF  file  of  6  variables  (var)  and  2  dimensions  (dim)  with  local   coefficients  for  global  nitrate  estimation.  

 

1.1  var1  (dim1):  Longitude  (size[360  1])   1.2  var2:  (dim2)  Latitude  (size[180  1])  

1.3  var3:  Constant  coefficient  C  (size[360  180])   1.4  var4:  SST  coefficient  (size[360  180])  

1.5  var5:  MLD  coefficient  (size[360  180])   1.6  var6:  Chl  coefficient  (size[360  180])    

Figures  

fs01.pdf  -­‐  Monthly  predicted  original  (green  continuous  line)  and  predictions   obtained  with  high  (a  =  1,  red  continuous  line  “noisy”),  medium  (a  =  0.25,  cyan   continuous  line  noisy025),  and  low  (a  =  0.01,  black  continuous  line  “noisy01”)   noise  levels  added  to  the  predictor  datasets  of  nitrate  concentrations  for  HOT   (a),  BATS  (b),  and  Munida  (c)  from  January  2005  to  December  2010.  In-­‐situ  data:  

blue  dashed  line.  (d)  Global  distribution  of  relative  differences  between  original   predicted  nitrate  (Figure  1a)  and  nitrate  predicted  with  the  maximum  estimated   random  error  induced  in  the  predictive  data  set  (a=0.01).  

   

Referenzen

ÄHNLICHE DOKUMENTE

For the purpose of this work 178 tide gauges are selected in the latitudinal band 65 o S-65 o N from the PSMSL database (RLR, monthly) that have at least 30 annual mean values

Temperature and salinity variations of Mediterranean Sea surface waters over the last 16,000 years from records of planktonic stable oxygen isotopes and alkenone unsaturation

Comparison of Mg/Ca- and alkenone based sea surface temperature estimates in the fresh water-influenced Gulf of Guinea, eastern equatorial Atlantic.

Figure 4. a) Distribution of sail heights fitted with a negative exponential function. No sails lower than the cut-off height of 0.8 m are detected. b) Histograms of sail spacing

The effects of single and multiple reflections on the microwave reflectivity of sea surface are shown in Figure 7, in which calculations were made at 19.35 GHz for a

Calibration of the alkenone palaeotemperature index UK´37 base d on core-tops from the eastern South Atlantic and the global ocean (60°N-60°S).. The correlation between the

Considering this observation quality levels of diatom estimates obtained from locations where both diatom and radiolarian estimates are available have been downgraded to ensure

The actual width of the surface peak appeared somewhat broader (Fig. 3), either due to larger beam aperture or acoustical surface conditions such as waves and