Changes between Version 13 and Version 14 of CarbonCycleUnits


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Timestamp:
12/01/17 12:52:01 (6 years ago)
Author:
smoreira
Comment:

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  • CarbonCycleUnits

    v13 v14  
    5555 
    5656Lines 410 to 425 show the calculations of the DIC, OC13 and OC14 dynamics. In line 421, we can observe how ODIC is calculated using variable '''vdic''', which includes PHYTO_dif, ZOO_dif, TPP_dif, ODOC_dif and ODOCS_dif. 
    57 [[BR]] 
     57[[BR]]  
    5858From the previous analysis of Six and Maier-Reimer (1996) and its equivalences in OCYCC, we have concluded that all those variables are expressed in µmol×kg^-1^, or equivalently in µmol×L^-1^. It is precisely in line 421, where ODIC is calculated, where variable vdic (µmol×kg^-1^) is multiplied by the '''SCANU''' factor equal to 1.0e^-06^. This is precisely the conversion factor, 1 µmol = 10^-6^ mol. 
    5959 
    6060=== out_ocycc.f & eco2.f, scale_m factor === 
     61 
     62The output file '''C_reservoirs.txt''' contains some values related to total carbon content in the ocean, atmosphere and vegetation and looking into the values of '''OC_C''' around 39000 coincides with the accepted value of GtC ("gigatons of carbon") of total carbon in the ocean. Calues in this file are written in line 340 of '''out_cycc.f''' and they are calculated in file '''eco2.f'''. 
     63[[BR]] 
     64In lines 96 and 230 of eco2.f, initial total carbon inthe ocean is calculated using the following expression:  
     65[[BR]] 
     66ca_oc = ca_oc + (PHYTO_M(i,J,n) + ZOO_M(i,J,n) + ODOC(i,J,n) + OPOC(i,J,n) + ODOCS(i,J,n) + ODIC(i,J,n)*1e06) * fhypt(j) * DVOL(i,J,n) *12 * SCALE_M * 1.028 
     67[[BR]] 
     68 
     69Here we can see that ODIC values are multiplied by 1.0e06, which confirms that phytoplankton, zooplankton and organic carbon are expressed in µmol×kg^-1^ and ODIC is expressed in mol×kg^-1^ 
     70 
     71Let's have a look more in detail to this equation. The first part of the equation, expressed in µmol×kg^-1^, is turned into µmol×L^-1^ when we multiply by a density value of 1.028 kg/L. Then, it is necessary to multply by 10^3^ to convert the volume of the ocean layer from m^3^ to L. Next step is multiplying by a factor of 10^-6^ to convert µmol into mol before multiplying by the atomic weight of carbon, 12 g/mol to get the total mass in grams. The final step would be multiplying by a factor of 10^-15^ to convert from g to Gt of carbon. 
     72[[BR]] 
     73 
     74This combination of 10^3^x 10^-6^x 10^-15^ turns to be exactly the value of SCALE_M, 1.0e-018. 
     75 
    6176=== out_ocycc.f & eco2.f, scale_b factor === 
    6277