| 61 | |
| 62 | The 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]] |
| 64 | In lines 96 and 230 of eco2.f, initial total carbon inthe ocean is calculated using the following expression: |
| 65 | [[BR]] |
| 66 | ca_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 | |
| 69 | Here 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 | |
| 71 | Let'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 | |
| 74 | This combination of 10^3^x 10^-6^x 10^-15^ turns to be exactly the value of SCALE_M, 1.0e-018. |
| 75 | |