Extended Data Table. 2 Details of GOBM simulations
From: Unexpected decline in the ocean carbon sink under record-high sea surface temperatures in 2023
Model name | CESM-ETHZ | FESOM-REcoM |
---|---|---|
Reference | Doney et al. (2009); Lindsay et al. (2014); Yang and Gruber (2016) (ref. 35) | Gürses et al. (2023) (ref. 34) |
Vertical layers | 60 | 46 |
Native horizontal resolution | lon: 1.125° lat: 0.27° - 0.53° | 1°; refined in equatorial, coastal, and polar regions |
Initial conditions | POP2 model using Levitus data and a state of rest, carbonate chemistry from GLODAPv2 pre-industrial | DIC and TA (GLODAPv2 preindustrial); N, Si, and O2 (WOA13); Fe (PISCES, corrected with observations), temperature and salinity from PHC3.0 climatology |
Spin up procedure | 180 years with CORE forcing and 1850 pCO2, switch to JRA forcing for 14 years; 3x cycling through JRA with historical forcing | Spun up from 1611-1957 with JRA55-do v1.3, repeating the year 1961. |
Length of spin up | 180 years (CORE) + 14 years (JRA) | 1850-1957 |
Physical forcing | JRA-55 v1.3 | JRA55-do v1.3 |
Kw parameters | a = 0.31 (Wanninkhof 1992), 1-fice | a = 0.251 (Wanninkhof 2014), 1-fice |
Atmospheric CO2 | monthly, global mean xCO2 (Friedlingstein et al. 2022) | monthly, global mean xCO2 (Friedlingstein et al. 2022) |