Effect of assimilating CO2 observations in the Korean Peninsula on the inverse modeling to estimate surface CO2 flux over Asia
Fig 4
Annual and average biosphere CO2 fluxes (Pg C yr-1) from the prior (black), CNTL (gray), and EXP1 (white) with their uncertainties aggregated over the (a) Eurasia Boreal, (b) Eurasia Temperate, and (c) Tropical Asia.