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Interannual and decadal changes in the sea‐air CO 2 flux from atmospheric CO 2 inverse modeling
Author(s) -
Patra Prabir K.,
Maksyutov Shamil,
Ishizawa Misa,
Nakazawa Takakiyo,
Takahashi Taro,
Ukita Jinro
Publication year - 2005
Publication title -
global biogeochemical cycles
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.512
H-Index - 187
eISSN - 1944-9224
pISSN - 0886-6236
DOI - 10.1029/2004gb002257
Subject(s) - environmental science , flux (metallurgy) , climatology , upwelling , pacific decadal oscillation , atmospheric model , atmosphere (unit) , atmospheric sciences , sea surface temperature , oceanography , geology , meteorology , chemistry , geography , organic chemistry
The atmosphere‐land‐ocean fluxes of CO 2 were derived for 64 partitioned areas of the globe (22 over the ocean and 42 over the land) using a time‐dependent inverse (TDI) model for the period of January 1988 to December 2001. The model calculation partially follow the TransCom‐3 protocol, and is constrained by atmospheric CO 2 concentration data from 87 stations and fully time‐dependent atmospheric transport model simulations. The air‐to‐land and air‐to‐sea fluxes averaged over the 1990s are estimated at 1.15 ± 0.74 and 1.88 ± 0.53 Pg‐C yr −1 , respectively. These estimates, however, remain uncertain owing to sampling biases arising from the sparse distribution of atmospheric CO 2 data, are compared with other estimates by various methods. The sensitivity analysis indicates that the differences in fluxes and flux variability caused by the choices of initial conditions for the TDI model are smaller compared to those due to the selection of measurement networks. Our model results capture interannual variations in global and regional CO 2 fluxes realistically. The estimated oceanic CO 2 flux anomalies appear to be closely related to prominent climate modes such as El Niño–Southern Oscillation (ENSO), the North Atlantic Oscillation (NAO), and the Pacific Decadal Oscillation (PDO). The results from the correlation analyses show that the oceanic CO 2 flux in the tropics is strongly influenced by the ENSO dynamical cycle, and that in the sub‐polar regions by upwelling of sub‐surface waters in the winter and plankton blooms in the spring.