Seasonal CO2 fluxes in the tropical and subtropical Indian Ocean

Improved estimates of the variability in air-sea CO2 fluxes on seasonal and interannual time scales are necessary to help constrain the net partitioni ng of CO2 between the atmosphere, oceans and terrestrial biosphere. Few dir ect measurements of the carbon system have been made in the main Indian Oce an basin. In the mid 1990s, several global carbon measurement programs focu sed on the Indian Ocean, greatly increasing the existing carbon database fo r this basin. This study examines the combined surface CO2 measurements fro m three major US programs in the Indian Ocean: the global carbon survey cru ises, conducted in conjunction with the World Ocean Circulation Experiment (WOCE), the NOAA Ocean-Atmosphere Carbon Exchange Study (OACES) Indian Ocea n survey and the Joint Global Ocean Flux Study (JGOFS) Arabian Sea Process Study. These data are fit with multiparameter linear regressions as a funct ion of commonly measured hydrographic parameters. These fits are then used with NCEP/NCAR reanalysis and Levitus 94 gridded values to evaluate the sea sonal variability of surface seawater CO2 in the tropical and subtropical I ndian Ocean and to estimate the magnitude of the Indian Ocean as a net sink for atmospheric CO2. The net annual flux for the Indian Ocean (north of 36 degrees S) was - 12.4 +/- 0.5 X 10(12) mol of carbon (equivalent to -0.15 Pg C) in 1995. The rel atively small net flux results from the very different surface water pCO(2) distributions and seasonal variations in the northern and southern Indian Ocean. The equatorial and northern hemisphere regions have values that are generally above atmospheric values. During the S-W monsoon, pCO(2) values i n the Arabian Sea coastal upwelling region are among the highest observed i n the oceans. The upwelling is seasonal in nature, however, and only affect s a relatively small area. The Indian Ocean equatorial region generally has values slightly above atmospheric. Unlike the Pacific and Atlantic Oceans, however, no clear equatorial upwelling signature was observed in 1995. The Southern Hemisphere Indian Ocean, which represents the largest region by a rea, generally has values below atmospheric. The strongest undersaturations are observed in the austral winter, with summer values reaching near or sl ightly above atmospheric. (C) 2000 Elsevier Science B.V. All rights reserve d.