Rainwater dissolved organic carbon: Concentrations and global flux

Dissolved organic carbon (DOC) is a major component of both marine (23 mu M ) and continental (161 mu M) rain, present in concentrations greater than n itric and sulfuric acids combined. Rain is a significant source of DOC to s urface seawater (90 x 10(12) g C yr(-1)), equivalent to the magnitude of ri ver input of DOC to the open ocean and half the magnitude of carbon buried in marine sediments per year on a global scale. Current models of global ca rbon cycling focus primarily on inorganic forms of carbon and are unable to account for approximately 20% of the global carbon dioxide, suggesting a s ignificant missing carbon sink. Quantification of the average DOC concentra tion in marine rain allows calculation of the global rainwater flux of DOC of 430 +/- 150 x 10(12) g C yr(-1). When inorganic carbon is included, this rainwater carbon flux becomes 510 +/- 170 x 10(12) g C yr(-1), which, alth ough not the same carbon, is equivalent in magnitude to over one third of t he missing carbon sink.