A mechanistic semi‐analytical method for remotely sensing sea surface<i>p</i><scp>CO</scp>₂in river‐dominated coastal oceans: A case study from the<scp>E</scp>ast<scp>C</scp>hina<scp>S</scp>ea

Abstract

Abstract While satellite remote sensing has become a very useful tool contributing to assessments of sea surface partial pressure of carbon dioxide ( p CO 2 ) that subsequently allow quantification of air‐sea CO 2 flux, the application of empirical approaches in coastal oceans has proven challenging owing to the interaction of multiple controlling factors. We propose a “mechanistic semi‐analytic algorithm” (MeSAA) to estimate sea surface p CO 2 in river‐dominated coastal oceans using satellite data. Observed p CO 2 can be analytically expressed as the sum of individual components controlled by major factors such as thermodynamics (or temperature), mixing, and biology. With marine carbonate system calculations, temperature and mixing effects can be predicted using thermodynamic principles and by assuming conservative two end‐member mixing of total dissolved inorganic carbon and total alkalinity (e.g., the Changjiang River and Kuroshio water in the East China Sea, ECS). Next, an integral expression for p CO 2 drawdown due to biological effects can be parameterized using the chlorophyll a concentration ( chla ). We demonstrate the validity and applicability of the algorithm in the ECS during summertime. Sensitivity analysis shows that errors in empirical coefficients and three input satellite parameters (salinity, SST, chla) have limited influence on the algorithm, and satellite‐derived p CO 2 is consistent with underway data, even though no in situ p CO 2 data from the ECS shelves was used to train the algorithm. Our algorithm has more physical and biogeochemical mechanistic meaning than empirical methods, and should be applicable to other similar systems.