Abstract

In April 2006, diurnal variations of carbon dioxide (CO 2) and oxygen (O 2) in the surface water east of Gotland in the Baltic Sea were investigated with a unique multitechnology approach. Several parameters were measured simultaneously providing an overview of the CO 2 system. Moored instruments were continuously recording partial pressure of CO 2 in the surface water ( pCO 2 w), currents, mixing, waves, salinity, temperature and O 2. Measurements of total alkalinity ( A T) and dissolved inorganic carbon ( C T) were taken from R/V Skagerak. These measurements were converted to pCO 2 w to support the continuous pCO 2 w data and also calculate the air–sea exchange of CO 2. Additionally, the time derivatives of O 2 and C T concentrations in the water were determined using incubations and a Productivity Autosampler (PA). O 2 and pCO 2 w were significantly anti-correlated and periods dominated of either biological processes, mixing, air–sea exchange or a combination of these were detected. O 2 and pCO 2 w had a daily cycle and variations occurred on the 1 h time scale. In April 2006, the sea was a CO 2 sink and the averaged parameterized air–sea exchange was − 1.0 ± 0.6 mmol m −2 h −1.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call