Distribution of net community production and surface pCO2 in the Scotia Sea, Antarctica, during austral spring 2001'

Abstract Surface and water column measurements of p CO 2 , alkalinity, and nutrients were made in the Scotia Sea in December 2001. From 54°S to 60°S along 52°W, p CO 2 , TCO 2 , and nutrients in surface seawater increased southward. The p CO 2 concentration ranged from 370 μatm in the north to 420 μatm in the south and increased abruptly across the Polar and Scotia fronts by about 10–20 μatm. Net community production values from the preceding winter to the observation time were calculated at stations south of the Polar Front; values ranged from 1.0 to 1.2 mol m − 2 and were comparable to other Southern Ocean measurements in summer, in or during an algal bloom. Processes affecting the surface p CO 2 distribution (e.g., thermodynamical change, air–sea exchange, biological production, and physical mixing) were evaluated from the preceding winter to the observation time at the stations. Seasonal warming increased surface p CO 2 at rates of 0.08–0.27 μatm day − 1 ; the highest values were observed at the station closest to the Polar Front. The air–sea exchange decreased surface p CO 2 at rates of − 0.08 to − 0.23 μatm day − 1 , suggesting that the area around the study stations acted as a weak CO 2 source during the study period. The surface p CO 2 variation caused by biological production was − 0.24 to − 0.30 μatm day − 1 and was high south of the Scotia Front, where concentrations of chlorophyll a , biomass, and particulate Fe were relatively high. Physical mixing promoted an increase of 0.16–0.47 μatm day − 1 in surface p CO 2 , a substantial contribution to total variation in p CO 2 . This result contrasts with patterns in other Southern Ocean regions, where physical mixing was considered to be minimal or was ignored in previous studies. At station WS 8 in the Weddell–Scotia Confluence region, mixing was the dominant process of surface p CO 2 change during the study period, suggesting lateral and vertical transport of CO 2 -rich water masses from the Weddell Sea and the deep ocean.