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To quantitatively assess the inorganic carbon cycle in the eastern Indian sector of the Southern Ocean (80–150°E, south of 60°S), we measured ocean surface temperature, salinity, total alkalinity (TA), the partial pressure of carbon dioxide (pCO2), and concentrations of chlorophyll‐a(chl a), dissolved inorganic carbon (DIC), and nutrients during the KY18 survey (December 2018–January 2019). The sea–air CO2flux in this region was −8.3 ± 12.7 mmol m−2day−1(−92.1 to +10.6 mmol m−2day−1). The ocean was therefore a weak CO2sink. Based on the DIC and TA in the temperature minimum layer, we estimated the change of pCO2from winter to summer (δpCO2) due to changes in water temperature, salinity, and biological activity (photosynthesis). The spatial distribution of pCO2in the western part (80–110°E) of the study area was mainly driven by biological activity, which decreased pCO2from December to early January, and in the eastern part (110–150°E) by temperature, which increased pCO2from January to February. We also examined the changes in the CO2concentrations (xCO2) over time by comparing data from 1996 with our data (2018–2019). The oceanic and atmospheric xCO2increased by 23 and 45 ppm in 23 years, respectively. These changes of ocean xCO2were mainly driven by an increase in CO2uptake from the atmosphere as a result of the rise in atmospheric xCO2and increase in biological activity associated with the change in the water‐mass distribution. Determining the drivers of seasonal changes in ocean CO2is important for estimating the global carbon cycle. Seawater samples were collected in the eastern Indian sector of the Southern Ocean to investigate the carbonate chemistry of the ocean surface water. During winter and summer, the partial pressure of carbon dioxide (pCO2) at the ocean surface decreased and increased due to photosynthesis and temperature changes, respectively. Surface water pCO2was lower than the pCO2of the atmosphere in summer: the result was CO2uptake by the ocean. A comparison of data from 1996 with our data (2018–2019) indicated that the CO2concentration (xCO2) of the seawater had increased by 23 ppm. This increase was due primarily to an increase in uptake of CO2from the atmosphere as a result of the rise of atmospheric xCO2. The eastern Indian sector of the Southern Ocean absorbs atmospheric CO2weakly in summerBiological activity and increases in water temperature change the pCO2from winter to summerChanges in atmospheric pCO2and water masses explained the interannual variations of dissolved CO2in the ocean The eastern Indian sector of the Southern Ocean absorbs atmospheric CO2weakly in summer Biological activity and increases in water temperature change the pCO2from winter to summer Changes in atmospheric pCO2and water masses explained the interannual variations of dissolved CO2in the ocean

To clarify the effect of basal melting of ice tongues/ice shelf on the CO2system in the Antarctic continental margin, seawater samples were collected for analysis of dissolved inorganic carbon (DIC), total alkalinity (TA), nutrients, chlorophyll a (chl.a), and oxygen isotopic ratios at the ice front of the Shirase Glacier Tongue (SGT) in Lützow‐Holm Bay (LHB), East Antarctica during the summers of 2017 and 2018. At depths greater than ∼20 dbar in LHB, CO2system parameters were strongly influenced by the dilution effect of SGT basal melting and the inflow of modified Circumpolar Deep Water (mCDW). The distributions of DIC and TA agreed well with an offshore origin of mCDW that flowed beneath the SGT and mixing of basal meltwater and mCDW beneath the SGT. The fraction of SGT meltwater was highest at the station near the ice front. Dilution by SGT basal meltwater reduced the partial pressure of CO2in the mCDW from 431 to 387 μatm. The water then became a sink rather than source of atmospheric CO2. In the sea surface, DIC and TA were strongly influenced by biological processes. Salinity‐normalized DIC decreased with the increase of salinity‐normalized TA in accord with 106:16 C:N molar stoichiometry; the chl.a concentration at the sea surface was as high as 31 μg L−1. Oceanographic observations were made during the summers of 2017 and 2018 near the ice shelf in an ice‐covered bay in East Antarctica. Results revealed that the parameters such as dissolved inorganic carbon (DIC), total alkalinity (TA), and nutrients at subsurface layer (>20 m) was strongly influenced by the dilution effect of the melting of ice sheet and the inflow of warm and high salinity water from outside of the bay. In contrast, within the surface layer, DIC, TA, and nutrients were strongly influenced by phytoplankton activity. The CO2system is strongly influenced by the dilution effect of the basal melting of the Shirase Glacier Tongue (SGT)The decrease of pCO2by basal melting caused the water to shift from a CO2source to a sink of atmospheric CO2in Lützow‐Holm BaySurface water was strongly influenced by biological processes near the SGT The CO2system is strongly influenced by the dilution effect of the basal melting of the Shirase Glacier Tongue (SGT) The decrease of pCO2by basal melting caused the water to shift from a CO2source to a sink of atmospheric CO2in Lützow‐Holm Bay Surface water was strongly influenced by biological processes near the SGT