13 citations as recorded by crossref.

1. Summer trends and drivers of sea surface fCO<sub>2</sub> and pH changes observed in the southern Indian Ocean over the last two decades (1998–2019) C. Leseurre et al. 10.5194/bg-19-2599-2022
2. Transport of Anthropogenic Carbon From the Antarctic Shelf to Deep Southern Ocean Triggers Acidification S. Zhang et al. 10.1029/2023GB007921
3. Annually Resolved Propagation of CFCs and SF6 in the Global Ocean Over Eight Decades L. Cimoli et al. 10.1029/2022JC019337
4. Circumpolar distributions of age and anthropogenic CO2 content of Antarctic Bottom Water revealed by chlorofluorocarbon and sulfur hexafluoride Y. Ohashi et al. 10.1016/j.pocean.2023.103153
5. Assessment of Annual Physico-Chemical Variability via High-Temporal Resolution Monitoring in an Antarctic Shallow Coastal Site (Terra Nova Bay, Ross Sea) C. Lombardi et al. 10.3390/min11040374
6. Tides regulate the flow and density of Antarctic Bottom Water from the western Ross Sea M. Bowen et al. 10.1038/s41598-023-31008-w
7. Severe 21st-century ocean acidification in Antarctic Marine Protected Areas C. Nissen et al. 10.1038/s41467-023-44438-x
8. Observing Antarctic Bottom Water in the Southern Ocean A. Silvano et al. 10.3389/fmars.2023.1221701
9. Plio-Pleistocene deep-sea ventilation in the eastern Pacific and potential linkages with Northern Hemisphere glaciation L. Yi et al. 10.1126/sciadv.add1467
10. East–west contrasting changes in Southern Indian Ocean Antarctic Bottom Water salinity over three decades Y. Choi & S. Nam 10.1038/s41598-022-16331-y
11. Physical and biological controls on anthropogenic CO2 sink of the Ross Sea G. Ingrosso et al. 10.3389/fmars.2022.954059
12. Future changes in Antarctic coastal polynyas and bottom water formation simulated by a high-resolution coupled model H. Jeong et al. 10.1038/s43247-023-01156-y
13. Spatial and temporal variability of the physical, carbonate and CO2 properties in the Southern Ocean surface waters during austral summer (2005-2019) M. Brandon et al. 10.1016/j.dsr.2022.103836