Drivers of Marine CO 2 ‐Carbonate Chemistry in the Northern Antarctic Peninsula

• Published in: Global Biogeochemical Cycles
• Main Authors: Santos‐andrade, Maurício, Kerr, Rodrigo, Orselli, Iole, B M, Monteiro, Thiago, Mata, Mauricio, M, Goyet, Catherine
• Other Authors: UMR 228 Espace-Dev, Espace pour le développement, Institut de Recherche pour le Développement (IRD)-Université de Perpignan Via Domitia (UPVD)-Avignon Université (AU)-Université de La Réunion (UR)-Université de la Nouvelle-Calédonie (UNC)-Université de Guyane (UG)-Université des Antilles (UA)-Université de Montpellier (UM)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2023
• Subjects: CO2; NORTHERN ANTARTIC PENINSULA; [SDE]Environmental Sciences; Antarctic; Antarctic Peninsula; Bellingshausen Sea; Bransfield Strait; Central Basin; Weddell; Weddell Sea; Western Basin; Antarc*; antartic*
• Online Access: https://univ-perp.hal.science/hal-04050313; https://univ-perp.hal.science/hal-04050313/document; https://univ-perp.hal.science/hal-04050313/file/Goyet,%20Santos-Andrade%20et%20al%202023_CO2%20carbonate%20system%20NAP.pdf; https://doi.org/10.1029/2022GB007518

International audience The Bransfield Strait is a climate change hotspot at the tip of the northern Antarctic Peninsula (NAP). The region is marked by a mixture of relatively warm waters from the Bellingshausen Sea with cold shelf waters from the Weddell Sea. Additionally, its deep central basin (>800 m) preserves seawater properties from the north-western Weddell Sea continental shelf. This study assessed long-term changes in carbonate chemistry in the Bransfield Strait and found that the hydrographic setting (i.e., a mixture between modified-Circumpolar Deep Water with Dense Shelf Water [DSW]) drives temporal variability of carbonate parameters. The western basin has experienced decreases in pH (seawater scale) over the last three decades (1996–2019), varying from −0.003 to −0.017 pH units yr −1, while Ωar decreased from −0.01 to −0.07 yr −1 throughout the water column. The central basin was characterized by a high contribution of DSW with high carbon dioxide (CO2) content and the decomposition of organic matter produced and transported into its deep layer. With lower variability for all carbonate system variables, the eastern basin was likely regulated by internal mixing. Overall, the entire strait is almost reaching a CO2-saturated condition, highlighting how sensitive subpolar regions are to the effects of human-induced climate change.