AUTHOR=Yang Wei , Zhao Yu , Wu Yingxu , Chen Zijie , Gao Xiang , Lin Hongmei , Ouyang Zhangxian , Cai Weijun , Chen Liqi , Qi Di TITLE=The impact of sea ice melt on the evolution of surface pCO2 in a polar ocean basin JOURNAL=Frontiers in Marine Science VOLUME=11 YEAR=2024 URL=https://www.frontiersin.org/journals/marine-science/articles/10.3389/fmars.2024.1307295 DOI=10.3389/fmars.2024.1307295 ISSN=2296-7745 ABSTRACT=

The strong CO₂ sink in Arctic Ocean plays a significant role in the global carbon budget. As a high-latitude oceanic ecosystem, the features of sea surface pCO₂ and air-sea CO₂ flux are significantly influenced by sea ice melt; however, our understanding of pCO₂ evolution during sea ice melt remains limited. In this study, we investigate the dynamics of pCO₂ during the progression of sea ice melt in the western Arctic Ocean based on data from two cruises conducted in 2010 and 2012. Our findings reveal substantial spatiotemporal variability in surface pCO₂ on the Chukchi Sea shelf and Canada Basin, with a boundary along the shelf breaks at depths of 250-500 m isobaths. On the Chukchi Sea shelf, strong biological consumption dominates pCO₂ variability. Moreover, in Canada Basin, the pCO₂ dynamics are modulated by various processes. During the active sea ice melt stage before sea ice concentration decreases to 15%, biological production through photosynthetic processes and dilution of ice melt water lead to a reduction in DIC concentration and subsequent decline in pCO₂. Further, these effects are counteracted by the air-sea CO₂ exchange at the sea surface which tends to increase seawater DIC and subsequently elevate surface pCO₂. Compared to the pCO₂ reduction resulting from biological production and dilution effects, the contribution of air-sea CO₂ exchange is significantly lower. The combined effects of these factors have a significant impact on reducing pCO₂ during this stage. Conversely, during the post sea ice melt stage, an increase in pCO₂ resulting from high temperatures and air-sea CO₂ exchange outweighs its decrease caused by biological production. Their combined effects result in a prevailing increase in sea surface pCO₂. We argue that enhanced air-sea CO₂ uptake under high wind speeds also contributes to the high sea surface pCO₂ observed in 2012, during both active sea ice melt stage and post sea ice melt stage. The present study reports, for the first time, the carbonate dynamics and pCO₂ controlling processes during the active sea ice melt stage. These findings have implications for accurate estimation of air-sea CO₂ fluxes and improved modeling simulations within the Arctic Ocean.