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1. How old is too old? Implications of averaging 14C-Based estimates of ventilation age to assess the Pacific Ocean's role in sequestering CO2 in the past

   https://doi.org/10.1016/j.quascirev.2023.108122  

   Stott, Lowell D. ( June 2023 , Quaternary Science Reviews)
2. Advances in research and applications of CO2-based demand-controlled ventilation in commercial buildings: A critical review of control strategies and performance evaluation

   https://doi.org/10.1016/j.buildenv.2022.109455  

   Lu, Xing ; Pang, Zhihong ; Fu, Yangyang ; O'Neill, Zheng ( September 2022 , Building and Environment)
3. Evaluating the Glacial-Deglacial Carbon Respiration and Ventilation Change Hypothesis as a Mechanism for Changing Atmospheric CO2

   Stott, Lowell Shao ( January 2021 , Geophysical research letters)

   null (Ed.)

   The prevailing hypothesis to explain pCO2 rise at the last glacial termination calls upon enhanced ventilation of excess respired carbon that accumulated in the deep sea during the glacial. Recent studies argue lower [O2] in the glacial ocean is indicative of increased carbon respiration. The magnitude of [O2] depletion was 100–140 μ mol/kg at the glacial maximum. Because respiration is coupled to δ13C of dissolved inorganic carbon (DIC), [O2] depletion of 100–140 μ mol/kg from carbon respiration would lower deep water δ13CDIC by ∼1‰ relative to surface water. Prolonged sequestration of respired carbon would also lower the amount of 14C in the deep sea. We show that Pacific Deep Water δ13CDIC did not decrease relative to the surface ocean and Δ14C was only ∼50‰ lower during the late glacial. Model simulations of the hypothesized ventilation change during deglaciation lead to large increases in δ13CDIC, Δ14C, and ε14C that are not recorded in observations. 

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4. Ocean ventilation controls the contrasting anthropogenic CO2 uptake rates between the western and eastern South Atlantic Ocean basins

   Gao, H. ; W.-J. Cai ; M. Jin ; C. Dong ; A. H. V Timmerman ( June 2022 , Global biogeochemical cycles)

   The South Atlantic Ocean is an important region for anthropogenic CO2 (Canth) uptake and storage in the world ocean, yet is less studied. Here, after an extensive sensitivity test and method comparison, we applied an extended multiple linear regression (eMLR) method with six characteristic water masses to estimate Canth change or increase (ΔCanth) between 1980s and 2010s in the South Atlantic Ocean using two meridional transects (A16S and A13.5) and one zonal transect (A10). Over a period of about 25 years, the basin-wide ΔCanth was 3.86±0.14 Pg C decade-1. The two basins flanking the Mid-Atlantic Ridge had different meridional patterns of ΔCanth, yielding an average depth‐integrated ΔCanth in the top 2000 m of 0.91±0.25 mol m-2 yr-1 along A16S on the west and 0.57±0.22 mol m-2 yr-1 along A13.5 on the east. The west-east basin ΔCanth contrasts were most prominent in the tropical region (0-20°S) in the Surface Water (SW), approximately from equator to 35°S in the Subantarctic Mode Water (SAMW), and all latitudes in the Antarctic Intermediate Water (AAIW). Less Canth in the eastern basin than the western basin was caused by weaker ventilation driven by SAMW and AAIW formation and subduction and stronger Antarctic Bottom Water (AABW) formation in the former than the latter. In addition to the spatial heterogeneity, Canth increase rates accelerated from the 1990s to the 2000s, consistent with the overall increase in air-sea CO2 exchange in the South Atlantic Ocean. 

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5. Importance of mesoscale eddies and mean circulation in ventilation of the Southern Ocean: VENTILATION OF THE SOUTHERN OCEAN

   https://doi.org/10.1002/2016JC012292  

   Kamenkovich, Igor ; Garraffo, Zulema ; Pennel, Romain ; Fine, Rana A. ( April 2017 , Journal of Geophysical Research: Oceans)