Heat and carbon uptake in the Southern Ocean: the state of the art and future priorities

Meijers, Andrew J. S.; Quéré, Corinne Le; Monteiro, Pedro M. S.; Sallée, Jean‐Baptiste

doi:10.1098/rsta.2022.0071

Cited by 1 publication

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References 12 publications

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“…The Southern Ocean plays an essential role in mitigating the rate of climate change through its globally disproportionate uptake of anthropogenic carbon dioxide (CO 2 ) and the associated excess planetary heat (Friedlingstein et al., 2022; Frölicher et al., 2015). However, the processes controlling heat and CO 2 uptake remain poorly understood as evidenced by the divergence in projected estimates by state‐of‐the‐art Earth System Models (ESMs) (Fox‐Kemper et al., 2021; Friedlingstein et al., 2022; Frölicher et al., 2015; Hauck et al., 2020; Meijers et al., 2023; Sallée et al., 2023). There is much debate regarding the spatio‐temporal scales of motion required to be explicitly resolved by ESMs, and whether resolving finer scales will result in model convergence (Fox‐Kemper et al., 2019; Hewitt et al., 2020).…”

Section: Introductionmentioning

confidence: 99%

The Heat and Carbon Characteristics of Modeled Mesoscale Eddies in the South–East Atlantic Ocean

Smith,

Nicholson,

Engelbrecht

et al. 2023

JGR Oceans

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Mesoscale eddies provide critical links between the atmosphere and the ocean interior modulating the exchanges of key climatic tracers across the air‐sea and mixed‐layer interface. Mesoscale eddies, widespread in the Southern Ocean, are unresolved by Earth System Models; to what extent they modify contemporary and future heat and CO2 uptake remains unknown. The missing contribution of mesoscale eddies and their effects on properties and fluxes of heat and CO2 are investigated in the South‐East Atlantic using a mesoscale resolving (1/12°) physical biogeochemical model. Unsupervised Self‐Organizing Maps are used to separate anticyclonic and cyclonic eddies into distinct sub‐categories based on spatial characteristics in relative vorticity. Thermal drivers dominated over non‐thermal on partial pressure of ocean CO2 (pCO2sw) leading to a weaker CO2 sink in anticyclonic eddies and a stronger CO2 sink in cyclonic eddies relative to the climatological mean. Magnitudes and depth extents of tracer anomalies scale with eddy size but are also dependent on background tracer gradients. Resolving only the largest (>50 km radii) eddies leads to underestimations in total magnitude of heat storage by 52% and 77%, and underestimations of 61% and 77% in dissolved inorganic carbon (CT) storage for anticyclonic and cyclonic eddies respectively. The inclusion of smaller eddy features (<50 km) also offsets the asymmetry in heat and CT storage between anticyclonic and cyclonic eddies. Resolving eddies explicitly or improvements in existing parameterizations that fail to sufficiently include eddy effects are crucial to improving estimates of heat and CO2.

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