Abstract Purpose of Review The changes or updates in ocean biogeochemistry component
have been mapped between CMIP5 and CMIP6 model versions, and an assessment made …

Fossil fuel combustion, land use change and other human activities have increased the
atmospheric carbon dioxide (CO2) abundance by about 50% since the beginning of the …

We describe the baseline coupled model configuration and simulation characteristics of
GFDL's Earth System Model Version 4.1 (ESM4. 1), which builds on component and coupled …

Anthropogenic climate change is projected to lead to ocean warming, acidification,
deoxygenation, reductions in near-surface nutrients, and changes to primary production, all …

The coastal ocean contributes to regulating atmospheric greenhouse gas concentrations by
taking up carbon dioxide (CO2) and releasing nitrous oxide (N2O) and methane (CH4). In …

This contribution to the RECCAP2 (REgional Carbon Cycle Assessment and Processes)
assessment analyzes the processes that determine the global ocean carbon sink, and its …

The current generation of Earth system models used by the United Nations to project future
climate scenarios (CMIP6) relies heavily on marine biogeochemical models to track the fate …

Abstract We assess the Southern Ocean CO2 uptake (1985–2018) using data sets gathered
in the REgional Carbon Cycle Assessment and Processes Project Phase 2. The Southern …

The ocean slows global warming by currently taking up around one-quarter of all human-
made CO 2 emissions. However, estimates of the ocean anthropogenic carbon uptake vary …

The seasonal cycle is the dominant mode of variability in the air‐sea CO2 flux in most
regions of the global ocean, yet discrepancies between different seasonality estimates are …