Net primary production (NPP) is the foundation of the oceans' ecosystems and the fisheries
they support. In the Arctic Ocean, NPP is controlled by a complex interplay of light and …

The ongoing uptake of anthropogenic carbon by the ocean leads to ocean acidification, a
process that results in a reduction in pH and in the saturation state of biogenic calcium …

Accurately predicting future ocean acidification (OA) conditions is crucial for advancing OA
research at regional and global scales, and guiding society's mitigation and adaptation …

The ocean attenuates global warming by taking up about one quarter of global
anthropogenic carbon emissions. Around 40% of this carbon sink is located in the Southern …

Ocean acidity extreme events are short-term periods of relatively high [H+] concentrations.
The uptake of anthropogenic CO 2 emissions by the ocean is expected to lead to more …

As a contribution to the Regional Carbon Cycle Assessment and Processes phase 2
(RECCAP2) project, we present synthesized estimates of Arctic Ocean sea‐air CO2 fluxes …

Future ocean acidification mainly depends on the continuous ocean uptake of CO 2 from the
atmosphere. The trajectory of future atmospheric CO 2 is prescribed in traditional climate …

The ocean is a major carbon sink and takes up 25%–30% of the anthropogenically emitted
CO2. A state‐of‐the‐art method to quantify this sink are global ocean biogeochemistry …

In combination with drastic emission reduction cuts, limiting global warming below 1.5 C or 2
C requires atmospheric carbon dioxide removal (CDR) of up to 16 GtCO 2 yr− 1 by 2050 …

The inflow of Atlantic Water to the Arctic Ocean is a crucial determinant for the future
trajectory of this ocean basin with regard to warming, loss of sea ice, and ocean acidification …