The carbon cycle of the coastal ocean is a dynamic component of the global carbon budget.
But the diverse sources and sinks of carbon and their complex interactions in these waters …

The recent warming in the Arctic is affecting a broad spectrum of physical, ecological, and
human/cultural systems that may be irreversible on century time scales and have the …

We have estimated global air–sea CO 2 fluxes (fg CO 2) from the open ocean to coastal
seas. Fluxes and associated uncertainty are computed from an ensemble-based …

Owing to anthropogenic-induced acidification, surface waters of the high latitudes are
projected to become persistently undersaturated with respect to aragonite as early as mid …

At present, although seasonal sea-ice cover mitigates atmosphere-ocean gas exchange, the
Arctic Ocean takes up carbon dioxide (CO 2) on the order of− 66 to− 199 Tg C year− 1 (10 …

Over the past decade, estimates of the atmospheric CO2 uptake by continental shelf seas
were constrained within the 0.18–0.45 Pg C yr− 1 range. However, most of those estimates …

The increase in anthropogenic carbon dioxide emissions and attendant increase in ocean
acidification and sea ice melt act together to decrease the saturation state of calcium …

Observations from the last decade suggest an important role of sea ice in the global
biogeochemical cycles, promoted by (i) active biological and chemical processes within the …

Sea ice in the Arctic Ocean has undergone an unprecedented reduction in area and
thickness in the last decade, exposing an ever increasing fraction of the sea surface to solar …

Net Arctic Ocean primary production (PP) is expected to increase over this century, due to
less perennial sea ice and more available light, but could decrease depending on changes …