We estimated monthly air–sea CO 2 fluxes in the Arctic Ocean and its adjacent seas north of
60∘ N from 1997 to 2014. This was done by mapping partial pressure of CO 2 in the surface …

We produced 204 monthly maps of the air–sea CO 2 flux in the Arctic north of 60° N,
including the Arctic Ocean and its adjacent seas, from January 1997 to December 2013 by …

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 …

The Arctic Ocean has experienced an unprecedented reduction in sea ice over the last 3
decades, increasing the potential for greater exchange of gases such as carbon dioxide …

The uptake of carbon dioxide (CO2) by the Arctic Ocean is most likely increasing because of
the rapid sea-ice retreat that lifted the barriers preventing gas exchange and light …

The rapid recent decline of Arctic Ocean sea ice area increases the flux of solar radiation
available for primary production and the area of open water for air‐sea gas exchange. We …

Carbon system data from five expeditions over the time period of 1991 to 2005 in the central
Arctic Ocean are evaluated with respect to the partial pressure of carbon dioxide in the …

The interannual variations of CO2 sources and sinks in the surface waters of the Antarctic
Ocean (south of 50° S) were studied between 1986 and 1994. An existing, slightly modified …

The biogeochemical seascape of the western Arctic coastal ocean is in rapid transition.
Changes in sea ice cover will be accompanied by alterations in sea‐air carbon dioxide …

An inventory and sequestering rate of anthropogenic carbon dioxide CTanthro in the Arctic
Ocean, calculated by a plume‐entrainment model, are presented. The plume is initiated by a …