Dense waters formed in the Nordic Seas spill across gaps in the Greenland-Scotland Ridge
into the abyss of the North Atlantic to feed the lower limb of the Atlantic Meridional …

The ocean is currently a significant net sink for anthropogenically remobilised CO 2, taking
up around 24% of global emissions. Numerical models predict a diversity of responses of …

The processes of warming, anthropogenic CO2 (Canth) accumulation, decreasing pHT
(increasing [H+] T; concentration in total scale) and calcium carbonate saturation in the …

We evaluate the decadal evolution of ventilation and anthropogenic carbon (Cant) in the
Nordic Seas between 1982 and the 2010s. Ventilation changes on decadal timescale are …

Tidewater glaciers are highly vulnerable to climate change due to warming from both
atmospheric and seawater sources. Most tidewater glaciers are rapidly retreating, but little is …

The Atlantic meridional overturning circulation (AMOC) is a critical element of Earth's climate
system and it is currently weakening. While this weakening is frequently explained by …

In this study we present hydrography, biogeochemistry and sediment trap observations
between 2003 and 2012 at Porcupine Abyssal Plain (PAP) sustained observatory in the …

Vertical water mass structure in the Polar North Atlantic Ocean plays a critical role in
planetary climate by influencing the formation rate of North Atlantic deepwater, which in turn …

This study compares inter-annual dynamics of the two biomass dominant copepods in the
Iceland Sea, the North Atlantic species Calanus finmarchicus and the Arctic C. hyperboreus …

Mangroves, saltmarshes, and seagrasses are known as blue carbon ecosystems because of
their high rates of productivity and efficiency in sequestering carbon. Carbon can be stored …