Minimizing the impact of ocean acidification requires an understanding of species
responses and environmental variability of population habitats. Whereas the literature is …

The turbulent mixing in thin ocean surface boundary layers (OSBL), which occupy the upper
100 m or so of the ocean, control the exchange of heat and trace gases between the …

The efficiency of transfer of gases and particles across the air-sea interface is controlled by
several physical, biological and chemical processes in the atmosphere and water which are …

Gas transfer velocities (k) of CO2 and CH4 were determined from 209 deployments of a
newly designed floating chamber in six mangrove dominated estuaries in Australia and the …

Oceans alleviate the accumulation of atmospheric CO 2 by absorbing approximately a
quarter of all anthropogenic emissions. In the deep oceans, carbon uptake is dominated by …

The European Research Infrastructure Consortium “Integrated Carbon Observation
System”(ICOS) aims at delivering high quality greenhouse gas (GHG) observations and …

Grid and spectral nudging are effective ways of preventing drift from large-scale weather
patterns in regional climate models. However, the effect of nudging on the wind speed …

In situ measurements representing the marine atmosphere and air–sea interaction are taken
at ships, buoys, stationary moorings and land-based towers, where each observation …

Air‐sea exchange of gaseous elemental mercury (Hg0) is not well constrained, even though
it is a major component of the global Hg cycle. Lack of Hg0 flux measurements to validate …

Combination of surface water cooling and a deep ocean mixed layer generates convective
eddies scaling with the depth of a mixed layer that enhances the efficiency of the air‐sea …