Based on a century of ocean plankton science and the 10 international experiments on
iron fertilization over the last 15 years we are confident that the scale, methods and technologies of the work we are planning will have positive impacts on all fronts, improving water quality, buffering surface water acidity, recharging the marine food chain, and safely sequestering enormous amounts of CO2 to help slow climate change.
Not exact matches
Following the SOFeX
iron -
fertilization experiment in the Southern Ocean, deep - diving Carbon Explorer floats continuously collected data for
over a year, straight through the Antarctic winter.
We carried out a number of DCESS model simulations
over the last three glacial cycles using the dust radiative and / or
iron fertilization forcings shown in Fig. 4 and Fig.
We also made combined radiative and
iron fertilization forcing simulations
over the last three glacial cycles (Figs.
Comparison with data and data - based reconstructions
over the last glacial cycle of a model simulation for combined dust radiative and
iron fertilization forcing.
While controlled
iron fertilization experiments have shown an increase in phytoplankton growth, and a temporary increase in drawdown of atmospheric CO2, it is uncertain whether this would increase carbon transfer into the deep ocean
over the longer - term.