A second general method for cooling the planet involves removing carbon dioxide (CO2) from the atmosphere, either via sequestration or CO2 capture, or possibly
through ocean iron fertilization to promote the growth of CO2 - consuming algae.
Not exact matches
Possible mechanisms include (iv)
fertilization of phytoplankton growth in the Southern
Ocean by increased deposition of iron - containing dust from the atmosphere after being carried by winds from colder, drier continental areas, and a subsequent redistribution of limiting nutrients; (v) an increase in the whole ocean nutrient content (e.g., through input of material exposed on shelves or nitrogen fixation); and (vi) an increase in the ratio between carbon and other nutrients assimilated in organic material, resulting in a higher carbon export per unit of limiting nutrient expo
Ocean by increased deposition of
iron - containing dust from the atmosphere after being carried by winds from colder, drier continental areas, and a subsequent redistribution of limiting nutrients; (v) an increase in the whole
ocean nutrient content (e.g., through input of material exposed on shelves or nitrogen fixation); and (vi) an increase in the ratio between carbon and other nutrients assimilated in organic material, resulting in a higher carbon export per unit of limiting nutrient expo
ocean nutrient content (e.g.,
through input of material exposed on shelves or nitrogen fixation); and (vi) an increase in the ratio between carbon and other nutrients assimilated in organic material, resulting in a higher carbon export per unit of limiting nutrient exported.
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.
Potential carbon dioxide (CO2) drawdown
through dust - induced
iron fertilization of
ocean biota is restricted to high - nutrient, low - chlorophyll (HNLC) regions, mainly the Southern Ocean and northern Pacific where iron is the limiting micronutrient (6,
ocean biota is restricted to high - nutrient, low - chlorophyll (HNLC) regions, mainly the Southern
Ocean and northern Pacific where iron is the limiting micronutrient (6,
Ocean and northern Pacific where
iron is the limiting micronutrient (6, 13).
Far riskier is intentional acceleration of carbon dioxide removal by enhancing the biological uptake in the
ocean through iron fertilization.