There is strong evidence for a tight relation of
Southern Ocean iron fertilization to this record (30, 31).
--
Southern Ocean Iron Fertilization Experiment (SOFeX)-- The basics of the most recent expedition — Penny Chisholm's site, which lists many professional papers — Paul Falkowski's article (PDF document)-- DOE article: Climate Change Scenarios Compel Studies of Ocean Carbon Storage — Government site for carbon sequestration research — An earlier piece Williams wrote on sequestration — Will Ocean Fertilization To Remove Carbon Dioxide from the Atmosphere Work?
From recent article «Iron fertilization enhanced net community production but not downward particle flux during
the Southern Ocean iron fertilization experiment LOHAFEX», by P. Martin, M. Rutgers van der Loeff, N. Cassar, P. Vandromme, F. d'Ovidio, L. Stemmann, R. Rengarajan,... Continue reading →
Not exact matches
(
Iron fertilization enthusiasts focus on the
Southern Ocean because other seas have much more natural algae, so growing blooms might just foster growth that would have happened anyway.)
Oceanographers have long recognized that
iron fertilization in the
Southern Ocean will drive phytoplankton blooms.
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.
There have been
iron fertilization experiments of the
ocean before, many of them, in the equatorial Pacific, the Southern Ocean, and the North Pac
ocean before, many of them, in the equatorial Pacific, the
Southern Ocean, and the North Pac
Ocean, and the North Pacific.
Blain, S. Effect of natural
iron fertilization on carbon sequestration in the
Southern Ocean.
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.
For
iron fertilization forcing, we choose temperature − dust relationships from the high
southern latitudes, as the Southern Ocean is the main region where this process is r
southern latitudes, as the
Southern Ocean is the main region where this process is r
Southern Ocean is the main region where this process is relevant.
To estimate the role of time - varying,
ocean iron fertilization, we turned to the Southern Ocean, the main HNLC, iron - limited region of the global o
ocean iron fertilization, we turned to the
Southern Ocean, the main HNLC, iron - limited region of the global o
Ocean, the main HNLC,
iron - limited region of the global
oceanocean.
Here we took a different approach by seeking and applying dust deposition observations from hotspots for dust radiative and
iron fertilization forcing: NH subtropical latitudes and the
Southern Ocean.
This allows us to scale the two records by their respective interglacial levels, combine them to better resolve the
Southern Ocean, and use the combined record as our proxy for glacial / interglacial
iron fertilization forcing.
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).
This is how the model deals with
iron fertilization strength in the Southern Ocean (SO; see Dust Radiative and Iron Fertilization Forcin
iron fertilization strength in the Southern Ocean (SO; see Dust Radiative and Iron Fertilizati
fertilization strength in the
Southern Ocean (SO; see Dust Radiative and
Iron Fertilization Forcin
Iron FertilizationFertilization Forcings).
Early climate models hinted that intentional
iron fertilization across the entire
southern Ocean could erase 1 billion to 2 billion tons of carbon emissions each year — 10 to 25 percent of the world's annual total.