Sparse in situ measurements and poor understanding of the impact of sea ice on air-sea gas exchange introduce large uncertainties to models of polar oceanic carbon uptake. The eddy covariance technique can be used to produce insightful air-sea gas exchange datasets in the presence of sea ice, but results differ between studies. We present a critical review of historical polar eddy covariance studies and can identify only five that present comparable flux datasets. Assessment of ancillary datasets, including sea-ice coverage and type and air-sea concentration gradient of carbon dioxide, used to interpret flux datasets (with a specific focus on their role in estimating and interpreting sea ice zone gas transfer velocities) identif...
Although salt rejection from sea ice is a key process in deep-water formation in ice-covered seas, t...
Air-sea carbon dioxide (CO2) flux is generally estimated by the bulk method using upper ocean CO2 fu...
Air-sea carbon dioxide (CO2) flux is generally estimated by the bulk method using upper ocean CO2 fu...
Sparse in situ measurements and poor understanding of the impact of sea ice on air-sea gas exchange ...
This is the author accepted manuscript. The final version is available from Elsevier via the DOI in ...
The Arctic Ocean is an important sink for atmospheric CO₂. The impact of decreasing sea-ice extent a...
Author Posting. © American Geophysical Union, 2011. This article is posted here by permission of Am...
The Arctic marine environment plays an important role in the global carbon cycle. However, there re...
Given rapid sea ice changes in the Arctic Ocean in the context of climate warming, better constraint...
Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of Am...
The biogeochemical seascape of the western Arctic coastal ocean is in rapid transition. Changes in s...
Sea ice exchanges gases with the atmosphere including climate and ozone-depleting gases We will rapi...
The Arctic Ocean is an important sink for atmospheric CO2. The impact of decreasing sea ice extent a...
The Arctic Ocean (AO) is an important basin for global oceanic carbon dioxide (CO2) uptake, but the ...
Carbon budgets for the polar oceans require better constraint on air–sea gas exchange in the sea ice...
Although salt rejection from sea ice is a key process in deep-water formation in ice-covered seas, t...
Air-sea carbon dioxide (CO2) flux is generally estimated by the bulk method using upper ocean CO2 fu...
Air-sea carbon dioxide (CO2) flux is generally estimated by the bulk method using upper ocean CO2 fu...
Sparse in situ measurements and poor understanding of the impact of sea ice on air-sea gas exchange ...
This is the author accepted manuscript. The final version is available from Elsevier via the DOI in ...
The Arctic Ocean is an important sink for atmospheric CO₂. The impact of decreasing sea-ice extent a...
Author Posting. © American Geophysical Union, 2011. This article is posted here by permission of Am...
The Arctic marine environment plays an important role in the global carbon cycle. However, there re...
Given rapid sea ice changes in the Arctic Ocean in the context of climate warming, better constraint...
Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of Am...
The biogeochemical seascape of the western Arctic coastal ocean is in rapid transition. Changes in s...
Sea ice exchanges gases with the atmosphere including climate and ozone-depleting gases We will rapi...
The Arctic Ocean is an important sink for atmospheric CO2. The impact of decreasing sea ice extent a...
The Arctic Ocean (AO) is an important basin for global oceanic carbon dioxide (CO2) uptake, but the ...
Carbon budgets for the polar oceans require better constraint on air–sea gas exchange in the sea ice...
Although salt rejection from sea ice is a key process in deep-water formation in ice-covered seas, t...
Air-sea carbon dioxide (CO2) flux is generally estimated by the bulk method using upper ocean CO2 fu...
Air-sea carbon dioxide (CO2) flux is generally estimated by the bulk method using upper ocean CO2 fu...