Effects of sea‐ice and biogeochemical processes and storms on under‐ice water f CO 2 during the winter‐spring transition in the high A rctic O cean: Implications for sea‐air CO 2 fluxes

Author:

Fransson Agneta1ORCID,Chierici Melissa2ORCID,Skjelvan Ingunn3,Olsen Are4ORCID,Assmy Philipp1ORCID,Peterson Algot K.4ORCID,Spreen Gunnar5ORCID,Ward Brian6ORCID

Affiliation:

1. Norwegian Polar InstituteFram CentreTromsø Norway

2. Institute of Marine ResearchTromsø Norway

3. Bjerknes Centre for Climate ResearchUni Research ClimateBergen Norway

4. Bjerknes Centre for Climate Research, Geophysical InstituteUniversity of BergenBergen Norway

5. Institute of Environmental PhysicsUniversity of BremenBremen Germany

6. AirSea Laboratory, School of Physics and Ryan InstituteNational University of IrelandGalway Ireland

Funder

Marine Institute

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Reference82 articles.

1. Assmy P. et al. (2016) N‐ICE2015 Water Column Biogeochemistry Norw. Polar Inst. Tromsø Norway doi:10.21334/npolar.2016.3ebb7f64.

2. Leads in Arctic pack ice enable early phytoplankton blooms below snow-covered sea ice

3. Assur A.(1960) Composition of sea ice and its tensile strength U.S. Army Snow Ice Permafrost Res. Estab. Res. Rep. 44 Corps of Eng. Wilmette Ill.

4. A multi-decade record of high-quality fCO<sub>2</sub> data in version 3 of the Surface Ocean CO<sub>2</sub> Atlas (SOCAT)

5. Distribution of CO2species, estimates of net community production, and air-sea CO2exchange in the Ross Sea polynya

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