Modeling Phytoplankton Blooms and Inorganic Carbon Responses to Sea‐Ice Variability in the West Antarctic Peninsula-Reference-Cited by-同舟云学术

Modeling Phytoplankton Blooms and Inorganic Carbon Responses to Sea‐Ice Variability in the West Antarctic Peninsula

Published:2021-04 Issue:4 Volume:126 Page:
ISSN:2169-8953
Container-title:Journal of Geophysical Research: Biogeosciences
language:en
Short-container-title:J Geophys Res Biogeosci

Author:

Schultz C.¹²³^ORCID,Doney S. C.¹^ORCID,Hauck J.⁴^ORCID,Kavanaugh M. T.⁵,Schofield O.⁶^ORCID

Affiliation:

1. Department of Environmental Sciences University of Virginia Charlottesville VA USA

2. Department of Marine Chemistry and Geochemistry Woods Hole Oceanographic Institution Woods Hole MA USA

3. Department of Earth and Atmospheric Sciences Massachusetts Institute of Technology Cambridge MA USA

4. Marine Biogeoscience Division Alfred‐Wegener‐Institut Helmholtz‐Zentrum für Polar und Meeresforschung Bremerhaven Germany

5. Ocean Ecology and Biogeochemistry College of Earth, Ocean, and Atmospheric Sciences Oregon State University Corvallis OR USA

6. Department of Marine and Coastal Sciences Center for Ocean Observing Leadership School of Environmental and Biological Sciences Rutgers University New Brunswick NJ USA

Funder

National Science Foundation

University of Virginia

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JG006227

Reference56 articles.

1. Controls on dissolved and particulate iron distributions in surface waters of the Western Antarctic Peninsula shelf

2. Comparative roles of upwelling and glacial iron sources in Ryder Bay, coastal western Antarctic Peninsula

3. Coastal Southern Ocean: A strong anthropogenic CO2sink

4. Early Spring Phytoplankton Dynamics in the Western Antarctic Peninsula

5. Evidences of strong sources of DFe and DMn in Ryder Bay, Western Antarctic Peninsula

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