View the new short film highlighting Ocean Carbon & Biogeochemistry research and the exciting technology scientists are using to understand the oceans of today and tomorrow.
View the new short film highlighting Ocean Carbon & Biogeochemistry research and the exciting technology scientists are using to understand the oceans of today and tomorrow.
How does the enormous diversity of zooplankton species, life cycles, size, feeding ecology, and physiology affect their role in ocean food webs and cycling of carbon? In the 2017 issue of Annual Review of Marine Science, Steinberg and Landry review the fundamental and multifaceted roles that zooplankton play in the cycling and export of carbon […]
The sea surface microlayer (SML) is the boundary interface between the atmosphere and ocean, spanning the uppermost ~1 mm of the ocean. Covering 70% of the Earth’s surface, the SML supports a rich diversity of life, serving as an incubator for eggs and larvae. The SML controls air-sea interactions and serves as an important hotspot […]
Dongxiao Zhang1,2, Meghan F. Cronin2, Xiaopei Lin3, Ryuichiro Inoue4, Andrea J. Fassbender5, Stuart P. Bishop6, Adrienne Sutton2 1. University of Washington 2. NOAA Pacific Marine Environmental Laboratory 3. Ocean University of China, China 4. Japan Agency for Marine-Earth Science and Technology, Japan 5. Monterey Bay Aquarium Research Institute 6. North Carolina State University Western […]
Alison R. Gray1, Jaime Palter2 1. University of Washington 2. University of Rhode Island Estimates of contemporary global air-sea carbon dioxide (CO2) flux (Takahashi et al. 2009; Landschützer et al. 2014) suggest that subtropical western boundary currents (WBCs) and their zonal extensions are key regions of oceanic carbon uptake (Figure 1a). These narrow, intensified currents, which […]
WBC Series Guest Editors: Andrea J. Fassbender1 and Stuart P. Bishop2 1. Monterey Bay Aquarium Research Institute 2. North Carolina State University Western boundary current (WBC) regions are often studied for their intensity of air-sea interaction and mesoscale variability, yet research addressing the implications of these characteristics for biogeochemical cycling has lagged behind. WBCs, and […]
Keith B. Rodgers1, Ping Zhai1, Daniele Iudicone2, Olivier Aumont3, Brendan Carter4, Andrea J. Fassbender5, Stephen M. Griffies6, Yves Plancherel7, Laure Resplandy8, Richard D. Slater1, Katsuya Toyama9 1. Princeton University 2. Stazione Anton Dohrn, Italy 3. Sorbonne Universités, LOCEAN/IPSL, France 4. University of Washington 5. Monterey Bay Aquarium Research Institute 6. NOAA Geophysical Fluid Dynamics Laboratory […]
Bo Qiu1, Eitarou Oka2, Stuart P. Bishop3, Shuiming Chen1, Andrea J. Fassbender4 1. University of Hawaii at Manoa 2. The University of Tokyo 3. North Carolina State University 4. Monterey Bay Aquarium Research Institute After separating from the Japanese coast at 36°N, 141°E, the Kuroshio enters the open basin of the North Pacific, where it […]
Sophie Clayton1, Peter Gaube1, Takeyoshi Nagai2, Melissa M. Omand3, Makio Honda4 1. University of Washington 2. Tokyo University of Marine Science and Technology, Japan 3. University of Rhode Island 4. Japan Agency for Marine-Earth Science and Technology, Japan Western boundary current (WBC) regions are largely thought to be hotspots of productivity, biodiversity, and carbon export. […]
Antarctic shelf systems generate the densest waters in the world. These shelf waters are the building blocks of Antarctic Bottom Water, the ocean’s abyssal water mass. These bottom waters have the potential to sequester carbon out of the atmosphere for millennia. One such form of marine carbon is dissolved organic carbon (DOC). DOC is produced […]
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Funding for the Ocean Carbon & Biogeochemistry Project Office is provided by the National Science Foundation (NSF) and the National Aeronautics and Space Administration (NASA). The OCB Project Office is housed at the Woods Hole Oceanographic Institution.