Research

Research Theme: Oceans

Here is an atmospheric-level view of all the Oceans
research and happenings at INSTAAR.

Research on any aspect of the world’s oceans, from the sea surface to the seafloor. Currents and circulation, water temperature, coastal processes, marine sediments, ocean chemistry, tides, sea ice, and water quality, among other subjects, are all part of the Oceans category.

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Recent Publications

Quay, P., Sonnerup, R., David Munro, Sweeney, C. 2017: Anthropogenic CO2 accumulation and uptake rates in the Pacific Ocean based on changes in the C-13/C-12 of dissolved inorganic carbon. Global Biogeochemical Cycles, 31(1): 59-80. DOI: 10.1002/2016GB005460

Gemery, L., Cronin, T. M., Briggs, W. M., Jr., Brouwers, E. M., Schornikov, E. I., Stepanova, A., Wood, A. M., Yasuhara, M. 2017: An Arctic and Subarctic ostracode database: Biogeographic and paleoceanographic applications. Hydrobiologia, 786(1): 59-95. DOI: 10.1007/s10750-015-2587-4

Gill, E. C., Rajagopalan, B., Molnar, P. H., Kushnir, Y., Tom Marchitto 2017: Reconstruction of Indian summer monsoon winds and precipitation over the past 10,000 years using equatorial pacific SST proxy records. Paleoceanography, 32(2): 195-216. DOI: 10.1002/2016PA002971

Otto-Bliesner, B. L., Alexandra Jahn, Feng, R., Brady, E. C., Hu, A., Löfverström, M. 2017: Amplified North Atlantic warming in the late Pliocene by changes in Arctic gateways. Geophysical Research Letters, 44(2): 957-964. DOI: 10.1002/2016GL071805

Kristjánsdóttir, G. B., Moros, M., John T. AndrewsAnne Jennings 2017: Holocene Mg/Ca, alkenones, and light stable isotope measurements on the outer North Iceland shelf (MD99-2269): A comparison with other multi-proxy data and sub-division of the Holocene. The Holocene, 27(1): 52-62. DOI: 10.1177/0959683616652703

Markle, B. R., Steig, E. J., Buizert, C., Schoenemann, S. W., Bitz, C. M., Fudge, T. J., Pedro, J. B., Ding, Q., Tyler JonesJames W. C. White, Sowers, T. 2017: Global atmospheric teleconnections during Dansgaard–Oeschger events. Nature Geoscience, 10: 36-40. DOI: 10.1038/ngeo2848

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