Assistant Professor of Earth Sciences
Departments and Programs
Hinman Box: HB 6105
B.A. Middlebury College; M.S. University of Otago; Ph.D. University of Maine
Paleoclimatology; climate dynamics; atmospheric chemistry; snow and ice chemistry
Campbell, S.W., Kreutz, K.J., Osterberg, E.C. , Arcone, S.A., Wake, C., Volkening, K., Winski, D., 2011. Flow dynamics of an accumulation basin: a case study of the Upper Kahiltna Glacier on Mount McKinley, Alaska, Journal of Glaciology 10J233 .
Campbell, S.W., Kreutz, K.J., Osterberg, E.C. , Arcone, S.A., Wake, C., Introne, D., Volkening, K., Winski, D., 2011. Melt regimes, internal stratigraphy, and flow dynamics of three glaciers in the Alaska Range, Journal of Glaciology 10J238 .
Osterberg, E.C .,Mayewski, P.A., Kreutz, K.J., et al., 2008. Ice core record of rising lead pollution in the North Pacific atmosphere, Geophys. Res. Lett . doi: 10.1029/2007GL032680.
Fisher, D.A, Osterberg, E.C., Dyke, A. et al., 2008. The Mt. Logan Holocene-Late Wisconsin isotope record: tropical Pacific – Yukon connections, _The Holocene _ 18, 667-677.
Upton, P., Osterberg, E.C ., 2007. Paleoseismicity and mass movements interpreted from seismic-reflection data, Lake Tekapo, South Canterbury, New Zealand, N.Z. J. Geol. Geophys . 50 , 343-356.
Osterberg, E.C ., Handley, M.J., Sneed, S.B., Mayewski, P.A., Kreutz, K.J., 2006. A continuous ice core melter system with discrete sampling for major ion, trace element and stable isotope analyses, Environ. Sci. Technol. 40, 10, 3355-3361.
Osterberg, E.C., 2006. Late Quaternary (Marine Isotope Stages 6-1) seismic sequence stratigraphic evolution of the Otago Continental Shelf, New Zealand, Mar. Geol. 229, 159-178.
Tracking radioactive fallout transport and deposition across the Arctic from the 2011 Japanese Fukushima Dai-ichi disaster; Investigating the response of the Greenland Ice Sheet to previous warm and cold periods during the past 10,000 years; Developing ice core reconstructions of precipitation and climate patterns in central Alaska spanning the past 1,000 years; Reconstructing natural and anthropogenic emissions of mercury from Asia to North America over the past 10,000 years; Constraining the variability of snow accumulation on the northwest Greenland Ice Sheet in space and time.