People

Faculty & Staff

Joseph Licciardi

Joseph M. Licciardi
Associate Professor of Earth Sciences

Ph.D. Oregon State University, 2000
e-mail address: joe.licciardi@unh.edu
603-862-3135


Primary Courses taught:

Graduate students:

My past and current research integrates field work, laboratory techniques, and modeling studies in order to resolve key issues in Quaternary geology, with a unifying theme of understanding mechanisms of climate change.

One ongoing research focus has been the development of alpine glacier and pluvial lake records of late Pleistocene climate variability across the western U.S. A centerpiece of this research, funded by the National Science Foundation, is a high-resolution 3He and 10Be chronology of glaciation in greater Yellowstone and the Teton Range. Another major research aim, also funded by the National Science Foundation, is to improve knowledge of deglacial and volcanic events in Iceland. Work in Iceland has focused on 3He dating of subglacially erupted tuyas, which indicate the ice surface elevation at the time of their eruption. An integral component of the western U.S. and Iceland projects is the calibration of cosmogenic 3He and 36Cl production rates, which are critical to obtaining accurate exposure ages.

Newly developed research involves 10Be dating of early Holocene and ‘Little Ice Age’ glacier fluctuations in southern Peru, with results suggesting climate teleconnections between the tropics and the North Atlantic region. I have also recently worked with graduate students on investigating late-glacial moraines in the central Alaska Range, and developing a Pleistocene temperature history of a pluvial lake basin in eastern Oregon.

Another broad research interest concerns the role of the Laurentide Ice Sheet in the glacial-age climate system. Earlier research involved numerical reconstructions of ice sheet geometry and its sensitivity to subglacial sediment deformation. Subsequent work reconstructed changes in the routing and flux of North American freshwater runoff. More recently, the Laurentide reconstructions are being used as boundary conditions in work that examines the mechanisms and impacts of rapid ice sheet retreat during the early Holocene.

Publications

Recent Abstracts

Graduate Student Projects


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