Quaternary paleoclimate of the Arctic, lake sediments, glacier reconstructions, tephrochronology
Utilizing the biogeochemistry of lakes sediments, such as stable isotopes and lipid biomarkers, to reconstruct past environmental changes (e.g. landscape, temperature and hydrology)
David Harning,Áslaug Geirsdóttir,Gifford H. Miller,Leif Anderson{/exp:playa:children, 2016: Episodic expansion of Drangajokull, Vestfiroir, Iceland, over the last 3 ka culminating in its maximum dimension during the Little Ice Age. Quaternary Science Reviews, 152: 118-131. DOI: 10.1016/j.quascirev.2016.10.001
{playaOVMh1kQ8:title},Áslaug Geirsdóttir,Gifford H. Miller,{playaso7p0mJZ:title}{/exp:playa:children, 2016: Early Holocene deglaciation of Drangajokull, Vestfiroir, Iceland. Quaternary Science Reviews, 153: 192-198. DOI: 10.1016/j.quascirev.2016.09.030
Gifford H. Miller, Fellow and Associate Director of INSTAAR