VISCOUS HEATING in the Earths Mantle Induced by Glacial Loading L. Hanyk 1, C. Matyska 1, D. A. Yuen 2 and B. J. Kadlec 2 1 Department of Geophysics, Faculty.
Zheng-Tian Lu Physics Division, Argonne National Laboratory Department of Physics, University of Chicago Supported by Department of Energy, Office of Nuclear.
8:309:00Executive SessionNSF/consultants 9:009:30Overview of SB groupGrannis 9:3010:00Atlas overview, HV system, outreachMcCarthy 10:0010:30Atlas calibrations,
Mid-Pleistocene Revolution By Robert Spellacy. MPR Describes the transition between 41kyr and 100kyr glacial –interglacial cycles. Initiated between 900-650.
"AlSiC-Based Hybrid Composite Tool Kit" By Richard W. Adams and Mark A. Occhionero Ceramics Process Systems 111 South Worcester St Chartley MA 02712-0338.
External Causes Change in incoming radiation Change in composition of the atmosphere Change in Earth’s surface Feedback Mechanisms Water vapor-greenhouse.
Abrupt Climate Change Paleoceanography Presentation 6/15/2015 By Beth Hart ?
A High-Resolution Record of Late Quaternary Aeolian Activity at Witpan, South Africa: Palaeoclimatic and Palaeoenvironmental Implications Matt Telfer Prof.
Marketing Section. Def: Individuals or companies that are interested in your particular product or service and are willing to pay for it (Who & Where)
Lecture 13 Orbital-Scale Interactions, Feedbacks and Unresolved Problems The Cause of Glacial Cycles? (Chapter 11)
Lecture 10: Orbital Control of Ice Sheets (Chapter 9)