EP53A-3627:
Glacial Erosion Rates from Bayesian Inversion of Cosmogenic Nuclide Concentrations in a Bedrock Core, Streaked Mtn., ME
EP53A-3627:
Glacial Erosion Rates from Bayesian Inversion of Cosmogenic Nuclide Concentrations in a Bedrock Core, Streaked Mtn., ME
Friday, 19 December 2014
Abstract:
Glacial erosion is an important source of sediment and could be an important coupling to glacier and ice sheet models that track sediment. However, glacial erosion is difficult to quantify, and models of glacial erosion can benefit from independent erosion rate estimates. Here we present the results of a Bayesian Markov chain Monte Carlo (MCMC) inversion of a cosmogenic nuclide (CN) geomorphic model for glacial erosion rates on a bedrock landform formerly eroded beneath the Laurentide ice sheet. The CN 10Be was measured in quartz to 8 m depth in a bedrock core from the summit of Streaked Mountain, ME. ThePatil, A., D. Huard and C.J. Fonnesbeck (2010), PyMC: Bayesian Stochastic Modelling in Python. J. Statistical Software, 35(4), 1-81.
Ploskey, Z.T and J.O. Stone (2013), Measuring glacial erosion of bedrock landforms with cosmogenic nuclide depth profiles, Abstract #EP41A-0794 presented at 2013 Fall Meeting, AGU, San Francisco, Calif., 9-13 Dec.