A dynamic continental runoff routing model applied to the last Northern Hemisphere deglaciation

We describe and evaluate a dynamical continental runoff routing model for the Northern Hemisphere that calculates the runoff pathways in response to topographic modifications due to changes in ice thickness and isostatic adjustment. The algorithm is based on the steepest gradient method and takes as...

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Bibliographic Details
Main Authors: H. Goelzer, I. Janssens, J. Nemec, P. Huybrechts
Format: Article
Language:English
Published: Copernicus Publications 2012-05-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/5/599/2012/gmd-5-599-2012.pdf