Laurentide ice saddle mergers drive rapid sea level drops during glaciations

This is PISM v1.0 simulation data from a steady-state simulating the glaciation of Laurentide Ice Sheet by decreasing equilibrium-line altitude (ELA). We use a hybrid stress balance scheme in PISM (shallow ice approximation + shallow shelf approximation) and a thickness-based calving criterion. The...

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Bibliographic Details
Main Author: Ji, W (via Mendeley Data)
Language:unknown
Published: 2021
Subjects:
Ela
Online Access:http://nbn-resolving.org/urn:nbn:nl:ui:13-hu-8oka
https://easy.dans.knaw.nl/ui/datasets/id/easy-dataset:210564
Description
Summary:This is PISM v1.0 simulation data from a steady-state simulating the glaciation of Laurentide Ice Sheet by decreasing equilibrium-line altitude (ELA). We use a hybrid stress balance scheme in PISM (shallow ice approximation + shallow shelf approximation) and a thickness-based calving criterion. The horizontal resolution is 20 km. it includes three ELA decreasing speeds (ELA gradually decreases in 20 kyr, 100kyr, and step changes).