This directory contains sea level output used to calculate change in slope, the manually located locations of cutoffs and meanders, the boundaries of the downstream distance for river reaches, and shape files of centerlines for the studies rivers.

The above data was used in the paper: 
“Glacial isostatic adjustment modulates lateral migration rate and morphology of the Red River (North Dakota, USA and Manitoba, Canada)” in Geophysical Research Letters
by Samuel T. Kodama, Tamara Pico, Noah J. Finnegan, Mathieu G. A. Lapôtre, and Jane K. Willenbring
 

Included is:

SEA LEVEL OUTPUT
ice6g_deg_vm5a.mat
ice6g_deg_127p515.mat
ice6g_deg_96p530.mat
ice6g_deg_96p510.mat
ice6g_deg_96p410.mat
ice6g_deg_71p43.mat
gi36_96p510.mat
ANU_6gt_127p515.mat
ANU_6gt_96p530.mat
ANU_6gt_96p510.mat
ANU_6gt_71p43.mat

Naming convention of the files follows IceHistory_EarthStructure
The Earth Structure is XXpYZZ where YY is lithospheric thickness (km), pY is 0.Y x 10^21 (Pa s) for upper mantle viscosity, and ZZ is ZZ x 10^21 (Pa s) for lower mantle viscosity. 
i.e.) 127p515 has lithospheric thickness of 127 km, 0.5 x 10^21 (Pa s) upper mantle viscosity, and 15 x 10^21 (Pa s) lower mantle viscosity.

To calculate relative sea level at a given time-step you must subtract the final time-step (0 ka) from the time-step of interest.

timesteps for the sea level output is found in 
timesteps.mat

RIVER CENTERLINES
RedRiver_CL.shp
AssiniboineRiver_CL.shp
RedLakeRiver_CL.shp

CUTOFF AND MEANDER LOCATIONS AND RIVER REACH BOUNDARIES
RedRiver.xlsx
AssiniboineRiver.xlsx
RedLakeRiver.xlsx

Each file contains the tabs:
Cutoffs
Meanders
Elevation
River Reach Boundaries