tupdate readme for clarity - granular-channel-hydro - subglacial hydrology model for sedimentary channels (HTM) git clone git://src.adamsgaard.dk/granular-channel-hydro (DIR) Log (DIR) Files (DIR) Refs (DIR) README (DIR) LICENSE --- (DIR) commit f35dfcc4086c4dbbbec93ae2e6885e8a10850707 (DIR) parent 3c1886f85c00fc3f7f1ea8f3a885b8e273636698 (HTM) Author: Anders Damsgaard <andersd@riseup.net> Date: Tue, 17 Oct 2017 13:40:50 -0400 update readme for clarity Diffstat: M README.md | 16 +++++++++------- 1 file changed, 9 insertions(+), 7 deletions(-) --- (DIR) diff --git a/README.md b/README.md t@@ -1,12 +1,14 @@ # README -Supplementary code for *Sediment behavior controls equilibrium width of -subglacial channels* (A. Damsgaard, J. Suckale, J.A. Piotrowski, M. Houssais, -M.R. Siegfried, H.A. Fricker) accepted for publication in Journal of -Glaciology. +This repository contains supplementary code for *Sediment behavior controls +equilibrium width of subglacial channels* (A. Damsgaard, J. Suckale, J.A. +Piotrowski, M. Houssais, M.R. Siegfried, H.A. Fricker) accepted for publication +in Journal of Glaciology. -This finite-difference example implementation will simulate the dynamics of a -1d channel segment along a square-root ice geometry, with constant water -pressure at the terminus. +The finite-difference example implementation (`1d-channel.py`) simulates the +dynamics of a 1d channel segment along a square-root ice geometry, with +constant water pressure at the terminus. The channel is forced with constant +water influx and evolves its geometry according to fluvial sediment transport, +and plasticity-related limits to channel size. ## License GNU Public License v3 or later, see `LICENSE.md` for details.