Sediment Supply to the Global Ocean
In this lab, we are using a theoretical river basin of ~1990 km2, with 1200m of relief and a river length of ~100 km. All parameters that are shown by default once the HydroTrend model is loaded are based on a present-day, temperate climate.
Whereas these runs are not meant to be specific, we are using parameters that are realistic for the Waiapaoa River in New Zealand. The Waiapaoa River, located on North Island, receives high rain and has erodible soils, so the river sediment loads are exceptionally high. It has been called the 'dirtiest small river in the world'. A more detailed description of applying HydroTrend to the Waipaoa basin has been published in Water Resources Research: http://dx.doi.org/10.1029/2006WR005570. To learn more about HydroTrend and its approach to sediment supply modeling, download the presentation listed below.This lab can be run on the CSDMS JupyterHub. (If you don't already have an account, follow the instructions to sign up at: https://csdms.colorado.edu/wiki/JupyterHub.) Run the lab Notebook by clicking the "start" link under the Run online heading at the top of this page. If you're an educator using this lab in a class, you can get CSDMS JupyterHub accounts for students. For more information, please contact us through the CSDMS Help Desk: https://github.com/csdms/help-desk.
Download associated file: SedimentSupplyModeling02_2013.ppt
Learn more about HydroTrend and its approach to sediment supply modeling from this presentation.
- Use pymt to run the HydroTrend model
- Become familiar with a basic configuration of the HydroTrend model
- Make small changes to key input parameters in HydroTrend
- Gain hands-on experience with visualizing output in Python
- Explore the HydroTrend base-case river simulation
- Explore how a river system responds to climate change
- Learn how humans can affect river sediment loads
>> Open a new browser window and go to: https://pymt.readthedocs.io/en/latest/examples.html
>> You will see that there are several example models. In this lab we will select the HydroTrend model.
>> Click on the "Launch Binder" button to run this lab.
Note that Binder is a free and popular service for running Jupyter Notebooks, so it can be slow to load at times.
The HydroTrend model is run with the Python Modeling Tool, pymt. Learn more about pymt at: https://pymt.readthedocs.io.For a similar lab done with a spreadsheet, download and try: https://csdms.colorado.edu/csdms_wiki/images/RiverFluxtoOceanSpreadsheetLab.zip.
If run locally, this lab requires the installtion of pymt; see https://pymt.readthedocs.io/en/latest/quickstart.html for instructions. This lab runs on Linux and macOS.
This material is based upon work supported by the National Science Foundation under Grant No. 1831623, Community Facility Support: The Community Surface Dynamics Modeling System (CSDMS).
- Kettner, A.J., and Syvitski, J.P.M., 2008. HydroTrend version 3.0: a Climate-Driven Hydrological Transport Model that Simulates Discharge and Sediment Load leaving a River System. Computers & Geosciences, 34(10), 1170-1183. doi: 10.1016/j.cageo.2008.02.008