Empirical wave runup models implemented in Python for coastal engineers and scientists.
Wave runup refers to the final part of a wave's journey as it travels from offshore onto the beach. It is observable by anyone who goes to the beach and watches the edge of the water "runup" and rundown the beach. It is comprised of two components:
- setup: the height of the time averaged superelevation of the mean water level above the Still Water Level (SWL)
- swash: the height of the time varying fluctuation of the instantaneous water level about the setup elevation
Setup, swash and other components of Total Water Level (TWL) rise are shown in this handy figure below.
Figure from Vitousek et al. (2017) [1]
Wave runup can contribute a significant portion of the increase in TWL in coastal storms causing erosion and inundation. For example, Stockdon et al. (2006) [2] collated data from numerous experiments, some of which showed wave runup 2% excedence heights in excess of 3 m during some storms.
Given the impact such a large increase in TWL can have on coastlines, there has been much research conducted to try improve our understanding of wave runup processes. Although there are many processes which can influence wave runup (such as nonlinear wave transformation, wave reflection, three-dimensional effects, porosity, roughness, permeability and groundwater) [3], many attempts have been made to derive empirical relatinoships based on easily measurable parameters. Typically, empirical wave runup models include:
- Hs: significant wave height
- Tp: peak wave length
- beta: beach slope
This python package attempts to consolidate the work done by others in this field and collate the numerous empirical relationships for wave runup which have been published.
Installation of py-wave-runup
can be done with pip:
pip install py-wave-runup
from py_wave_runup import models
model_sto06 = models.Stockdon2006(Hs=4, Tp=12, beta=0.1)
model_sto06.R2 # 2.54
model_sto06.setup # 0.96
model_sto06.sinc # 2.06
model_sto06.sig # 1.65
Documentation is located at https://py-wave-runup.readthedocs.io.
- Fork it (https://github.com/chrisleaman/py-wave-runup/fork)
- Create your feature branch (
git checkout -b feature/fooBar
) - Commit your changes (
git commit -am 'Add some fooBar
) - Push to the branch (
git push origin feature/fooBar
) - Create a new Pull Request
Distributed under the GNU General Public License v3.
[1] | Vitousek, Sean, Patrick L. Barnard, Charles H. Fletcher, Neil Frazer, Li Erikson, and Curt D. Storlazzi. "Doubling of Coastal Flooding Frequency within Decades Due to Sea-Level Rise." Scientific Reports 7, no. 1 (May 18, 2017): 1399. https://doi.org/10.1038/s41598-017-01362-7. |
[2] | Stockdon, Hilary F., Robert A. Holman, Peter A. Howd, and Asbury H. Sallenger. "Empirical Parameterization of Setup, Swash, and Runup." Coastal Engineering 53, no. 7 (May 1, 2006): 573-88. https://doi.org/10.1016/j.coastaleng.2005.12.005 |
[3] | United States, Army, and Corps of Engineers. Coastal Engineering Manual. Washington, D.C.: U.S. Army Corps of Engineers, 2006. |