@article{Shook-2021-WDPM:,
title = "WDPM: the Wetland DEM Ponding Model",
author = "Shook, Kevin and
Spiteri, Raymond J. and
Pomeroy, John W. and
Liu, Tonghe and
Sharomi, Oluwaseun and
Shook, Kevin and
Spiteri, Raymond J. and
Pomeroy, John W. and
Liu, Tonghe and
Sharomi, Oluwaseun",
journal = "Journal of Open Source Software, Volume 6, Issue 64",
volume = "6",
number = "64",
year = "2021",
publisher = "The Open Journal",
url = "https://gwf-uwaterloo.github.io/gwf-publications/G21-152001",
doi = "10.21105/joss.02276",
pages = "2276",
abstract = "The hydrography of the Canadian Prairies and adjacent northern US Great Plains is unusual in that the landscape is flat and recently formed due to the effects of pleistocene glaciation and a semi-arid climate since holocene deglaciation. Therefore, there has not been sufficient energy, time, or runoff water to carve typical dendritic surface water drainage networks in many locations. In these regions, runoff is often detented and sometimes stored by the millions of depressions (known locally as {``}potholes{''} or {``}sloughs{''}) that cover the landscape.",
}
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<abstract>The hydrography of the Canadian Prairies and adjacent northern US Great Plains is unusual in that the landscape is flat and recently formed due to the effects of pleistocene glaciation and a semi-arid climate since holocene deglaciation. Therefore, there has not been sufficient energy, time, or runoff water to carve typical dendritic surface water drainage networks in many locations. In these regions, runoff is often detented and sometimes stored by the millions of depressions (known locally as “potholes” or “sloughs”) that cover the landscape.</abstract>
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%0 Journal Article
%T WDPM: the Wetland DEM Ponding Model
%A Shook, Kevin
%A Spiteri, Raymond J.
%A Pomeroy, John W.
%A Liu, Tonghe
%A Sharomi, Oluwaseun
%J Journal of Open Source Software, Volume 6, Issue 64
%D 2021
%V 6
%N 64
%I The Open Journal
%F Shook-2021-WDPM:
%X The hydrography of the Canadian Prairies and adjacent northern US Great Plains is unusual in that the landscape is flat and recently formed due to the effects of pleistocene glaciation and a semi-arid climate since holocene deglaciation. Therefore, there has not been sufficient energy, time, or runoff water to carve typical dendritic surface water drainage networks in many locations. In these regions, runoff is often detented and sometimes stored by the millions of depressions (known locally as “potholes” or “sloughs”) that cover the landscape.
%R 10.21105/joss.02276
%U https://gwf-uwaterloo.github.io/gwf-publications/G21-152001
%U https://doi.org/10.21105/joss.02276
%P 2276
Markdown (Informal)
[WDPM: the Wetland DEM Ponding Model](https://gwf-uwaterloo.github.io/gwf-publications/G21-152001) (Shook et al., GWF 2021)
ACL
- Kevin Shook, Raymond J. Spiteri, John W. Pomeroy, Tonghe Liu, Oluwaseun Sharomi, Kevin Shook, Raymond J. Spiteri, John W. Pomeroy, Tonghe Liu, and Oluwaseun Sharomi. 2021. WDPM: the Wetland DEM Ponding Model. Journal of Open Source Software, Volume 6, Issue 64, 6(64):2276.