Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
Authors: |
|
|
---|---|---|
Owners: |
|
This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource. |
Type: | Resource | |
Storage: | The size of this resource is 1.6 KB | |
Created: | Feb 06, 2023 at 8:32 p.m. | |
Last updated: | Feb 06, 2023 at 8:32 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
---|---|
Views: | 592 |
Downloads: | 230 |
+1 Votes: | Be the first one to this. |
Comments: | No comments (yet) |
Abstract
Groundwater is a priceless resource in Alberta and therefore, estimating groundwater are crucial to identifying and promoting holistic and integrated management of groundwater-surface water. However, it is a challenge to simulate groundwater storage due to the current rudimentary representation of two-way groundwater-surface water exchange in current hydrologic models, such as Soil and Water Assessment Tool (SWAT), which, in turn, limits our ability to predict land-atmosphere processes and groundwater storage. In this study, we modified the SWAT model to improve module of evapotranspiration in two-way groundwater-surface water exchange. The modified SWAT was calibrated and validated against the groundwater table height and evapotranspiration from 2008 to 2011 period at two location (Lethbridge and Barons) Alberta, Canada. The results showed that the modified SWAT model predicts the groundwater table height very well at both locations. The modified model predicted the daily groundwater table height with R-2 values of 0.86 and 0.89 in the calibration period (2008-2009), 0.81 and 0.83 for the validation period (2010-2011) at Lethbridge and Barons, respectively. The Nash-Sutcliffe model efficiency (NSE) for daily groundwater table height was 0.69 and 0.71 during calibration periods (2008-2009) while the model gives lower values of NSE 0.65 and 0.67 for validation periods (2010-2011) at Lethbridge and Barons, respectively. Similarly, the model estimates evapotranspiration well with correlation coefficient (R-2) of 0.77 during the calibration period and 0.81 for validation period. Our result showed that the modified SWAT model did improve estimates to dynamic groundwater table heights.
Subject Keywords
Coverage
Spatial
Content
Additional Metadata
Name | Value |
---|---|
DOI | 10.1016/j.jhydrol.2019.05.052 |
Depth | |
Scale | < 100 000 km² |
Layers | 2-5 layers |
Purpose | groundwater resources |
GroMoPo_ID | 17 |
IsVerified | True |
Model Code | SWAT |
Model Link | https://doi.org/10.1016/j.jhydrol.2019.05.052 |
Model Time | 2008 to 2011 |
Model Year | 2019 |
Model Authors | N.D.Melaku, J.Wang |
Model Country | Canada |
Data Available | report/paper only |
Developer Email | junyew@athabascau.ca |
Dominant Geology | Unsure |
Developer Country | Canada |
Publication Title | A modified SWAT module for estimating groundwater table at Lethbridge and Barons, Alberta, Canada |
Original Developer | No |
Additional Information | Modified the groundwater-module in SWAT model to represent two-way groundwater-surface water interactions through considering evapotranspiration |
Integration or Coupling | Surface water |
Evaluation or Calibration | static water levels;dynamic water levels |
Geologic Data Availability |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
Comments
There are currently no comments
New Comment