Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...

GroMoPo Metadata for Evrotas River Basin model


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 08, 2023 at 8:01 p.m.
Last updated: Feb 08, 2023 at 8:01 p.m.
Citation: See how to cite this resource
Sharing Status: Public
Views: 626
Downloads: 213
+1 Votes: Be the first one to 
 this.
Comments: No comments (yet)

Abstract

The objective of this research was to better understand the dynamics of surface-groundwater interactions in a large Mediterranean watershed (Evrotas River Basin) and to improve the seasonal forecasting of a potential hydrological drought under future climate change scenarios. This is achieved by integrating the quasi-distributed watershed Soil and Water Assessment Tool (SWAT) model with the three-dimensional groundwater flow Princeton Transport Code (PTC) model. The combined models are applied to the alluvial plain of Evrotas watershed in Greece by considering the interaction between the stream network and the aquifer to better spatially represent feedback fluxes within the surface and groundwater domains. Model simulation (2007-2011) was in good agreement with field observations demonstrating that this integrated modeling approach provides a more realistic representation of the water exchanges between surface and subsurface domains and constrains more the calibration with the use of both surface and subsurface observed data. Finally, the integrated SWAT-PTC model was used to study the impact of future climate change on surface and groundwater resources of the area under three different climate change scenarios. The results indicate that the study area is very sensitive to potential future climate changes. Upstream reaches display a loss of surface water to underlying groundwater systems whereas downstream the main river receives recharge from groundwater as the water table approached the surface topography. The low flow characterization for the current situation shows that a large part of the stream network will be too dry to accommodate the development of a viable aquatic ecological community throughout the years. In dry periods, the amount of water that is supplied to the aquifer is 40.9% less than the amount of water that is supplied under current climate conditions highlighting the need for new management strategies that must be implemented in order to avoid setbacks in the allocation of water resources in the future.

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Greece
North Latitude
37.5427°
East Longitude
22.7013°
South Latitude
36.8341°
West Longitude
22.1023°

Content

Additional Metadata

Name Value
DOI 10.1007/s12665-017-6721-7
Depth
Scale 1 001 - 10 000 km²
Layers 2
Purpose Surface water - groundwater interaction
GroMoPo_ID 394
IsVerified True
Model Code Princeton transport code
Model Link https://doi.org/10.1007/s12665-017-6721-7
Model Time 2007-2011
Model Year 2017
Model Authors Gamvroudis, C; Dokou, Z; Nikolaidis, NP; Karatzas, GP
Model Country Greece
Data Available Report/paper only
Developer Email christos.gamvroudis@gmail.com
Dominant Geology Model focuses on multiple geologic materials
Developer Country Greece; USA
Publication Title Impacts of surface and groundwater variability response to future climate change scenarios in a large Mediterranean watershed
Original Developer No
Additional Information
Integration or Coupling Surface water
Evaluation or Calibration Transient streamflow
Geologic Data Availability No

How to Cite

GroMoPo, D. Kretschmer (2023). GroMoPo Metadata for Evrotas River Basin model, HydroShare, http://www.hydroshare.org/resource/6ded4c73aae04b7da00e36acf1cecb1f

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

Comments

There are currently no comments

New Comment

required