Influence of the spatial resolution of Digital Elevation Models on water-balance estimations in temporary shallow lakes

• Published in: Journal of hydrology (Amsterdam) 2024-05, Vol.634, p.131098, Article 131098
• Main Authors: Sánchez-Emeterio, Gema, Sanchez-Ramos, David, Aragones, David G., Doña, Carolina, Camacho, Antonio
• Format: Article
• Language: English
• Subjects: basins; case studies; climate change; Digital Elevation Model (DEM); digital elevation models; ecosystems; Hydrological pattern; hydrology; lakes; lidar; Mapping Bathymetry; remote sensing; Shallow Lakes; Spain; Water-Balance Model
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2024.131098

•Different DEMs were used to simulate the water balance of a shallow lake.•Bathymetries obtained from Lidar data and field data showed similar results.•Acceptable water balance results were achieved with Lidar data DEMs until 50 m width.•The resolution of DEMs had a moderate influence on water balance estimations. Many shallow lakes are strongly degraded and their hydroecological functioning has been altered. At the same time, their rate of disappearance is remarkably high compared to other ecosystem types. Moreover, due to their relatively small size and shallow depth these lakes are highly sensitive to meteorological variability, making them highly vulnerable to climate change. The accurate estimation of their water balance is key to identifying proper management strategies. To carefully model the water balance, it is necessary to use a Digital Elevation Model (DEM) of a high-enough spatial resolution to understand the bathymetric relationships of the basin; however, it is not always possible to generate DEMs with field data. Even when DEMs are available, it is still unclear what spatial resolution is adequate to obtain an accurate water balance in shallow lakes. The aim of this work was to analyze the influence that bathymetries from different DEMs may have on shallow lake-water-balance estimations, using Lake Alcahozo (central Spain) as a case study. To do this, hydrological balances were developed with Lidar-derived DEMs with different spatial resolutions, and these balances were compared with one developed from bathymetric field data. The hydrological models obtained were calibrated with limnimetric measurements and validated with estimates of flooded areas calculated via remote-sensing imagery. The main results showed that, to a certain extent, the different resolutions of bathymetries do not have a strong influence on the result of water-balance estimations: DEMs up to a spatial resolution of 50 m (a pixel size representing 0.3 % of the basin area) have shown similar goodness-of-fit in the modeling of the hydrological balances in our case study. Therefore, depending on the objective of the study, Lidar data with different spatial resolutions can be used, up to a minimal resolution that should be determined on a case-by-case basis.