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Title: Bathymetric Modelling of High Mountain Tropical Lakes of Southern Ecuador
Authors: Vazquez Zambrano, Raul Fernando
Hampel , Henrietta
metadata.dc.ucuenca.correspondencia: Vazquez Zambrano, Raul Fernando, raul.vazquezz@ucuenca.edu.ec
Keywords: Ecuadorian Andes
Exceedance probability distribution
Fishing echo-sounder
High mountain lake
Interpolation method
Lake bathymetry
Lake geomorphology
Tropical lake
Weibull plotting position
metadata.dc.ucuenca.areaconocimientofrascatiamplio: 1. Ciencias Naturales y Exactas
metadata.dc.ucuenca.areaconocimientofrascatidetallado: 1.5.10 Recursos Hídricos
metadata.dc.ucuenca.areaconocimientofrascatiespecifico: 1.5 Ciencias de la Tierra y el Ambiente
metadata.dc.ucuenca.areaconocimientounescoamplio: 05 - Ciencias Físicas, Ciencias Naturales, Matemáticas y Estadísticas
metadata.dc.ucuenca.areaconocimientounescodetallado: 0521 - Ciencias Ambientales
metadata.dc.ucuenca.areaconocimientounescoespecifico: 052 - Medio Ambiente
Issue Date: 2024
metadata.dc.ucuenca.volumen: Volumen 6, número 8
metadata.dc.source: Water (Switzerland)
metadata.dc.identifier.doi: 10.3390/w16081142
metadata.dc.type: ARTÍCULO
Abstract: 
Very little is known on high mountain tropical lakes of South America. Thus, the main motivation of this research was obtaining base bathymetric data of 119 tropical lakes of the Cajas National Park (CNP), Ecuador, that could be used in future geomorphological studies. Eleven interpolation methods were applied with the intention of selecting the best one for processing the scattered observations that were collected with a low-cost fishing echo-sounder. A split-sample (SS) test was used and repeated several times considering different proportions of available observations, selected randomly, for training of the interpolation methods and accuracy evaluation of the respective products. This accuracy was assessed through the use of empirical exceedance probability distributions of the mean absolute error (MAE). A single best interpolation method could not be identified. Instead, the study suggested six better-performing methods, including the complex methods Kriging (ordinary), minimum curvature (spline), multiquadric, and TIN with linear interpolation but also the much simpler methods natural neighbour and nearest neighbour. A sensitivity analysis (SA), considering several data error magnitudes, confirmed this. This advocated that sophisticated interpolation methods do not always produce the best products as geomorphological characteristics of the study site(s) together with observation data characteristics are likely to play important roles in their performance. As such, this type of assessment should be carried out in any terrestrial mapping of bathymetry that is based on the interpolation of scattered observations. Upon the analysis of the relative hypsometric curves of the 119 study lakes, they were classified into three average form categories: convex, concave, and mixed. The separated accuracy analysis of these three groups of lakes did not help in identifying a single best method. Finally, the interpolated bathymetries of 114 of the study lakes were incorporated into the best DEM of the study site by equalising their elevation reference systems. It is believed that the resulting enhanced DEM could be a very useful tool for a more appropriate management of these very beautiful but fragile high mountain tropical lakes.
URI: https://www.scopus.com/inward/record.uri?eid=2-s2.0-85191298588&doi=10.3390%2fw16081142&partnerID=40&md5=65e00c6cefae6c2999b0b30c594645b4
metadata.dc.ucuenca.urifuente: https://www.mdpi.com/2073-4441/16/8/1142
ISSN: 2073-4441
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