Abstract

This study was conducted in the Zamora Huayco (ZH) river basin, located in the inter-Andean region of southern Ecuador. The objective was to describe, through land use/land cover change (LUCC), the natural physical processes under current conditions and to project them to 2029. Moreover, temperature and precipitation forecasts were estimated to detail possible effects of climate change. Using remote sensing techniques, satellite images were processed to prepare a projection to 2029. Water recharge was estimated considering the effects of slope, groundcover, and soil texture. Flash floods were estimated using lumped models, concatenating the information to HEC RAS. Water availability was estimated with a semi-distributed hydrological model (SWAT). Precipitation and temperature data were forecasted using autoregressive and exponential smoothing models. Under the forecast, forest and shrub covers show a growth of 6.6%, water recharge projects an increase of 7.16%. Flood flows suffer a reduction of up to 16.54%, and the flow regime with a 90% of probability of exceedance is 1.85% (7.72 l/s) higher for 2029 than for the 2019 scenario, so an improvement in flow regulation is evident. Forecasts show an increase in average temperature of 0.11 °C and 15.63% in extreme rainfall by 2029. Therefore, intervention strategies in Andean basins should be supported by prospective studies that use these key variables of the system for an integrated management of water resources.

Highlights

  • Land use/land cover change (LUCC) impacts on various natural physical processes within watersheds have been extensively investigated worldwide [1,2]

  • Under the forecast, forest and shrub covers show a growth of 6.6%, water recharge projects an increase of 7.16%

  • Our study focuses on the integrated water resources management (IWRM) in Andean basins

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Summary

Introduction

Land use/land cover change (LUCC) impacts on various natural physical processes within watersheds have been extensively investigated worldwide [1,2]. The location of the Andean basins within intervention policies has been the subject of analysis over the last several decades [3,4,5]. Changes and distribution of land use have an important influence on natural processes in a basin [1,2]. For example, shows sensitivity to different coverage due to the different infiltration rates that can occur under the same precipitation conditions [6,7], which is the reason why a change or alteration must be analyzed to evaluate its consequences. That is why water recharge was estimated in order to evaluate the effects that LUCC would have on it. The areas of the basin that favored it were spatially represented [8,9,10]

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