3.8 Proceedings Paper

IMPROVEMENT OF THE TECHNIQUES FOR THE COMPUTATION OF EVAPOTRANSPIRATION MAPS

出版社

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/isprs-archives-XLIII-B3-2022-997-2022

关键词

Evapotranspiration; Remote Sensing; Copernicus; Sentinel Satellite; Sen-ET

资金

  1. Research Fund for the Italian Electrical System

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This study aims to establish a methodology for estimating suitable areas for new renewable sources by identifying possible indexes, such as evapotranspiration, to describe the fields. Different procedures, including the use of satellite images, have been tested to compute evapotranspiration. The results are compared with those obtained from traditional hydrological models, revealing interesting findings for continuous monitoring of water-stressed areas.
The definition of a methodology for estimating suitable areas for new renewable sources needs to identify possible indexes that describe the fields. One interesting index is the Evapotranspiration (ET). This is usually determined from hydrological models, which however do not provide a real-time estimation. So, new different procedures have been tested to compute it, for example, the use of Satellite images. The Sen-ET project allows using the Copernicus data to compute daily evapotranspiration. An improvement in the automatization of methodology is presented within this work. The model is tested in two different Italian regions with different climates and geographical conditions, considering also different months to study the results in different seasons over the same area. Results are then compared with those obtained in the same areas and period with two hydrological models (BIGBANG and GlobWat). The different outputs are analysed according to their spatial resolutions and respect to agricultural land cover classes. The comparison between Sen-ET evapotranspiration maps and hydrological model results has shown, in the analysed areas, relevant differences and suggests interesting future insights for continuous monitoring of land subject to water stress.

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