Performance of Satellite-Based Evapotranspiration Models in Temperate Pastures of Southern Chile

Farmers in the temperate zone of southern Chile have started to irrigate historically rainfed pastures during recent years to reduce dairy productivity losses against increasingly severe summer droughts. The lack of information on pasture water requirements (i.e., evapotranspiration), however, hampe...

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Main Authors: Italo Moletto-Lobos, Cristian Mattar, Jonathan Barichivich
Format: Article
Language:English
Published: MDPI AG 2020-12-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/12/3587
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author Italo Moletto-Lobos
Cristian Mattar
Jonathan Barichivich
author_facet Italo Moletto-Lobos
Cristian Mattar
Jonathan Barichivich
author_sort Italo Moletto-Lobos
collection DOAJ
description Farmers in the temperate zone of southern Chile have started to irrigate historically rainfed pastures during recent years to reduce dairy productivity losses against increasingly severe summer droughts. The lack of information on pasture water requirements (i.e., evapotranspiration), however, hampers the implementation of efficient irrigation programs. Here, we use in-situ observations to evaluate the skill of four remote sensing Surface Energy Balance (SEB) models and two satellite-based global evapotranspiration products (PML_V2 and GLEAM) to estimate actual evapotranspiration (ET<sub>a</sub>) of pastures in southern Chile during 2014–2017. Daily ET<sub>a</sub> measured at an evaluation site over the period ranges between 1.2 mm and 6.2 mm day<sup>−1</sup> during the growing season (October–March), with an annual maximum of about 4.8 mm day<sup>−1</sup> in January and a minimum 0.6 mm day<sup>−1</sup> in June. Only the Simplified SEB (SEBS) model and its operational variant (SSEBop) and the PML_V2 global evapotranspiration product perform well, capturing 63–79% of the variance of in-situ evapotranspiration with an error between 0.75 mm day<sup>−1</sup> and 1.1 mm day<sup>−1</sup>. The readily available PML_V2 product can be used as a convenient way to determine average water footprint of pastures and the two SEBs models can be implemented to monitor irrigation requirements in near-real time from field to regional scales. These results demonstrated a high potential of satellite observations for monitoring evapotranspiration and quantify the water footprint of pastures in southern Chile for a sustainable irrigation practice.
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spelling doaj.art-13e4896794ee48ce825b5628ebe2b4402023-11-21T01:52:35ZengMDPI AGWater2073-44412020-12-011212358710.3390/w12123587Performance of Satellite-Based Evapotranspiration Models in Temperate Pastures of Southern ChileItalo Moletto-Lobos0Cristian Mattar1Jonathan Barichivich2Laboratory for Analysis of the Biosphere (LAB), University of Chile, Santiago 1030000, ChileLaboratory of Geosciences, University of Aysén, Calle Obispo Vielmo N_62, Coyhaique 5952039, ChileInstituto de Conservación Biodiversidad y Territorio, Universidad Austral de Chile, Valdivia 5090000, ChileFarmers in the temperate zone of southern Chile have started to irrigate historically rainfed pastures during recent years to reduce dairy productivity losses against increasingly severe summer droughts. The lack of information on pasture water requirements (i.e., evapotranspiration), however, hampers the implementation of efficient irrigation programs. Here, we use in-situ observations to evaluate the skill of four remote sensing Surface Energy Balance (SEB) models and two satellite-based global evapotranspiration products (PML_V2 and GLEAM) to estimate actual evapotranspiration (ET<sub>a</sub>) of pastures in southern Chile during 2014–2017. Daily ET<sub>a</sub> measured at an evaluation site over the period ranges between 1.2 mm and 6.2 mm day<sup>−1</sup> during the growing season (October–March), with an annual maximum of about 4.8 mm day<sup>−1</sup> in January and a minimum 0.6 mm day<sup>−1</sup> in June. Only the Simplified SEB (SEBS) model and its operational variant (SSEBop) and the PML_V2 global evapotranspiration product perform well, capturing 63–79% of the variance of in-situ evapotranspiration with an error between 0.75 mm day<sup>−1</sup> and 1.1 mm day<sup>−1</sup>. The readily available PML_V2 product can be used as a convenient way to determine average water footprint of pastures and the two SEBs models can be implemented to monitor irrigation requirements in near-real time from field to regional scales. These results demonstrated a high potential of satellite observations for monitoring evapotranspiration and quantify the water footprint of pastures in southern Chile for a sustainable irrigation practice.https://www.mdpi.com/2073-4441/12/12/3587evapotranspirationGLEAMPML_V2pasturegrasslandremote sensing
spellingShingle Italo Moletto-Lobos
Cristian Mattar
Jonathan Barichivich
Performance of Satellite-Based Evapotranspiration Models in Temperate Pastures of Southern Chile
Water
evapotranspiration
GLEAM
PML_V2
pasture
grassland
remote sensing
title Performance of Satellite-Based Evapotranspiration Models in Temperate Pastures of Southern Chile
title_full Performance of Satellite-Based Evapotranspiration Models in Temperate Pastures of Southern Chile
title_fullStr Performance of Satellite-Based Evapotranspiration Models in Temperate Pastures of Southern Chile
title_full_unstemmed Performance of Satellite-Based Evapotranspiration Models in Temperate Pastures of Southern Chile
title_short Performance of Satellite-Based Evapotranspiration Models in Temperate Pastures of Southern Chile
title_sort performance of satellite based evapotranspiration models in temperate pastures of southern chile
topic evapotranspiration
GLEAM
PML_V2
pasture
grassland
remote sensing
url https://www.mdpi.com/2073-4441/12/12/3587
work_keys_str_mv AT italomolettolobos performanceofsatellitebasedevapotranspirationmodelsintemperatepasturesofsouthernchile
AT cristianmattar performanceofsatellitebasedevapotranspirationmodelsintemperatepasturesofsouthernchile
AT jonathanbarichivich performanceofsatellitebasedevapotranspirationmodelsintemperatepasturesofsouthernchile