Improving the Evapotranspiration Estimation under Cloudy Condition by Extending the Ts-VI Triangle Model

Evapotranspiration (ET) of soil-vegetation system is the main process of the water and energy exchange between the atmosphere and the land surface. Spatio-temporal continuous ET is vitally important to agriculture and ecological applications. Surface temperature and vegetation index (Ts-VI) triangle...

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Main Authors: Boyang Li, Yaokui Cui, Xiaozhuang Geng, Huan Li
Format: Article
Language:English
Published: MDPI AG 2021-04-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/13/8/1516
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spelling doaj-3b4904babfce40ef9cf90ddae69a369b2021-04-14T23:05:43ZengMDPI AGRemote Sensing2072-42922021-04-01131516151610.3390/rs13081516Improving the Evapotranspiration Estimation under Cloudy Condition by Extending the Ts-VI Triangle ModelBoyang Li0Yaokui Cui1Xiaozhuang Geng2Huan Li3Institute of RS and GIS, School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaInstitute of RS and GIS, School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaInstitute of RS and GIS, School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaInstitute of RS and GIS, School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaEvapotranspiration (ET) of soil-vegetation system is the main process of the water and energy exchange between the atmosphere and the land surface. Spatio-temporal continuous ET is vitally important to agriculture and ecological applications. Surface temperature and vegetation index (Ts-VI) triangle ET model based on remote sensing land surface temperature (LST) is widely used to monitor the land surface ET. However, a large number of missing data caused by the presence of clouds always reduces the availability of the main parameter LST, thus making the remote sensing-based ET estimation unavailable. In this paper, a method to improve the availability of ET estimates from Ts-VI model is proposed. Firstly, continuous LST product of the time series is obtained using a reconstruction algorithm, and then, the reconstructed LST is applied to the estimate ET using the Ts-VI model. The validation in the Heihe River Basin from 2009 to 2011 showed that the availability of ET estimates is improved from 25 days per year (d/yr) to 141 d/yr. Compared with the in situ data, a very good performance of the estimated ET is found with RMSE 1.23 mm/day and R<sup>2</sup> 0.6257 at point scale and RMSE 0.32 mm/day and R<sup>2</sup> 0.8556 at regional scale. This will improve the understanding of the water and energy exchange between the atmosphere and the land surface, especially under cloudy conditions.https://www.mdpi.com/2072-4292/13/8/1516evapotranspirationspatio-temporal continuityland surface temperatureTs-VI ET modelrobust regression
collection DOAJ
language English
format Article
sources DOAJ
author Boyang Li
Yaokui Cui
Xiaozhuang Geng
Huan Li
spellingShingle Boyang Li
Yaokui Cui
Xiaozhuang Geng
Huan Li
Improving the Evapotranspiration Estimation under Cloudy Condition by Extending the Ts-VI Triangle Model
Remote Sensing
evapotranspiration
spatio-temporal continuity
land surface temperature
Ts-VI ET model
robust regression
author_facet Boyang Li
Yaokui Cui
Xiaozhuang Geng
Huan Li
author_sort Boyang Li
title Improving the Evapotranspiration Estimation under Cloudy Condition by Extending the Ts-VI Triangle Model
title_short Improving the Evapotranspiration Estimation under Cloudy Condition by Extending the Ts-VI Triangle Model
title_full Improving the Evapotranspiration Estimation under Cloudy Condition by Extending the Ts-VI Triangle Model
title_fullStr Improving the Evapotranspiration Estimation under Cloudy Condition by Extending the Ts-VI Triangle Model
title_full_unstemmed Improving the Evapotranspiration Estimation under Cloudy Condition by Extending the Ts-VI Triangle Model
title_sort improving the evapotranspiration estimation under cloudy condition by extending the ts-vi triangle model
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2021-04-01
description Evapotranspiration (ET) of soil-vegetation system is the main process of the water and energy exchange between the atmosphere and the land surface. Spatio-temporal continuous ET is vitally important to agriculture and ecological applications. Surface temperature and vegetation index (Ts-VI) triangle ET model based on remote sensing land surface temperature (LST) is widely used to monitor the land surface ET. However, a large number of missing data caused by the presence of clouds always reduces the availability of the main parameter LST, thus making the remote sensing-based ET estimation unavailable. In this paper, a method to improve the availability of ET estimates from Ts-VI model is proposed. Firstly, continuous LST product of the time series is obtained using a reconstruction algorithm, and then, the reconstructed LST is applied to the estimate ET using the Ts-VI model. The validation in the Heihe River Basin from 2009 to 2011 showed that the availability of ET estimates is improved from 25 days per year (d/yr) to 141 d/yr. Compared with the in situ data, a very good performance of the estimated ET is found with RMSE 1.23 mm/day and R<sup>2</sup> 0.6257 at point scale and RMSE 0.32 mm/day and R<sup>2</sup> 0.8556 at regional scale. This will improve the understanding of the water and energy exchange between the atmosphere and the land surface, especially under cloudy conditions.
topic evapotranspiration
spatio-temporal continuity
land surface temperature
Ts-VI ET model
robust regression
url https://www.mdpi.com/2072-4292/13/8/1516
work_keys_str_mv AT boyangli improvingtheevapotranspirationestimationundercloudyconditionbyextendingthetsvitrianglemodel
AT yaokuicui improvingtheevapotranspirationestimationundercloudyconditionbyextendingthetsvitrianglemodel
AT xiaozhuanggeng improvingtheevapotranspirationestimationundercloudyconditionbyextendingthetsvitrianglemodel
AT huanli improvingtheevapotranspirationestimationundercloudyconditionbyextendingthetsvitrianglemodel
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