The Evapotranspiration in a Changing Climate: In-Situ Measurements, Remote Sensing, Modeling, and Application

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "New Sensors, New Technologies and Machine Learning in Water Sciences".

Deadline for manuscript submissions: closed (30 November 2021) | Viewed by 2634

Special Issue Editors


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Guest Editor
Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China
Interests: evapotranspiration; large-scale hydrological processes; remote sensing of hydrology; water-carbon coupling; hydrological modeling and prediction
Special Issues, Collections and Topics in MDPI journals
Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China
Interests: evapotranspiration; land surface processes; land-atmosphere interactions; hydrological processes

Special Issue Information

Dear Colleagues,

Evapotranspiration (ET) is a key component in Earth’s water, energy, and carbon cycles and affects the climate and ecosystem via a wide range of feedbacks acting on air temperature, humidity, and precipitation. An accurate estimation of ET is therefore a requirement, but it is challenging both in situ and remotely, introducing uncertainties for model parameterization development and validation. Since 1802, when John Dalton published his pioneering work on evaporation, remarkable achievements have been made by the community in understanding ET processes at varying spatiotemporal scales. However, there are numerous remaining questions in critical ET-based science and application from local to global scales due to limitations in our observation and simulation skills.

In this Special Issue, we are calling for papers that address ET scientific topics in coordination with efforts in different regions of the world, aiming to synthesize results at the global scale. We invite papers covering, but not limited to, the following topics:

(1) Better measurements and modeling of ET and its components (soil evaporation, plant transpiration, and canopy interception) at multiple scales from plot to regional and global scales;

(2) Estimating evaporation/sublimation from unconventional land surfaces including water bodies (especially inland lakes), snow, and glaciers;

(3) Challenges and opportunities in quantifying ET trends in a changing climate using state-of-the-art techniques;

(4) Responses and feedbacks of ET to climate change and anthropogenic activities;

(5) Role of ET in drought monitoring, agricultural management, and water resources; and

(6) Employing high-resolution ET products for improved hydrological and/or climate modeling in poorly gauged regions of the world.

Prof. Dr. Yongqiang Zhang
Dr. Ning Ma
Guest Editors

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Keywords

  • evapotranspiration
  • advanced techniques in ET measurement
  • remote sensing of ET
  • multiscale ET estimation
  • responses of ET to climate change and human activities
  • feedbacks of ET to climate

Published Papers (1 paper)

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Research

15 pages, 2791 KiB  
Article
Spatiotemporal Variations and Influencing Factors of Terrestrial Evapotranspiration and Its Components during Different Impoundment Periods in the Three Gorges Reservoir Area
by Yongyue Ji, Qingqing Tang, Lingyun Yan, Shengjun Wu, Liming Yan, Daming Tan, Jilong Chen and Qiao Chen
Water 2021, 13(15), 2111; https://0-doi-org.brum.beds.ac.uk/10.3390/w13152111 - 31 Jul 2021
Cited by 9 | Viewed by 2114
Abstract
Identifying the spatiotemporal variations and influencing climate factors of evapotranspiration (ET) and its components (vegetation transpiration (Ec), soil evaporation (Es), and canopy interception evaporation (Ei)) can greatly improve our understanding of water cycle, carbon cycle, and biogeochemical processes in a warming climate. As [...] Read more.
Identifying the spatiotemporal variations and influencing climate factors of evapotranspiration (ET) and its components (vegetation transpiration (Ec), soil evaporation (Es), and canopy interception evaporation (Ei)) can greatly improve our understanding of water cycle, carbon cycle, and biogeochemical processes in a warming climate. As the world′s largest hydropower project, the construction of the Three Gorges Project (TGP) coupled with the significant land use/land cover change affected the regional water and energy exchange in the Three Gorges Reservoir Area (TGRA). This study aimed to reveal the spatiotemporal variations and influencing climate factors in ET and its components using PML-V2 products in TGRA during 2000–2020. Results showed that the mean annual ET, Ec, Es, and Ei in TGRA were 585.12, 328.49, 173.07, and 83.56 mm, respectively. The temporal variation of ET was dominated by Ec, with no significant change in the time trend. Es decreased (2.92 mm/y) and Ei increased (1.66 mm/y) significantly mainly in the cultivated land. ET, Ec, and Ei showed a similar seasonal variation pattern with a single peak, while Es presented a bimodal pattern. From the pre-impoundment to the first impoundment period, ET and Ec mainly increased in the head of TGRA, meanwhile, Es in urban area increased significantly by 27.8%. In the subsequent impoundment periods, ET and Ec changed slightly while Es sharply decreased. The Ei increased persistently during different impoundment period. The dominant climate factors affecting changes in Ec and Es were air temperature, vapor pressure deficit, and sunshine hours, while the variation of Ei was mainly affected by air temperature, vapor pressure deficit, and precipitation. Full article
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