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Effects of Human Activities on Evapotranspiration and Its Components in Arid Areas

With the increasing impact of human activities on the environment, evapotranspiration (ET) has changed in arid areas, which further affects the water resources availability in the region. Therefore, understanding the impact of human activities on ET and its components is helpful to the management of...

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Autores principales: Liu, Yunfei, Gui, Dongwei, Yin, Changjun, Zhang, Lei, Xue, Dongping, Liu, Yi, Ahmed, Zeeshan, Zeng, Fanjiang
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9956289/
https://www.ncbi.nlm.nih.gov/pubmed/36833495
http://dx.doi.org/10.3390/ijerph20042795
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author Liu, Yunfei
Gui, Dongwei
Yin, Changjun
Zhang, Lei
Xue, Dongping
Liu, Yi
Ahmed, Zeeshan
Zeng, Fanjiang
author_facet Liu, Yunfei
Gui, Dongwei
Yin, Changjun
Zhang, Lei
Xue, Dongping
Liu, Yi
Ahmed, Zeeshan
Zeng, Fanjiang
author_sort Liu, Yunfei
collection PubMed
description With the increasing impact of human activities on the environment, evapotranspiration (ET) has changed in arid areas, which further affects the water resources availability in the region. Therefore, understanding the impact of human activities on ET and its components is helpful to the management of water resources in arid areas. This study verified the accuracy of Fisher’s model (PT-JPL model) for ET estimation in southern Xinjiang, China by using the evaporation complementarity theory dataset (AET dataset). The ET and the evapotranspiration components (T:E) of six land-use types were estimated in southern Xinjiang from 1982 to 2015, and the impact of human activities on ET was analyzed. In addition, the impact of four environmental factors (temperature (Temp), net radiation (Rn), relative humidity (RH), and NDVI) on ET were evaluated. The results showed that the calculated ET values of the PT-JPL model were close to the ET values of the AET dataset. The correlation coefficient (R(2)) was more than 0.8, and the NSE was close to 1. In grassland, water area, urban industrial and mining land, forest land, and cultivated land, the ET values were high, and in unused land types, the ET values were the lowest. The T:E values varied greatly in urban industrial and mining land, forest land, and cultivated land, which was due to the intensification of human activities, and the values were close to 1 in summer in recent years. Among the four environmental factors, temperature largely influenced the monthly ET. These findings suggest that human activities have significantly reduced soil evaporation and improved water use efficiency. The impact of human activities on environmental factors has caused changes in ET and its components, and appropriate oasis expansion is more conducive to regional sustainable development.
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spelling pubmed-99562892023-02-25 Effects of Human Activities on Evapotranspiration and Its Components in Arid Areas Liu, Yunfei Gui, Dongwei Yin, Changjun Zhang, Lei Xue, Dongping Liu, Yi Ahmed, Zeeshan Zeng, Fanjiang Int J Environ Res Public Health Article With the increasing impact of human activities on the environment, evapotranspiration (ET) has changed in arid areas, which further affects the water resources availability in the region. Therefore, understanding the impact of human activities on ET and its components is helpful to the management of water resources in arid areas. This study verified the accuracy of Fisher’s model (PT-JPL model) for ET estimation in southern Xinjiang, China by using the evaporation complementarity theory dataset (AET dataset). The ET and the evapotranspiration components (T:E) of six land-use types were estimated in southern Xinjiang from 1982 to 2015, and the impact of human activities on ET was analyzed. In addition, the impact of four environmental factors (temperature (Temp), net radiation (Rn), relative humidity (RH), and NDVI) on ET were evaluated. The results showed that the calculated ET values of the PT-JPL model were close to the ET values of the AET dataset. The correlation coefficient (R(2)) was more than 0.8, and the NSE was close to 1. In grassland, water area, urban industrial and mining land, forest land, and cultivated land, the ET values were high, and in unused land types, the ET values were the lowest. The T:E values varied greatly in urban industrial and mining land, forest land, and cultivated land, which was due to the intensification of human activities, and the values were close to 1 in summer in recent years. Among the four environmental factors, temperature largely influenced the monthly ET. These findings suggest that human activities have significantly reduced soil evaporation and improved water use efficiency. The impact of human activities on environmental factors has caused changes in ET and its components, and appropriate oasis expansion is more conducive to regional sustainable development. MDPI 2023-02-04 /pmc/articles/PMC9956289/ /pubmed/36833495 http://dx.doi.org/10.3390/ijerph20042795 Text en © 2023 by the authors. https://creativecommons.org/licenses/by/4.0/Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
spellingShingle Article
Liu, Yunfei
Gui, Dongwei
Yin, Changjun
Zhang, Lei
Xue, Dongping
Liu, Yi
Ahmed, Zeeshan
Zeng, Fanjiang
Effects of Human Activities on Evapotranspiration and Its Components in Arid Areas
title Effects of Human Activities on Evapotranspiration and Its Components in Arid Areas
title_full Effects of Human Activities on Evapotranspiration and Its Components in Arid Areas
title_fullStr Effects of Human Activities on Evapotranspiration and Its Components in Arid Areas
title_full_unstemmed Effects of Human Activities on Evapotranspiration and Its Components in Arid Areas
title_short Effects of Human Activities on Evapotranspiration and Its Components in Arid Areas
title_sort effects of human activities on evapotranspiration and its components in arid areas
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9956289/
https://www.ncbi.nlm.nih.gov/pubmed/36833495
http://dx.doi.org/10.3390/ijerph20042795
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