Evapotranspiration Trends and Interactions in Light of the Anthropogenic Footprint and the Climate Crisis: A Review
Evapotranspiration (ET) is a parameter of major importance participating in both hydrological cycle and surface energy balance. Trends of ET are discussed along with the dependence of evaporation to key environmental variables. The evaporation paradox can be approached via natural phenomena aggravat...
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Format: | Article |
Language: | English |
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MDPI AG
2021-11-01
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Series: | Hydrology |
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Online Access: | https://www.mdpi.com/2306-5338/8/4/163 |
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author | Stavroula Dimitriadou Konstantinos G. Nikolakopoulos |
author_facet | Stavroula Dimitriadou Konstantinos G. Nikolakopoulos |
author_sort | Stavroula Dimitriadou |
collection | DOAJ |
description | Evapotranspiration (ET) is a parameter of major importance participating in both hydrological cycle and surface energy balance. Trends of ET are discussed along with the dependence of evaporation to key environmental variables. The evaporation paradox can be approached via natural phenomena aggravated by anthropogenic impact. ET appears as one of the most affected parameters by human activities. Complex hydrological processes are governed by local environmental conditions thus generalizations are difficult. However, in some settings, common hydrological interactions could be detected. Mediterranean climate regions (MCRs) appear vulnerability to the foreseen increase in ET, aggravated by precipitation shifting and air temperature warming, whereas in tropical forests its role is rather beneficial. ET determines groundwater level and quality. Groundwater level appeared to be a robust predictor of annual ET for peatlands in Southeast Asia. In semi-arid to arid areas, increases in ET have implications on water availability and soil salinization. ET-changes after a wildfire can be substantial for groundwater recharge if a canopy-loss threshold is surpassed. Those consequences are site-specific. Post-fire ET rebound seems climate and fire-severity-dependent. Overall, this qualitative structured review sets the foundations for interdisciplinary researchers and water managers to deploy ET as a means to address challenging environmental issues such as water availability. |
first_indexed | 2024-03-10T03:58:51Z |
format | Article |
id | doaj.art-c33de9e9a351467291a302153cafd386 |
institution | Directory Open Access Journal |
issn | 2306-5338 |
language | English |
last_indexed | 2024-03-10T03:58:51Z |
publishDate | 2021-11-01 |
publisher | MDPI AG |
record_format | Article |
series | Hydrology |
spelling | doaj.art-c33de9e9a351467291a302153cafd3862023-11-23T08:39:29ZengMDPI AGHydrology2306-53382021-11-018416310.3390/hydrology8040163Evapotranspiration Trends and Interactions in Light of the Anthropogenic Footprint and the Climate Crisis: A ReviewStavroula Dimitriadou0Konstantinos G. Nikolakopoulos1Department of Geology, University of Patras, 26504 Rion, GreeceDepartment of Geology, University of Patras, 26504 Rion, GreeceEvapotranspiration (ET) is a parameter of major importance participating in both hydrological cycle and surface energy balance. Trends of ET are discussed along with the dependence of evaporation to key environmental variables. The evaporation paradox can be approached via natural phenomena aggravated by anthropogenic impact. ET appears as one of the most affected parameters by human activities. Complex hydrological processes are governed by local environmental conditions thus generalizations are difficult. However, in some settings, common hydrological interactions could be detected. Mediterranean climate regions (MCRs) appear vulnerability to the foreseen increase in ET, aggravated by precipitation shifting and air temperature warming, whereas in tropical forests its role is rather beneficial. ET determines groundwater level and quality. Groundwater level appeared to be a robust predictor of annual ET for peatlands in Southeast Asia. In semi-arid to arid areas, increases in ET have implications on water availability and soil salinization. ET-changes after a wildfire can be substantial for groundwater recharge if a canopy-loss threshold is surpassed. Those consequences are site-specific. Post-fire ET rebound seems climate and fire-severity-dependent. Overall, this qualitative structured review sets the foundations for interdisciplinary researchers and water managers to deploy ET as a means to address challenging environmental issues such as water availability.https://www.mdpi.com/2306-5338/8/4/163actual evapotranspirationpotential evapotranspirationreference evapotranspirationevaporationevaporation paradoxglobal dimming |
spellingShingle | Stavroula Dimitriadou Konstantinos G. Nikolakopoulos Evapotranspiration Trends and Interactions in Light of the Anthropogenic Footprint and the Climate Crisis: A Review Hydrology actual evapotranspiration potential evapotranspiration reference evapotranspiration evaporation evaporation paradox global dimming |
title | Evapotranspiration Trends and Interactions in Light of the Anthropogenic Footprint and the Climate Crisis: A Review |
title_full | Evapotranspiration Trends and Interactions in Light of the Anthropogenic Footprint and the Climate Crisis: A Review |
title_fullStr | Evapotranspiration Trends and Interactions in Light of the Anthropogenic Footprint and the Climate Crisis: A Review |
title_full_unstemmed | Evapotranspiration Trends and Interactions in Light of the Anthropogenic Footprint and the Climate Crisis: A Review |
title_short | Evapotranspiration Trends and Interactions in Light of the Anthropogenic Footprint and the Climate Crisis: A Review |
title_sort | evapotranspiration trends and interactions in light of the anthropogenic footprint and the climate crisis a review |
topic | actual evapotranspiration potential evapotranspiration reference evapotranspiration evaporation evaporation paradox global dimming |
url | https://www.mdpi.com/2306-5338/8/4/163 |
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