Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past Decades

The heterogeneous ecosystems in the Mediterranean Basin (MB) are becoming sensitive to water stress. To investigate the climatic stress, a water budget study was conducted over the basin using TerraClimate simulations for a long temporal range (1990–2020). According to the budget accounting, foreste...

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Main Authors: Unnisa, Zaib, Govind, Ajit, Lasserre, Bruno, Marchetti, Marco
Format: Journal Article
Language:Inglés
Published: MDPI 2023
Subjects:
Online Access:https://hdl.handle.net/10568/139692
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author Unnisa, Zaib
Govind, Ajit
Lasserre, Bruno
Marchetti, Marco
author_browse Govind, Ajit
Lasserre, Bruno
Marchetti, Marco
Unnisa, Zaib
author_facet Unnisa, Zaib
Govind, Ajit
Lasserre, Bruno
Marchetti, Marco
author_sort Unnisa, Zaib
collection Repository of Agricultural Research Outputs (CGSpace)
description The heterogeneous ecosystems in the Mediterranean Basin (MB) are becoming sensitive to water stress. To investigate the climatic stress, a water budget study was conducted over the basin using TerraClimate simulations for a long temporal range (1990–2020). According to the budget accounting, forested regions received the highest precipitation (P) on average compared to other land use types (annual mean ≈633 mm yr−1), and even then, they were in a water deficit state (−0.42 mm yr−1). Tree plantations in North Africa (Libya and Morocco) were also in a water deficit state; however, their average P was very low (≈12 mm yr−1) compared to that of northern parts of the MB, and the average Actual Evapotranspiration (AET) was ≈15 mm yr−1. Also, the water balance in other land use systems (rain-fed, irrigated croplands, and rangelands) was either negative or near zero. As a whole, the basin’s average annual P was ≈538 mm yr−1, the annual average AET was ≈415 mm yr−1, and the runoff (Q) was equivalent to 123 mm yr−1, which shows a strong influence of ET over the region. Since runoff was negligible in most dry areas, the AET’s large contribution was notable in the North African base of the Atlas Mountains including the Nile delta region. This indicates that precipitation and evaporation are the principal mechanisms of the water balance in the MB. The result shows strong climate variability over Southern Europe, Turkey, and the western Balkans in the recent years, affecting the AET and making their land use systems more vulnerable to water stress. This benchmark study signifies the consistent need for water storage in the Mediterranean vegetation systems of the basin. It also indicates two distinct climate clusters for water balance modeling.
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spelling CGSpace1396922025-12-08T10:29:22Z Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past Decades Unnisa, Zaib Govind, Ajit Lasserre, Bruno Marchetti, Marco climate change water availability Mediterranean region mediterranean climate ecosystems The heterogeneous ecosystems in the Mediterranean Basin (MB) are becoming sensitive to water stress. To investigate the climatic stress, a water budget study was conducted over the basin using TerraClimate simulations for a long temporal range (1990–2020). According to the budget accounting, forested regions received the highest precipitation (P) on average compared to other land use types (annual mean ≈633 mm yr−1), and even then, they were in a water deficit state (−0.42 mm yr−1). Tree plantations in North Africa (Libya and Morocco) were also in a water deficit state; however, their average P was very low (≈12 mm yr−1) compared to that of northern parts of the MB, and the average Actual Evapotranspiration (AET) was ≈15 mm yr−1. Also, the water balance in other land use systems (rain-fed, irrigated croplands, and rangelands) was either negative or near zero. As a whole, the basin’s average annual P was ≈538 mm yr−1, the annual average AET was ≈415 mm yr−1, and the runoff (Q) was equivalent to 123 mm yr−1, which shows a strong influence of ET over the region. Since runoff was negligible in most dry areas, the AET’s large contribution was notable in the North African base of the Atlas Mountains including the Nile delta region. This indicates that precipitation and evaporation are the principal mechanisms of the water balance in the MB. The result shows strong climate variability over Southern Europe, Turkey, and the western Balkans in the recent years, affecting the AET and making their land use systems more vulnerable to water stress. This benchmark study signifies the consistent need for water storage in the Mediterranean vegetation systems of the basin. It also indicates two distinct climate clusters for water balance modeling. 2023-05-02 2024-02-27T16:26:03Z 2024-02-27T16:26:03Z Journal Article https://hdl.handle.net/10568/139692 en Open Access MDPI Unnisa, Z.; Govind, A.; Lasserre, B.; Marchetti, M. 2023. Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past Decades. Water 2023, 15, 1889. https://doi.org/10.3390/w15101889
spellingShingle climate change
water availability
Mediterranean region
mediterranean climate
ecosystems
Unnisa, Zaib
Govind, Ajit
Lasserre, Bruno
Marchetti, Marco
Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past Decades
title Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past Decades
title_full Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past Decades
title_fullStr Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past Decades
title_full_unstemmed Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past Decades
title_short Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past Decades
title_sort water balance trends along climatic variations in the mediterranean basin over the past decades
topic climate change
water availability
Mediterranean region
mediterranean climate
ecosystems
url https://hdl.handle.net/10568/139692
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