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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MDPI AG
2023-05-01
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Online Access: | https://www.mdpi.com/2073-4441/15/10/1889 |
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author | Zaib Unnisa Ajit Govind Bruno Lasserre Marco Marchetti |
author_facet | Zaib Unnisa Ajit Govind Bruno Lasserre Marco Marchetti |
author_sort | Zaib Unnisa |
collection | DOAJ |
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<sup>−1</sup>), and even then, they were in a water deficit state (−0.42 mm yr<sup>−1</sup>). 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<sup>−1</sup>) compared to that of northern parts of the MB, and the average Actual Evapotranspiration (AET) was ≈15 mm yr<sup>−1</sup>. 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<sup>−1</sup>, the annual average AET was ≈415 mm yr<sup>−1</sup>, and the runoff (Q) was equivalent to 123 mm yr<sup>−1</sup>, 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 | doaj.art-0cf9f01921d74b3baa32490d939d85e32023-11-18T03:41:55ZengMDPI AGWater2073-44412023-05-011510188910.3390/w15101889Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past DecadesZaib Unnisa0Ajit Govind1Bruno Lasserre2Marco Marchetti3Department for Innovation in Biological, Agri-Food and Forest Systems (DIBAF), University of Tuscia, 01100 Viterbo, ItalyInternational Center for Agricultural Research in Dry Areas (ICARDA), Cairo 11435, EgyptDepartment of Biosciences and Territory, University of Molise, 86090 Pesche, ItalyDepartment of Biosciences and Territory, University of Molise, 86090 Pesche, ItalyThe 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<sup>−1</sup>), and even then, they were in a water deficit state (−0.42 mm yr<sup>−1</sup>). 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<sup>−1</sup>) compared to that of northern parts of the MB, and the average Actual Evapotranspiration (AET) was ≈15 mm yr<sup>−1</sup>. 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<sup>−1</sup>, the annual average AET was ≈415 mm yr<sup>−1</sup>, and the runoff (Q) was equivalent to 123 mm yr<sup>−1</sup>, 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.https://www.mdpi.com/2073-4441/15/10/1889Mediterranean basinclimate fluctuationswater deficitMediterranean ecosystemsBudyko curve |
spellingShingle | Zaib Unnisa Ajit Govind Bruno Lasserre Marco Marchetti Water Balance Trends along Climatic Variations in the Mediterranean Basin over the Past Decades Water Mediterranean basin climate fluctuations water deficit Mediterranean ecosystems Budyko curve |
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 | Mediterranean basin climate fluctuations water deficit Mediterranean ecosystems Budyko curve |
url | https://www.mdpi.com/2073-4441/15/10/1889 |
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