Hydrological Processes in Eucalypt and Pine Forested Headwater Catchments within Mediterranean Region

Mediterranean headwater catchments have experienced major land-use changes in recent centuries, namely characterized by afforestation with fast-growing tree species (e.g., pine and eucalyptus). This paper investigates differences in the hydrological response of two forested catchments with distinct...

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Main Authors: Anne-Karine Boulet, Mitas E. Rial-Rivas, Carla Ferreira, Celeste O. A. Coelho, Zahra Kalantari, Jan Jacob Keizer, António J. D. Ferreira
Format: Article
Language:English
Published: MDPI AG 2021-05-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/10/1418
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spelling doaj-8188d5e0099e4cc889638073d2e267f02021-06-01T00:31:26ZengMDPI AGWater2073-44412021-05-01131418141810.3390/w13101418Hydrological Processes in Eucalypt and Pine Forested Headwater Catchments within Mediterranean RegionAnne-Karine Boulet0Mitas E. Rial-Rivas1Carla Ferreira2Celeste O. A. Coelho3Zahra Kalantari4Jan Jacob Keizer5António J. D. Ferreira6CERNAS, Coimbra Agrarian Technical School, PC 3045-601 Coimbra, PortugalCESAM—Environment and Planning Department, Campus Universitário de Santiago, University of Aveiro, PC 3810-193 Aveiro, PortugalCERNAS, Coimbra Agrarian Technical School, PC 3045-601 Coimbra, PortugalCESAM—Environment and Planning Department, Campus Universitário de Santiago, University of Aveiro, PC 3810-193 Aveiro, PortugalDepartment of Physical Geography, Stockholm University and Bolin Centre for Climate Research, SE-10691 Stockholm, SwedenCESAM—Environment and Planning Department, Campus Universitário de Santiago, University of Aveiro, PC 3810-193 Aveiro, PortugalCERNAS, Coimbra Agrarian Technical School, PC 3045-601 Coimbra, PortugalMediterranean headwater catchments have experienced major land-use changes in recent centuries, namely characterized by afforestation with fast-growing tree species (e.g., pine and eucalyptus). This paper investigates differences in the hydrological response of two forested catchments with distinct <i>Pinus pinaster</i> Aiton (PIN) and <i>Eucalyptus globulus</i> Labill. (EUC) covers over 6 hydrological years, from 2010 to 2016. The study was developed in paired catchments located in North–Central Portugal, under wet Mediterranean climate and schist bedrock. Based on rainfall and streamflow measurements, the hydrological responses were analyzed through the water-balance calculations, rainfall-runoff event analyses, and correlations between rainfall characteristics, evapotranspiration, soil moisture, overland flow, and land-cover parameters. The study period recorded a wide range of annual rainfall, between 984 and 2127 mm per years. The annual streamflow displayed greater inter-annual variation, from 208 to 1430 mm for PIN and from 217 to 1291 mm for EUC. The runoff coefficient was higher in the wettest years, with a maximum of 58% for PIN and 61% for EUC, and decreased substantially in the driest year, representing only 17% of the rainfall in PIN and 22% in EUC. Rainfall was predominant during the winter season (41%), followed by autumn (30%) and spring (24%). The streamflow displayed a seasonal behavior in both catchments, with higher runoff coefficient for EUC that for PIN. Half of the annual streamflow occurs during the winter, with the highest average runoff coefficient attained for EUC and PIN respectively being 68% and 64% of the rainfall amount. Annual evapotranspiration was relatively constant through the six years of study and showed higher average values in PIN (907 mm) than EUC (739 mm), highlighting the importance of forest type and showing that mature pine plantations lead to higher water consumption than eucalypt stands. Annual rainfall amount affects evapotranspiration rate (%), the percentage of ET increasing from 37% to 78% for PIN and from 34% to 73% for EUC between the wettest and the driest years, which raises concerns regarding the impact of climate changes on water availability in the mountain areas of the Mediterranean region.https://www.mdpi.com/2073-4441/13/10/1418afforestationhydrological processespaired catchments<i>Pinus pinaster</i> Aiton<i>Eucalyptus globulus</i> Labill.schist
collection DOAJ
language English
format Article
sources DOAJ
author Anne-Karine Boulet
Mitas E. Rial-Rivas
Carla Ferreira
Celeste O. A. Coelho
Zahra Kalantari
Jan Jacob Keizer
António J. D. Ferreira
spellingShingle Anne-Karine Boulet
Mitas E. Rial-Rivas
Carla Ferreira
Celeste O. A. Coelho
Zahra Kalantari
Jan Jacob Keizer
António J. D. Ferreira
Hydrological Processes in Eucalypt and Pine Forested Headwater Catchments within Mediterranean Region
Water
afforestation
hydrological processes
paired catchments
<i>Pinus pinaster</i> Aiton
<i>Eucalyptus globulus</i> Labill.
schist
author_facet Anne-Karine Boulet
Mitas E. Rial-Rivas
Carla Ferreira
Celeste O. A. Coelho
Zahra Kalantari
Jan Jacob Keizer
António J. D. Ferreira
author_sort Anne-Karine Boulet
title Hydrological Processes in Eucalypt and Pine Forested Headwater Catchments within Mediterranean Region
title_short Hydrological Processes in Eucalypt and Pine Forested Headwater Catchments within Mediterranean Region
title_full Hydrological Processes in Eucalypt and Pine Forested Headwater Catchments within Mediterranean Region
title_fullStr Hydrological Processes in Eucalypt and Pine Forested Headwater Catchments within Mediterranean Region
title_full_unstemmed Hydrological Processes in Eucalypt and Pine Forested Headwater Catchments within Mediterranean Region
title_sort hydrological processes in eucalypt and pine forested headwater catchments within mediterranean region
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2021-05-01
description Mediterranean headwater catchments have experienced major land-use changes in recent centuries, namely characterized by afforestation with fast-growing tree species (e.g., pine and eucalyptus). This paper investigates differences in the hydrological response of two forested catchments with distinct <i>Pinus pinaster</i> Aiton (PIN) and <i>Eucalyptus globulus</i> Labill. (EUC) covers over 6 hydrological years, from 2010 to 2016. The study was developed in paired catchments located in North–Central Portugal, under wet Mediterranean climate and schist bedrock. Based on rainfall and streamflow measurements, the hydrological responses were analyzed through the water-balance calculations, rainfall-runoff event analyses, and correlations between rainfall characteristics, evapotranspiration, soil moisture, overland flow, and land-cover parameters. The study period recorded a wide range of annual rainfall, between 984 and 2127 mm per years. The annual streamflow displayed greater inter-annual variation, from 208 to 1430 mm for PIN and from 217 to 1291 mm for EUC. The runoff coefficient was higher in the wettest years, with a maximum of 58% for PIN and 61% for EUC, and decreased substantially in the driest year, representing only 17% of the rainfall in PIN and 22% in EUC. Rainfall was predominant during the winter season (41%), followed by autumn (30%) and spring (24%). The streamflow displayed a seasonal behavior in both catchments, with higher runoff coefficient for EUC that for PIN. Half of the annual streamflow occurs during the winter, with the highest average runoff coefficient attained for EUC and PIN respectively being 68% and 64% of the rainfall amount. Annual evapotranspiration was relatively constant through the six years of study and showed higher average values in PIN (907 mm) than EUC (739 mm), highlighting the importance of forest type and showing that mature pine plantations lead to higher water consumption than eucalypt stands. Annual rainfall amount affects evapotranspiration rate (%), the percentage of ET increasing from 37% to 78% for PIN and from 34% to 73% for EUC between the wettest and the driest years, which raises concerns regarding the impact of climate changes on water availability in the mountain areas of the Mediterranean region.
topic afforestation
hydrological processes
paired catchments
<i>Pinus pinaster</i> Aiton
<i>Eucalyptus globulus</i> Labill.
schist
url https://www.mdpi.com/2073-4441/13/10/1418
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