Drivers influencing streamflow changes in the Upper Turia basin, Spain
Many rivers across the world have experienced a significant streamflow reduction over the last decades. Drivers of the observed streamflow changes are multiple, including climate change (CC), land use and land cover changes (LULCC), water transfers and river impoundment. Many of these drivers inter-...
Ausführliche Beschreibung
Autor*in: |
Salmoral, Gloria [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2015 |
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Rechteinformationen: |
Nutzungsrecht: Copyright © 2014 Elsevier B.V. All rights reserved. |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: The science of the total environment - Amsterdam : Elsevier, 1972, 503-504(2015), Seite 258-268 |
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Übergeordnetes Werk: |
volume:503-504 ; year:2015 ; pages:258-268 |
Links: |
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DOI / URN: |
10.1016/j.scitotenv.2014.07.041 |
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Katalog-ID: |
OLC196743137X |
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520 | |a Many rivers across the world have experienced a significant streamflow reduction over the last decades. Drivers of the observed streamflow changes are multiple, including climate change (CC), land use and land cover changes (LULCC), water transfers and river impoundment. Many of these drivers inter-act simultaneously, making it difficult to discern the impact of each driver individually. In this study we isolate the effects of LULCC on the observed streamflow reduction in the Upper Turia basin (east Spain) during the period 1973-2008. Regression models of annual streamflow are fitted with climatic variables and also additional time variant drivers like LULCC. The ecohydrological model SWAT is used to study the magnitude and sign of streamflow change when LULCC occurs. Our results show that LULCC does play a significant role on the water balance, but it is not the main driver underpinning the observed reduction on Turia's streamflow. Increasing mean temperature is the main factor supporting increasing evapotranspiration and streamflow reduction. In fact, LULCC and CC have had an offsetting effect on the streamflow generation during the study period. While streamflow has been negatively affected by increasing temperature, ongoing LULCC have positively compensated with reduced evapotranspiration rates, thanks to mainly shrubland clearing and forest degradation processes. These findings are valuable for the management of the Turia river basin, as well as a useful approach for the determination of the weight of LULCC on the hydrological response in other regions. | ||
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10.1016/j.scitotenv.2014.07.041 doi PQ20160617 (DE-627)OLC196743137X (DE-599)GBVOLC196743137X (PRQ)c2066-78e7242cf1e5436d977a40c1b66af11ee87a12f9696dd6f980823cbf790b4ebf0 (KEY)0073664320150000503000000258driversinfluencingstreamflowchangesintheupperturia DE-627 ger DE-627 rakwb eng 570 333.7 610 DNB Salmoral, Gloria verfasserin aut Drivers influencing streamflow changes in the Upper Turia basin, Spain 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Many rivers across the world have experienced a significant streamflow reduction over the last decades. Drivers of the observed streamflow changes are multiple, including climate change (CC), land use and land cover changes (LULCC), water transfers and river impoundment. Many of these drivers inter-act simultaneously, making it difficult to discern the impact of each driver individually. In this study we isolate the effects of LULCC on the observed streamflow reduction in the Upper Turia basin (east Spain) during the period 1973-2008. Regression models of annual streamflow are fitted with climatic variables and also additional time variant drivers like LULCC. The ecohydrological model SWAT is used to study the magnitude and sign of streamflow change when LULCC occurs. Our results show that LULCC does play a significant role on the water balance, but it is not the main driver underpinning the observed reduction on Turia's streamflow. Increasing mean temperature is the main factor supporting increasing evapotranspiration and streamflow reduction. In fact, LULCC and CC have had an offsetting effect on the streamflow generation during the study period. While streamflow has been negatively affected by increasing temperature, ongoing LULCC have positively compensated with reduced evapotranspiration rates, thanks to mainly shrubland clearing and forest degradation processes. These findings are valuable for the management of the Turia river basin, as well as a useful approach for the determination of the weight of LULCC on the hydrological response in other regions. Nutzungsrecht: Copyright © 2014 Elsevier B.V. All rights reserved. Rivers - chemistry Willaarts, Bárbara A oth Troch, Peter A oth Garrido, Alberto oth Enthalten in The science of the total environment Amsterdam : Elsevier, 1972 503-504(2015), Seite 258-268 (DE-627)129297917 (DE-600)121506-1 (DE-576)014490919 0048-9697 nnns volume:503-504 year:2015 pages:258-268 http://dx.doi.org/10.1016/j.scitotenv.2014.07.041 Volltext http://www.ncbi.nlm.nih.gov/pubmed/25115604 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_4012 AR 503-504 2015 258-268 |
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10.1016/j.scitotenv.2014.07.041 doi PQ20160617 (DE-627)OLC196743137X (DE-599)GBVOLC196743137X (PRQ)c2066-78e7242cf1e5436d977a40c1b66af11ee87a12f9696dd6f980823cbf790b4ebf0 (KEY)0073664320150000503000000258driversinfluencingstreamflowchangesintheupperturia DE-627 ger DE-627 rakwb eng 570 333.7 610 DNB Salmoral, Gloria verfasserin aut Drivers influencing streamflow changes in the Upper Turia basin, Spain 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Many rivers across the world have experienced a significant streamflow reduction over the last decades. Drivers of the observed streamflow changes are multiple, including climate change (CC), land use and land cover changes (LULCC), water transfers and river impoundment. Many of these drivers inter-act simultaneously, making it difficult to discern the impact of each driver individually. In this study we isolate the effects of LULCC on the observed streamflow reduction in the Upper Turia basin (east Spain) during the period 1973-2008. Regression models of annual streamflow are fitted with climatic variables and also additional time variant drivers like LULCC. The ecohydrological model SWAT is used to study the magnitude and sign of streamflow change when LULCC occurs. Our results show that LULCC does play a significant role on the water balance, but it is not the main driver underpinning the observed reduction on Turia's streamflow. Increasing mean temperature is the main factor supporting increasing evapotranspiration and streamflow reduction. In fact, LULCC and CC have had an offsetting effect on the streamflow generation during the study period. While streamflow has been negatively affected by increasing temperature, ongoing LULCC have positively compensated with reduced evapotranspiration rates, thanks to mainly shrubland clearing and forest degradation processes. These findings are valuable for the management of the Turia river basin, as well as a useful approach for the determination of the weight of LULCC on the hydrological response in other regions. Nutzungsrecht: Copyright © 2014 Elsevier B.V. All rights reserved. Rivers - chemistry Willaarts, Bárbara A oth Troch, Peter A oth Garrido, Alberto oth Enthalten in The science of the total environment Amsterdam : Elsevier, 1972 503-504(2015), Seite 258-268 (DE-627)129297917 (DE-600)121506-1 (DE-576)014490919 0048-9697 nnns volume:503-504 year:2015 pages:258-268 http://dx.doi.org/10.1016/j.scitotenv.2014.07.041 Volltext http://www.ncbi.nlm.nih.gov/pubmed/25115604 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_4012 AR 503-504 2015 258-268 |
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10.1016/j.scitotenv.2014.07.041 doi PQ20160617 (DE-627)OLC196743137X (DE-599)GBVOLC196743137X (PRQ)c2066-78e7242cf1e5436d977a40c1b66af11ee87a12f9696dd6f980823cbf790b4ebf0 (KEY)0073664320150000503000000258driversinfluencingstreamflowchangesintheupperturia DE-627 ger DE-627 rakwb eng 570 333.7 610 DNB Salmoral, Gloria verfasserin aut Drivers influencing streamflow changes in the Upper Turia basin, Spain 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Many rivers across the world have experienced a significant streamflow reduction over the last decades. Drivers of the observed streamflow changes are multiple, including climate change (CC), land use and land cover changes (LULCC), water transfers and river impoundment. Many of these drivers inter-act simultaneously, making it difficult to discern the impact of each driver individually. In this study we isolate the effects of LULCC on the observed streamflow reduction in the Upper Turia basin (east Spain) during the period 1973-2008. Regression models of annual streamflow are fitted with climatic variables and also additional time variant drivers like LULCC. The ecohydrological model SWAT is used to study the magnitude and sign of streamflow change when LULCC occurs. Our results show that LULCC does play a significant role on the water balance, but it is not the main driver underpinning the observed reduction on Turia's streamflow. Increasing mean temperature is the main factor supporting increasing evapotranspiration and streamflow reduction. In fact, LULCC and CC have had an offsetting effect on the streamflow generation during the study period. While streamflow has been negatively affected by increasing temperature, ongoing LULCC have positively compensated with reduced evapotranspiration rates, thanks to mainly shrubland clearing and forest degradation processes. These findings are valuable for the management of the Turia river basin, as well as a useful approach for the determination of the weight of LULCC on the hydrological response in other regions. Nutzungsrecht: Copyright © 2014 Elsevier B.V. All rights reserved. Rivers - chemistry Willaarts, Bárbara A oth Troch, Peter A oth Garrido, Alberto oth Enthalten in The science of the total environment Amsterdam : Elsevier, 1972 503-504(2015), Seite 258-268 (DE-627)129297917 (DE-600)121506-1 (DE-576)014490919 0048-9697 nnns volume:503-504 year:2015 pages:258-268 http://dx.doi.org/10.1016/j.scitotenv.2014.07.041 Volltext http://www.ncbi.nlm.nih.gov/pubmed/25115604 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_4012 AR 503-504 2015 258-268 |
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10.1016/j.scitotenv.2014.07.041 doi PQ20160617 (DE-627)OLC196743137X (DE-599)GBVOLC196743137X (PRQ)c2066-78e7242cf1e5436d977a40c1b66af11ee87a12f9696dd6f980823cbf790b4ebf0 (KEY)0073664320150000503000000258driversinfluencingstreamflowchangesintheupperturia DE-627 ger DE-627 rakwb eng 570 333.7 610 DNB Salmoral, Gloria verfasserin aut Drivers influencing streamflow changes in the Upper Turia basin, Spain 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Many rivers across the world have experienced a significant streamflow reduction over the last decades. Drivers of the observed streamflow changes are multiple, including climate change (CC), land use and land cover changes (LULCC), water transfers and river impoundment. Many of these drivers inter-act simultaneously, making it difficult to discern the impact of each driver individually. In this study we isolate the effects of LULCC on the observed streamflow reduction in the Upper Turia basin (east Spain) during the period 1973-2008. Regression models of annual streamflow are fitted with climatic variables and also additional time variant drivers like LULCC. The ecohydrological model SWAT is used to study the magnitude and sign of streamflow change when LULCC occurs. Our results show that LULCC does play a significant role on the water balance, but it is not the main driver underpinning the observed reduction on Turia's streamflow. Increasing mean temperature is the main factor supporting increasing evapotranspiration and streamflow reduction. In fact, LULCC and CC have had an offsetting effect on the streamflow generation during the study period. While streamflow has been negatively affected by increasing temperature, ongoing LULCC have positively compensated with reduced evapotranspiration rates, thanks to mainly shrubland clearing and forest degradation processes. These findings are valuable for the management of the Turia river basin, as well as a useful approach for the determination of the weight of LULCC on the hydrological response in other regions. Nutzungsrecht: Copyright © 2014 Elsevier B.V. All rights reserved. Rivers - chemistry Willaarts, Bárbara A oth Troch, Peter A oth Garrido, Alberto oth Enthalten in The science of the total environment Amsterdam : Elsevier, 1972 503-504(2015), Seite 258-268 (DE-627)129297917 (DE-600)121506-1 (DE-576)014490919 0048-9697 nnns volume:503-504 year:2015 pages:258-268 http://dx.doi.org/10.1016/j.scitotenv.2014.07.041 Volltext http://www.ncbi.nlm.nih.gov/pubmed/25115604 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_4012 AR 503-504 2015 258-268 |
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10.1016/j.scitotenv.2014.07.041 doi PQ20160617 (DE-627)OLC196743137X (DE-599)GBVOLC196743137X (PRQ)c2066-78e7242cf1e5436d977a40c1b66af11ee87a12f9696dd6f980823cbf790b4ebf0 (KEY)0073664320150000503000000258driversinfluencingstreamflowchangesintheupperturia DE-627 ger DE-627 rakwb eng 570 333.7 610 DNB Salmoral, Gloria verfasserin aut Drivers influencing streamflow changes in the Upper Turia basin, Spain 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Many rivers across the world have experienced a significant streamflow reduction over the last decades. Drivers of the observed streamflow changes are multiple, including climate change (CC), land use and land cover changes (LULCC), water transfers and river impoundment. Many of these drivers inter-act simultaneously, making it difficult to discern the impact of each driver individually. In this study we isolate the effects of LULCC on the observed streamflow reduction in the Upper Turia basin (east Spain) during the period 1973-2008. Regression models of annual streamflow are fitted with climatic variables and also additional time variant drivers like LULCC. The ecohydrological model SWAT is used to study the magnitude and sign of streamflow change when LULCC occurs. Our results show that LULCC does play a significant role on the water balance, but it is not the main driver underpinning the observed reduction on Turia's streamflow. Increasing mean temperature is the main factor supporting increasing evapotranspiration and streamflow reduction. In fact, LULCC and CC have had an offsetting effect on the streamflow generation during the study period. While streamflow has been negatively affected by increasing temperature, ongoing LULCC have positively compensated with reduced evapotranspiration rates, thanks to mainly shrubland clearing and forest degradation processes. These findings are valuable for the management of the Turia river basin, as well as a useful approach for the determination of the weight of LULCC on the hydrological response in other regions. Nutzungsrecht: Copyright © 2014 Elsevier B.V. All rights reserved. Rivers - chemistry Willaarts, Bárbara A oth Troch, Peter A oth Garrido, Alberto oth Enthalten in The science of the total environment Amsterdam : Elsevier, 1972 503-504(2015), Seite 258-268 (DE-627)129297917 (DE-600)121506-1 (DE-576)014490919 0048-9697 nnns volume:503-504 year:2015 pages:258-268 http://dx.doi.org/10.1016/j.scitotenv.2014.07.041 Volltext http://www.ncbi.nlm.nih.gov/pubmed/25115604 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-FOR SSG-OPC-GGO GBV_ILN_21 GBV_ILN_70 GBV_ILN_4012 AR 503-504 2015 258-268 |
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Drivers influencing streamflow changes in the Upper Turia basin, Spain |
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Drivers influencing streamflow changes in the Upper Turia basin, Spain |
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drivers influencing streamflow changes in the upper turia basin, spain |
title_auth |
Drivers influencing streamflow changes in the Upper Turia basin, Spain |
abstract |
Many rivers across the world have experienced a significant streamflow reduction over the last decades. Drivers of the observed streamflow changes are multiple, including climate change (CC), land use and land cover changes (LULCC), water transfers and river impoundment. Many of these drivers inter-act simultaneously, making it difficult to discern the impact of each driver individually. In this study we isolate the effects of LULCC on the observed streamflow reduction in the Upper Turia basin (east Spain) during the period 1973-2008. Regression models of annual streamflow are fitted with climatic variables and also additional time variant drivers like LULCC. The ecohydrological model SWAT is used to study the magnitude and sign of streamflow change when LULCC occurs. Our results show that LULCC does play a significant role on the water balance, but it is not the main driver underpinning the observed reduction on Turia's streamflow. Increasing mean temperature is the main factor supporting increasing evapotranspiration and streamflow reduction. In fact, LULCC and CC have had an offsetting effect on the streamflow generation during the study period. While streamflow has been negatively affected by increasing temperature, ongoing LULCC have positively compensated with reduced evapotranspiration rates, thanks to mainly shrubland clearing and forest degradation processes. These findings are valuable for the management of the Turia river basin, as well as a useful approach for the determination of the weight of LULCC on the hydrological response in other regions. |
abstractGer |
Many rivers across the world have experienced a significant streamflow reduction over the last decades. Drivers of the observed streamflow changes are multiple, including climate change (CC), land use and land cover changes (LULCC), water transfers and river impoundment. Many of these drivers inter-act simultaneously, making it difficult to discern the impact of each driver individually. In this study we isolate the effects of LULCC on the observed streamflow reduction in the Upper Turia basin (east Spain) during the period 1973-2008. Regression models of annual streamflow are fitted with climatic variables and also additional time variant drivers like LULCC. The ecohydrological model SWAT is used to study the magnitude and sign of streamflow change when LULCC occurs. Our results show that LULCC does play a significant role on the water balance, but it is not the main driver underpinning the observed reduction on Turia's streamflow. Increasing mean temperature is the main factor supporting increasing evapotranspiration and streamflow reduction. In fact, LULCC and CC have had an offsetting effect on the streamflow generation during the study period. While streamflow has been negatively affected by increasing temperature, ongoing LULCC have positively compensated with reduced evapotranspiration rates, thanks to mainly shrubland clearing and forest degradation processes. These findings are valuable for the management of the Turia river basin, as well as a useful approach for the determination of the weight of LULCC on the hydrological response in other regions. |
abstract_unstemmed |
Many rivers across the world have experienced a significant streamflow reduction over the last decades. Drivers of the observed streamflow changes are multiple, including climate change (CC), land use and land cover changes (LULCC), water transfers and river impoundment. Many of these drivers inter-act simultaneously, making it difficult to discern the impact of each driver individually. In this study we isolate the effects of LULCC on the observed streamflow reduction in the Upper Turia basin (east Spain) during the period 1973-2008. Regression models of annual streamflow are fitted with climatic variables and also additional time variant drivers like LULCC. The ecohydrological model SWAT is used to study the magnitude and sign of streamflow change when LULCC occurs. Our results show that LULCC does play a significant role on the water balance, but it is not the main driver underpinning the observed reduction on Turia's streamflow. Increasing mean temperature is the main factor supporting increasing evapotranspiration and streamflow reduction. In fact, LULCC and CC have had an offsetting effect on the streamflow generation during the study period. While streamflow has been negatively affected by increasing temperature, ongoing LULCC have positively compensated with reduced evapotranspiration rates, thanks to mainly shrubland clearing and forest degradation processes. These findings are valuable for the management of the Turia river basin, as well as a useful approach for the determination of the weight of LULCC on the hydrological response in other regions. |
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title_short |
Drivers influencing streamflow changes in the Upper Turia basin, Spain |
url |
http://dx.doi.org/10.1016/j.scitotenv.2014.07.041 http://www.ncbi.nlm.nih.gov/pubmed/25115604 |
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Willaarts, Bárbara A Troch, Peter A Garrido, Alberto |
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