Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile
Abstract In this paper we present an analysis of the direct impacts of climate change on the hydrology of the upper watersheds (range in elevation from 1,000 to 5,500 m above sea level) of the snowmelt-driven Limarí river basin, located in north-central Chile (30° S, 70° W). A climate-driven hydrolo...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Vicuña, Sebastian [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2010 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer Science+Business Media B.V. 2010 |
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| Übergeordnetes Werk: |
Enthalten in: Climatic change - Springer Netherlands, 1977, 105(2010), 3-4 vom: 21. Aug., Seite 469-488 |
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| Übergeordnetes Werk: |
volume:105 ; year:2010 ; number:3-4 ; day:21 ; month:08 ; pages:469-488 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10584-010-9888-4 |
|---|
| Katalog-ID: |
OLC2062604459 |
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| 520 | |a Abstract In this paper we present an analysis of the direct impacts of climate change on the hydrology of the upper watersheds (range in elevation from 1,000 to 5,500 m above sea level) of the snowmelt-driven Limarí river basin, located in north-central Chile (30° S, 70° W). A climate-driven hydrology and water resources model was calibrated using meteorological and streamflow observations and later forced by a baseline and two climate change projections (A2, B2) that show an increase in temperature of about 3–4°C and a reduction in precipitation of 10–30% with respect to baseline. The results show that annual mean streamflow decreases more than the projected rainfall decrease because a warmer climate also enhances water losses to evapotranspiration. Also in future climate, the seasonal maximum streamflow tends to occur earlier than in current conditions, because of the increase in temperature during spring/summer and the lower snow accumulation in winter. | ||
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10.1007/s10584-010-9888-4 doi (DE-627)OLC2062604459 (DE-He213)s10584-010-9888-4-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Vicuña, Sebastian verfasserin aut Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2010 Abstract In this paper we present an analysis of the direct impacts of climate change on the hydrology of the upper watersheds (range in elevation from 1,000 to 5,500 m above sea level) of the snowmelt-driven Limarí river basin, located in north-central Chile (30° S, 70° W). A climate-driven hydrology and water resources model was calibrated using meteorological and streamflow observations and later forced by a baseline and two climate change projections (A2, B2) that show an increase in temperature of about 3–4°C and a reduction in precipitation of 10–30% with respect to baseline. The results show that annual mean streamflow decreases more than the projected rainfall decrease because a warmer climate also enhances water losses to evapotranspiration. Also in future climate, the seasonal maximum streamflow tends to occur earlier than in current conditions, because of the increase in temperature during spring/summer and the lower snow accumulation in winter. Streamflow Snow Water Equivalent Annual Streamflow Water Resource Model Streamflow Reduction Garreaud, René D. aut McPhee, James aut Enthalten in Climatic change Springer Netherlands, 1977 105(2010), 3-4 vom: 21. Aug., Seite 469-488 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:105 year:2010 number:3-4 day:21 month:08 pages:469-488 https://doi.org/10.1007/s10584-010-9888-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4325 RA 1000 AR 105 2010 3-4 21 08 469-488 |
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10.1007/s10584-010-9888-4 doi (DE-627)OLC2062604459 (DE-He213)s10584-010-9888-4-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Vicuña, Sebastian verfasserin aut Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2010 Abstract In this paper we present an analysis of the direct impacts of climate change on the hydrology of the upper watersheds (range in elevation from 1,000 to 5,500 m above sea level) of the snowmelt-driven Limarí river basin, located in north-central Chile (30° S, 70° W). A climate-driven hydrology and water resources model was calibrated using meteorological and streamflow observations and later forced by a baseline and two climate change projections (A2, B2) that show an increase in temperature of about 3–4°C and a reduction in precipitation of 10–30% with respect to baseline. The results show that annual mean streamflow decreases more than the projected rainfall decrease because a warmer climate also enhances water losses to evapotranspiration. Also in future climate, the seasonal maximum streamflow tends to occur earlier than in current conditions, because of the increase in temperature during spring/summer and the lower snow accumulation in winter. Streamflow Snow Water Equivalent Annual Streamflow Water Resource Model Streamflow Reduction Garreaud, René D. aut McPhee, James aut Enthalten in Climatic change Springer Netherlands, 1977 105(2010), 3-4 vom: 21. Aug., Seite 469-488 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:105 year:2010 number:3-4 day:21 month:08 pages:469-488 https://doi.org/10.1007/s10584-010-9888-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4325 RA 1000 AR 105 2010 3-4 21 08 469-488 |
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10.1007/s10584-010-9888-4 doi (DE-627)OLC2062604459 (DE-He213)s10584-010-9888-4-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Vicuña, Sebastian verfasserin aut Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2010 Abstract In this paper we present an analysis of the direct impacts of climate change on the hydrology of the upper watersheds (range in elevation from 1,000 to 5,500 m above sea level) of the snowmelt-driven Limarí river basin, located in north-central Chile (30° S, 70° W). A climate-driven hydrology and water resources model was calibrated using meteorological and streamflow observations and later forced by a baseline and two climate change projections (A2, B2) that show an increase in temperature of about 3–4°C and a reduction in precipitation of 10–30% with respect to baseline. The results show that annual mean streamflow decreases more than the projected rainfall decrease because a warmer climate also enhances water losses to evapotranspiration. Also in future climate, the seasonal maximum streamflow tends to occur earlier than in current conditions, because of the increase in temperature during spring/summer and the lower snow accumulation in winter. Streamflow Snow Water Equivalent Annual Streamflow Water Resource Model Streamflow Reduction Garreaud, René D. aut McPhee, James aut Enthalten in Climatic change Springer Netherlands, 1977 105(2010), 3-4 vom: 21. Aug., Seite 469-488 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:105 year:2010 number:3-4 day:21 month:08 pages:469-488 https://doi.org/10.1007/s10584-010-9888-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4325 RA 1000 AR 105 2010 3-4 21 08 469-488 |
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10.1007/s10584-010-9888-4 doi (DE-627)OLC2062604459 (DE-He213)s10584-010-9888-4-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Vicuña, Sebastian verfasserin aut Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science+Business Media B.V. 2010 Abstract In this paper we present an analysis of the direct impacts of climate change on the hydrology of the upper watersheds (range in elevation from 1,000 to 5,500 m above sea level) of the snowmelt-driven Limarí river basin, located in north-central Chile (30° S, 70° W). A climate-driven hydrology and water resources model was calibrated using meteorological and streamflow observations and later forced by a baseline and two climate change projections (A2, B2) that show an increase in temperature of about 3–4°C and a reduction in precipitation of 10–30% with respect to baseline. The results show that annual mean streamflow decreases more than the projected rainfall decrease because a warmer climate also enhances water losses to evapotranspiration. Also in future climate, the seasonal maximum streamflow tends to occur earlier than in current conditions, because of the increase in temperature during spring/summer and the lower snow accumulation in winter. Streamflow Snow Water Equivalent Annual Streamflow Water Resource Model Streamflow Reduction Garreaud, René D. aut McPhee, James aut Enthalten in Climatic change Springer Netherlands, 1977 105(2010), 3-4 vom: 21. Aug., Seite 469-488 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:105 year:2010 number:3-4 day:21 month:08 pages:469-488 https://doi.org/10.1007/s10584-010-9888-4 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4305 GBV_ILN_4325 RA 1000 AR 105 2010 3-4 21 08 469-488 |
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550 VZ 14 ssgn RA 1000 VZ rvk Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile Streamflow Snow Water Equivalent Annual Streamflow Water Resource Model Streamflow Reduction |
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Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile |
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Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile |
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Vicuña, Sebastian |
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Vicuña, Sebastian Garreaud, René D. McPhee, James |
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climate change impacts on the hydrology of a snowmelt driven basin in semiarid chile |
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Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile |
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Abstract In this paper we present an analysis of the direct impacts of climate change on the hydrology of the upper watersheds (range in elevation from 1,000 to 5,500 m above sea level) of the snowmelt-driven Limarí river basin, located in north-central Chile (30° S, 70° W). A climate-driven hydrology and water resources model was calibrated using meteorological and streamflow observations and later forced by a baseline and two climate change projections (A2, B2) that show an increase in temperature of about 3–4°C and a reduction in precipitation of 10–30% with respect to baseline. The results show that annual mean streamflow decreases more than the projected rainfall decrease because a warmer climate also enhances water losses to evapotranspiration. Also in future climate, the seasonal maximum streamflow tends to occur earlier than in current conditions, because of the increase in temperature during spring/summer and the lower snow accumulation in winter. © Springer Science+Business Media B.V. 2010 |
| abstractGer |
Abstract In this paper we present an analysis of the direct impacts of climate change on the hydrology of the upper watersheds (range in elevation from 1,000 to 5,500 m above sea level) of the snowmelt-driven Limarí river basin, located in north-central Chile (30° S, 70° W). A climate-driven hydrology and water resources model was calibrated using meteorological and streamflow observations and later forced by a baseline and two climate change projections (A2, B2) that show an increase in temperature of about 3–4°C and a reduction in precipitation of 10–30% with respect to baseline. The results show that annual mean streamflow decreases more than the projected rainfall decrease because a warmer climate also enhances water losses to evapotranspiration. Also in future climate, the seasonal maximum streamflow tends to occur earlier than in current conditions, because of the increase in temperature during spring/summer and the lower snow accumulation in winter. © Springer Science+Business Media B.V. 2010 |
| abstract_unstemmed |
Abstract In this paper we present an analysis of the direct impacts of climate change on the hydrology of the upper watersheds (range in elevation from 1,000 to 5,500 m above sea level) of the snowmelt-driven Limarí river basin, located in north-central Chile (30° S, 70° W). A climate-driven hydrology and water resources model was calibrated using meteorological and streamflow observations and later forced by a baseline and two climate change projections (A2, B2) that show an increase in temperature of about 3–4°C and a reduction in precipitation of 10–30% with respect to baseline. The results show that annual mean streamflow decreases more than the projected rainfall decrease because a warmer climate also enhances water losses to evapotranspiration. Also in future climate, the seasonal maximum streamflow tends to occur earlier than in current conditions, because of the increase in temperature during spring/summer and the lower snow accumulation in winter. © Springer Science+Business Media B.V. 2010 |
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Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile |
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