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
Autor*in: |
Vicuña, Sebastian [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2010 |
---|
Schlagwörter: |
---|
Systematik: |
|
---|
Anmerkung: |
© Springer Science+Business Media B.V. 2010 |
---|
Übergeordnetes Werk: |
Enthalten in: Climatic change - Springer Netherlands, 1977, 105(2010), 3-4 vom: 21. Aug., Seite 469-488 |
---|---|
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 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | OLC2062604459 | ||
003 | DE-627 | ||
005 | 20230503024157.0 | ||
007 | tu | ||
008 | 200819s2010 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1007/s10584-010-9888-4 |2 doi | |
035 | |a (DE-627)OLC2062604459 | ||
035 | |a (DE-He213)s10584-010-9888-4-p | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 550 |q VZ |
084 | |a 14 |2 ssgn | ||
084 | |a RA 1000 |q VZ |2 rvk | ||
100 | 1 | |a Vicuña, Sebastian |e verfasserin |4 aut | |
245 | 1 | 0 | |a Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile |
264 | 1 | |c 2010 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
500 | |a © Springer Science+Business Media B.V. 2010 | ||
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. | ||
650 | 4 | |a Streamflow | |
650 | 4 | |a Snow Water Equivalent | |
650 | 4 | |a Annual Streamflow | |
650 | 4 | |a Water Resource Model | |
650 | 4 | |a Streamflow Reduction | |
700 | 1 | |a Garreaud, René D. |4 aut | |
700 | 1 | |a McPhee, James |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Climatic change |d Springer Netherlands, 1977 |g 105(2010), 3-4 vom: 21. Aug., Seite 469-488 |w (DE-627)130479020 |w (DE-600)751086-X |w (DE-576)016068610 |x 0165-0009 |7 nnns |
773 | 1 | 8 | |g volume:105 |g year:2010 |g number:3-4 |g day:21 |g month:08 |g pages:469-488 |
856 | 4 | 1 | |u https://doi.org/10.1007/s10584-010-9888-4 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a SSG-OLC-UMW | ||
912 | |a SSG-OLC-GEO | ||
912 | |a SSG-OLC-IBL | ||
912 | |a SSG-OPC-GGO | ||
912 | |a GBV_ILN_11 | ||
912 | |a GBV_ILN_21 | ||
912 | |a GBV_ILN_22 | ||
912 | |a GBV_ILN_40 | ||
912 | |a GBV_ILN_62 | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_154 | ||
912 | |a GBV_ILN_601 | ||
912 | |a GBV_ILN_2003 | ||
912 | |a GBV_ILN_2006 | ||
912 | |a GBV_ILN_4012 | ||
912 | |a GBV_ILN_4305 | ||
912 | |a GBV_ILN_4325 | ||
936 | r | v | |a RA 1000 |
951 | |a AR | ||
952 | |d 105 |j 2010 |e 3-4 |b 21 |c 08 |h 469-488 |
author_variant |
s v sv r d g rd rdg j m jm |
---|---|
matchkey_str |
article:01650009:2010----::lmtcagipcsnhhdooyfsomldie |
hierarchy_sort_str |
2010 |
publishDate |
2010 |
allfields |
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 |
spelling |
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 |
allfields_unstemmed |
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 |
allfieldsGer |
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 |
allfieldsSound |
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 |
language |
English |
source |
Enthalten in Climatic change 105(2010), 3-4 vom: 21. Aug., Seite 469-488 volume:105 year:2010 number:3-4 day:21 month:08 pages:469-488 |
sourceStr |
Enthalten in Climatic change 105(2010), 3-4 vom: 21. Aug., Seite 469-488 volume:105 year:2010 number:3-4 day:21 month:08 pages:469-488 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Streamflow Snow Water Equivalent Annual Streamflow Water Resource Model Streamflow Reduction |
dewey-raw |
550 |
isfreeaccess_bool |
false |
container_title |
Climatic change |
authorswithroles_txt_mv |
Vicuña, Sebastian @@aut@@ Garreaud, René D. @@aut@@ McPhee, James @@aut@@ |
publishDateDaySort_date |
2010-08-21T00:00:00Z |
hierarchy_top_id |
130479020 |
dewey-sort |
3550 |
id |
OLC2062604459 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2062604459</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503024157.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2010 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10584-010-9888-4</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2062604459</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s10584-010-9888-4-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RA 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Vicuña, Sebastian</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2010</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Science+Business Media B.V. 2010</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Streamflow</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Snow Water Equivalent</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Annual Streamflow</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Water Resource Model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Streamflow Reduction</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Garreaud, René D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">McPhee, James</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Climatic change</subfield><subfield code="d">Springer Netherlands, 1977</subfield><subfield code="g">105(2010), 3-4 vom: 21. Aug., Seite 469-488</subfield><subfield code="w">(DE-627)130479020</subfield><subfield code="w">(DE-600)751086-X</subfield><subfield code="w">(DE-576)016068610</subfield><subfield code="x">0165-0009</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:105</subfield><subfield code="g">year:2010</subfield><subfield code="g">number:3-4</subfield><subfield code="g">day:21</subfield><subfield code="g">month:08</subfield><subfield code="g">pages:469-488</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s10584-010-9888-4</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-UMW</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-IBL</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">RA 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">105</subfield><subfield code="j">2010</subfield><subfield code="e">3-4</subfield><subfield code="b">21</subfield><subfield code="c">08</subfield><subfield code="h">469-488</subfield></datafield></record></collection>
|
author |
Vicuña, Sebastian |
spellingShingle |
Vicuña, Sebastian ddc 550 ssgn 14 rvk RA 1000 misc Streamflow misc Snow Water Equivalent misc Annual Streamflow misc Water Resource Model misc Streamflow Reduction Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile |
authorStr |
Vicuña, Sebastian |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)130479020 |
format |
Article |
dewey-ones |
550 - Earth sciences |
delete_txt_mv |
keep |
author_role |
aut aut aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
0165-0009 |
topic_title |
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 |
topic |
ddc 550 ssgn 14 rvk RA 1000 misc Streamflow misc Snow Water Equivalent misc Annual Streamflow misc Water Resource Model misc Streamflow Reduction |
topic_unstemmed |
ddc 550 ssgn 14 rvk RA 1000 misc Streamflow misc Snow Water Equivalent misc Annual Streamflow misc Water Resource Model misc Streamflow Reduction |
topic_browse |
ddc 550 ssgn 14 rvk RA 1000 misc Streamflow misc Snow Water Equivalent misc Annual Streamflow misc Water Resource Model misc Streamflow Reduction |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
hierarchy_parent_title |
Climatic change |
hierarchy_parent_id |
130479020 |
dewey-tens |
550 - Earth sciences & geology |
hierarchy_top_title |
Climatic change |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)130479020 (DE-600)751086-X (DE-576)016068610 |
title |
Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile |
ctrlnum |
(DE-627)OLC2062604459 (DE-He213)s10584-010-9888-4-p |
title_full |
Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile |
author_sort |
Vicuña, Sebastian |
journal |
Climatic change |
journalStr |
Climatic change |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science |
recordtype |
marc |
publishDateSort |
2010 |
contenttype_str_mv |
txt |
container_start_page |
469 |
author_browse |
Vicuña, Sebastian Garreaud, René D. McPhee, James |
container_volume |
105 |
class |
550 VZ 14 ssgn RA 1000 VZ rvk |
format_se |
Aufsätze |
author-letter |
Vicuña, Sebastian |
doi_str_mv |
10.1007/s10584-010-9888-4 |
dewey-full |
550 |
title_sort |
climate change impacts on the hydrology of a snowmelt driven basin in semiarid chile |
title_auth |
Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile |
abstract |
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 |
collection_details |
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 |
container_issue |
3-4 |
title_short |
Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile |
url |
https://doi.org/10.1007/s10584-010-9888-4 |
remote_bool |
false |
author2 |
Garreaud, René D. McPhee, James |
author2Str |
Garreaud, René D. McPhee, James |
ppnlink |
130479020 |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/s10584-010-9888-4 |
up_date |
2024-07-03T15:43:47.063Z |
_version_ |
1803573187906109440 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2062604459</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230503024157.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2010 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10584-010-9888-4</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2062604459</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s10584-010-9888-4-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RA 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Vicuña, Sebastian</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Climate change impacts on the hydrology of a snowmelt driven basin in semiarid Chile</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2010</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer Science+Business Media B.V. 2010</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Streamflow</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Snow Water Equivalent</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Annual Streamflow</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Water Resource Model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Streamflow Reduction</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Garreaud, René D.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">McPhee, James</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Climatic change</subfield><subfield code="d">Springer Netherlands, 1977</subfield><subfield code="g">105(2010), 3-4 vom: 21. Aug., Seite 469-488</subfield><subfield code="w">(DE-627)130479020</subfield><subfield code="w">(DE-600)751086-X</subfield><subfield code="w">(DE-576)016068610</subfield><subfield code="x">0165-0009</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:105</subfield><subfield code="g">year:2010</subfield><subfield code="g">number:3-4</subfield><subfield code="g">day:21</subfield><subfield code="g">month:08</subfield><subfield code="g">pages:469-488</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s10584-010-9888-4</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-UMW</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-IBL</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_154</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_601</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">RA 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">105</subfield><subfield code="j">2010</subfield><subfield code="e">3-4</subfield><subfield code="b">21</subfield><subfield code="c">08</subfield><subfield code="h">469-488</subfield></datafield></record></collection>
|
score |
7.397897 |