Hydrological Impacts of Climate Change in a Well-preserved Upland Watershed
Much attention has been focused on investigating the effects of climate change on hydrological processes on a regional scale. However, the landscape approach, especially the case of well-preserved upland watersheds needs to be further studied. The Representative Concentration Pathway (RCP) or emissi...
Gespeichert in:
| Veröffentlicht in: | Water resources management 2020-06, Vol.34 (8), p.2255-2267 |
|---|---|
| Hauptverfasser: | , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 2267 |
|---|---|
| container_issue | 8 |
| container_start_page | 2255 |
| container_title | Water resources management |
| container_volume | 34 |
| creator | de Moura, Carolina Natel Neto, Sílvio Luís Rafaeli Campos, Claudia Guimarães Camargo Sá, Eder Alexandre Schatz |
| description | Much attention has been focused on investigating the effects of climate change on hydrological processes on a regional scale. However, the landscape approach, especially the case of well-preserved upland watersheds needs to be further studied. The Representative Concentration Pathway (RCP) or emission scenarios RCP 4.5 and RCP 8.5 were used to project the impacts of the climate change on the hydrological components of a well-preserved upland landscape with temperate climate, using the Upper Canoas watershed as a case study. The future hydrological projection indicated an increase in the monthly rainfall as well as a shift in the rainiest months from winter to spring. This change resulted in an increase in water balance components. The maximum discharges, as well as the modal discharge (Q50), may increase in the future, and the minimums corresponding to Q95 and Q98 may reduce for both emission scenarios. The results showed that a well-preserved upland watershed in a sub-tropical region might be capable of maintaining water availability at level that is enough for human activities in the future, even with the reduction of minimum permit discharge, which is supported by the increase of maximum and medium monthly discharges and a stable flow-duration curve. |
| doi_str_mv | 10.1007/s11269-019-02450-1 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_2414131181</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2414131181</sourcerecordid><originalsourceid>FETCH-LOGICAL-c363t-e3ac5a455ea0ca7ef009d4db1706fd84b5114639af99d72a7c4a9eaaae3699cd3</originalsourceid><addsrcrecordid>eNp9kM1OwzAQhC0EEqXwApwscTZ4YyepjygCWlGJC1WP1tbe9EdpEuwWqW-PIUjcOKz28s3szjB2C_IepCwfIkBWGCEhTaZzKeCMjSAvlYAil-dsJE0mhS41XLKrGHdSJpmRI_Y6PfnQNd1667Dhs32P7hB5V_Oq2e7xQLzaYLsmvm058iU1jegDRQqf5Pmib7D1fJmwEDfkr9lFjU2km989Zovnp_dqKuZvL7PqcS6cKtRBkEKXo85zQumwpDp94rVfQSmL2k_0KgfQhTJYG-PLDEun0RAikiqMcV6N2d3g24fu40jxYHfdMbTppM00aFAAE0hUNlAudDEGqm0fUqRwsiDtd2l2KM2m0uxPafZbpAZRTHDKHf6s_1F9ATdlbys</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2414131181</pqid></control><display><type>article</type><title>Hydrological Impacts of Climate Change in a Well-preserved Upland Watershed</title><source>SpringerLink Journals</source><creator>de Moura, Carolina Natel ; Neto, Sílvio Luís Rafaeli ; Campos, Claudia Guimarães Camargo ; Sá, Eder Alexandre Schatz</creator><creatorcontrib>de Moura, Carolina Natel ; Neto, Sílvio Luís Rafaeli ; Campos, Claudia Guimarães Camargo ; Sá, Eder Alexandre Schatz</creatorcontrib><description>Much attention has been focused on investigating the effects of climate change on hydrological processes on a regional scale. However, the landscape approach, especially the case of well-preserved upland watersheds needs to be further studied. The Representative Concentration Pathway (RCP) or emission scenarios RCP 4.5 and RCP 8.5 were used to project the impacts of the climate change on the hydrological components of a well-preserved upland landscape with temperate climate, using the Upper Canoas watershed as a case study. The future hydrological projection indicated an increase in the monthly rainfall as well as a shift in the rainiest months from winter to spring. This change resulted in an increase in water balance components. The maximum discharges, as well as the modal discharge (Q50), may increase in the future, and the minimums corresponding to Q95 and Q98 may reduce for both emission scenarios. The results showed that a well-preserved upland watershed in a sub-tropical region might be capable of maintaining water availability at level that is enough for human activities in the future, even with the reduction of minimum permit discharge, which is supported by the increase of maximum and medium monthly discharges and a stable flow-duration curve.</description><identifier>ISSN: 0920-4741</identifier><identifier>EISSN: 1573-1650</identifier><identifier>DOI: 10.1007/s11269-019-02450-1</identifier><language>eng</language><publisher>Dordrecht: Springer Netherlands</publisher><subject>Atmospheric Sciences ; Civil Engineering ; Climate change ; Climate effects ; Components ; Discharge ; Earth and Environmental Science ; Earth Sciences ; Emission analysis ; Emissions ; Emissions control ; Environment ; Environmental impact ; Flow duration curves ; Geotechnical Engineering & Applied Earth Sciences ; Hydrogeology ; Hydrology ; Hydrology/Water Resources ; Landscape preservation ; Rain ; Rainfall ; Tropical climate ; Tropical environment ; Tropical environments ; Water availability ; Water balance ; Watersheds</subject><ispartof>Water resources management, 2020-06, Vol.34 (8), p.2255-2267</ispartof><rights>Springer Nature B.V. 2020</rights><rights>Springer Nature B.V. 2020.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c363t-e3ac5a455ea0ca7ef009d4db1706fd84b5114639af99d72a7c4a9eaaae3699cd3</citedby><cites>FETCH-LOGICAL-c363t-e3ac5a455ea0ca7ef009d4db1706fd84b5114639af99d72a7c4a9eaaae3699cd3</cites><orcidid>0000-0002-6640-1961 ; 0000-0003-3103-6789 ; 0000-0001-5010-1895 ; 0000-0002-3419-4865</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s11269-019-02450-1$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s11269-019-02450-1$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>de Moura, Carolina Natel</creatorcontrib><creatorcontrib>Neto, Sílvio Luís Rafaeli</creatorcontrib><creatorcontrib>Campos, Claudia Guimarães Camargo</creatorcontrib><creatorcontrib>Sá, Eder Alexandre Schatz</creatorcontrib><title>Hydrological Impacts of Climate Change in a Well-preserved Upland Watershed</title><title>Water resources management</title><addtitle>Water Resour Manage</addtitle><description>Much attention has been focused on investigating the effects of climate change on hydrological processes on a regional scale. However, the landscape approach, especially the case of well-preserved upland watersheds needs to be further studied. The Representative Concentration Pathway (RCP) or emission scenarios RCP 4.5 and RCP 8.5 were used to project the impacts of the climate change on the hydrological components of a well-preserved upland landscape with temperate climate, using the Upper Canoas watershed as a case study. The future hydrological projection indicated an increase in the monthly rainfall as well as a shift in the rainiest months from winter to spring. This change resulted in an increase in water balance components. The maximum discharges, as well as the modal discharge (Q50), may increase in the future, and the minimums corresponding to Q95 and Q98 may reduce for both emission scenarios. The results showed that a well-preserved upland watershed in a sub-tropical region might be capable of maintaining water availability at level that is enough for human activities in the future, even with the reduction of minimum permit discharge, which is supported by the increase of maximum and medium monthly discharges and a stable flow-duration curve.</description><subject>Atmospheric Sciences</subject><subject>Civil Engineering</subject><subject>Climate change</subject><subject>Climate effects</subject><subject>Components</subject><subject>Discharge</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Emission analysis</subject><subject>Emissions</subject><subject>Emissions control</subject><subject>Environment</subject><subject>Environmental impact</subject><subject>Flow duration curves</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Hydrogeology</subject><subject>Hydrology</subject><subject>Hydrology/Water Resources</subject><subject>Landscape preservation</subject><subject>Rain</subject><subject>Rainfall</subject><subject>Tropical climate</subject><subject>Tropical environment</subject><subject>Tropical environments</subject><subject>Water availability</subject><subject>Water balance</subject><subject>Watersheds</subject><issn>0920-4741</issn><issn>1573-1650</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kM1OwzAQhC0EEqXwApwscTZ4YyepjygCWlGJC1WP1tbe9EdpEuwWqW-PIUjcOKz28s3szjB2C_IepCwfIkBWGCEhTaZzKeCMjSAvlYAil-dsJE0mhS41XLKrGHdSJpmRI_Y6PfnQNd1667Dhs32P7hB5V_Oq2e7xQLzaYLsmvm058iU1jegDRQqf5Pmib7D1fJmwEDfkr9lFjU2km989Zovnp_dqKuZvL7PqcS6cKtRBkEKXo85zQumwpDp94rVfQSmL2k_0KgfQhTJYG-PLDEun0RAikiqMcV6N2d3g24fu40jxYHfdMbTppM00aFAAE0hUNlAudDEGqm0fUqRwsiDtd2l2KM2m0uxPafZbpAZRTHDKHf6s_1F9ATdlbys</recordid><startdate>20200601</startdate><enddate>20200601</enddate><creator>de Moura, Carolina Natel</creator><creator>Neto, Sílvio Luís Rafaeli</creator><creator>Campos, Claudia Guimarães Camargo</creator><creator>Sá, Eder Alexandre Schatz</creator><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QH</scope><scope>7ST</scope><scope>7UA</scope><scope>7WY</scope><scope>7WZ</scope><scope>7XB</scope><scope>87Z</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FH</scope><scope>8FK</scope><scope>8FL</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BEZIV</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>FRNLG</scope><scope>F~G</scope><scope>GNUQQ</scope><scope>H97</scope><scope>HCIFZ</scope><scope>K60</scope><scope>K6~</scope><scope>KR7</scope><scope>L.-</scope><scope>L.G</scope><scope>L6V</scope><scope>LK8</scope><scope>M0C</scope><scope>M2P</scope><scope>M7P</scope><scope>M7S</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQBIZ</scope><scope>PQBZA</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-6640-1961</orcidid><orcidid>https://orcid.org/0000-0003-3103-6789</orcidid><orcidid>https://orcid.org/0000-0001-5010-1895</orcidid><orcidid>https://orcid.org/0000-0002-3419-4865</orcidid></search><sort><creationdate>20200601</creationdate><title>Hydrological Impacts of Climate Change in a Well-preserved Upland Watershed</title><author>de Moura, Carolina Natel ; Neto, Sílvio Luís Rafaeli ; Campos, Claudia Guimarães Camargo ; Sá, Eder Alexandre Schatz</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c363t-e3ac5a455ea0ca7ef009d4db1706fd84b5114639af99d72a7c4a9eaaae3699cd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Atmospheric Sciences</topic><topic>Civil Engineering</topic><topic>Climate change</topic><topic>Climate effects</topic><topic>Components</topic><topic>Discharge</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Emission analysis</topic><topic>Emissions</topic><topic>Emissions control</topic><topic>Environment</topic><topic>Environmental impact</topic><topic>Flow duration curves</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Hydrogeology</topic><topic>Hydrology</topic><topic>Hydrology/Water Resources</topic><topic>Landscape preservation</topic><topic>Rain</topic><topic>Rainfall</topic><topic>Tropical climate</topic><topic>Tropical environment</topic><topic>Tropical environments</topic><topic>Water availability</topic><topic>Water balance</topic><topic>Watersheds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>de Moura, Carolina Natel</creatorcontrib><creatorcontrib>Neto, Sílvio Luís Rafaeli</creatorcontrib><creatorcontrib>Campos, Claudia Guimarães Camargo</creatorcontrib><creatorcontrib>Sá, Eder Alexandre Schatz</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Aqualine</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ABI/INFORM Collection</collection><collection>ABI/INFORM Global (PDF only)</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>ABI/INFORM Global (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ABI/INFORM Collection (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>Business Premium Collection</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Business Premium Collection (Alumni)</collection><collection>ABI/INFORM Global (Corporate)</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Business Collection (Alumni Edition)</collection><collection>ProQuest Business Collection</collection><collection>Civil Engineering Abstracts</collection><collection>ABI/INFORM Professional Advanced</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>ABI/INFORM Global</collection><collection>Science Database</collection><collection>Biological Science Database</collection><collection>Engineering Database</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Business</collection><collection>ProQuest One Business (Alumni)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Water resources management</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>de Moura, Carolina Natel</au><au>Neto, Sílvio Luís Rafaeli</au><au>Campos, Claudia Guimarães Camargo</au><au>Sá, Eder Alexandre Schatz</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrological Impacts of Climate Change in a Well-preserved Upland Watershed</atitle><jtitle>Water resources management</jtitle><stitle>Water Resour Manage</stitle><date>2020-06-01</date><risdate>2020</risdate><volume>34</volume><issue>8</issue><spage>2255</spage><epage>2267</epage><pages>2255-2267</pages><issn>0920-4741</issn><eissn>1573-1650</eissn><abstract>Much attention has been focused on investigating the effects of climate change on hydrological processes on a regional scale. However, the landscape approach, especially the case of well-preserved upland watersheds needs to be further studied. The Representative Concentration Pathway (RCP) or emission scenarios RCP 4.5 and RCP 8.5 were used to project the impacts of the climate change on the hydrological components of a well-preserved upland landscape with temperate climate, using the Upper Canoas watershed as a case study. The future hydrological projection indicated an increase in the monthly rainfall as well as a shift in the rainiest months from winter to spring. This change resulted in an increase in water balance components. The maximum discharges, as well as the modal discharge (Q50), may increase in the future, and the minimums corresponding to Q95 and Q98 may reduce for both emission scenarios. The results showed that a well-preserved upland watershed in a sub-tropical region might be capable of maintaining water availability at level that is enough for human activities in the future, even with the reduction of minimum permit discharge, which is supported by the increase of maximum and medium monthly discharges and a stable flow-duration curve.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s11269-019-02450-1</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-6640-1961</orcidid><orcidid>https://orcid.org/0000-0003-3103-6789</orcidid><orcidid>https://orcid.org/0000-0001-5010-1895</orcidid><orcidid>https://orcid.org/0000-0002-3419-4865</orcidid><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0920-4741 |
| ispartof | Water resources management, 2020-06, Vol.34 (8), p.2255-2267 |
| issn | 0920-4741 1573-1650 |
| language | eng |
| recordid | cdi_proquest_journals_2414131181 |
| source | SpringerLink Journals |
| subjects | Atmospheric Sciences Civil Engineering Climate change Climate effects Components Discharge Earth and Environmental Science Earth Sciences Emission analysis Emissions Emissions control Environment Environmental impact Flow duration curves Geotechnical Engineering & Applied Earth Sciences Hydrogeology Hydrology Hydrology/Water Resources Landscape preservation Rain Rainfall Tropical climate Tropical environment Tropical environments Water availability Water balance Watersheds |
| title | Hydrological Impacts of Climate Change in a Well-preserved Upland Watershed |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-05T00%3A30%3A15IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Hydrological%20Impacts%20of%20Climate%20Change%20in%20a%20Well-preserved%20Upland%20Watershed&rft.jtitle=Water%20resources%20management&rft.au=de%20Moura,%20Carolina%20Natel&rft.date=2020-06-01&rft.volume=34&rft.issue=8&rft.spage=2255&rft.epage=2267&rft.pages=2255-2267&rft.issn=0920-4741&rft.eissn=1573-1650&rft_id=info:doi/10.1007/s11269-019-02450-1&rft_dat=%3Cproquest_cross%3E2414131181%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2414131181&rft_id=info:pmid/&rfr_iscdi=true |