Long-term Water Table Monitoring of Rio Grande Riparian Ecosystems for Restoration Potential Amid Hydroclimatic Challenges.
Identifieur interne : 001313 ( Main/Exploration ); précédent : 001312; suivant : 001314Long-term Water Table Monitoring of Rio Grande Riparian Ecosystems for Restoration Potential Amid Hydroclimatic Challenges.
Auteurs : James R. Thibault [États-Unis] ; James R. Cleverly [États-Unis, Australie] ; Clifford N. Dahm [États-Unis]Source :
- Environmental management [ 1432-1009 ] ; 2017.
Descripteurs français
- KwdFr :
- Assainissement et restauration de l'environnement (MeSH), Climat désertique (MeSH), Eau douce (analyse), Inondations (MeSH), Mouvements de l'eau (MeSH), Nappe phréatique (analyse), Populus (croissance et développement), Surveillance de l'environnement (méthodes), Sécheresses (MeSH), Écosystème (MeSH), États du Sud-Ouest des États-Unis (MeSH).
- MESH :
- analyse : Eau douce, Nappe phréatique.
- croissance et développement : Populus.
- méthodes : Surveillance de l'environnement.
- Assainissement et restauration de l'environnement, Climat désertique, Inondations, Mouvements de l'eau, Sécheresses, Écosystème, États du Sud-Ouest des États-Unis.
English descriptors
- KwdEn :
- MESH :
- analysis : Fresh Water, Groundwater.
- growth & development : Populus.
- methods : Environmental Monitoring.
- Desert Climate, Droughts, Ecosystem, Environmental Restoration and Remediation, Floods, Southwestern United States, Water Movements.
Abstract
Hydrological processes drive the ecological functioning and sustainability of cottonwood-dominated riparian ecosystems in the arid southwestern USA. Snowmelt runoff elevates groundwater levels and inundates floodplains, which promotes cottonwood germination. Once established, these phreatophytes rely on accessible water tables (WTs). In New Mexico's Middle Rio Grande corridor diminished flooding and deepening WTs threaten native riparian communities. We monitored surface flows and riparian WTs for up to 14 years, which revealed that WTs and surface flows, including peak snowmelt discharge, respond to basin climate conditions and resource management. WT hydrographs influence the composition of riparian communities and can be used to assess if potential restoration sites meet native vegetation tolerances for WT depths, rates of recession, and variability throughout their life stages. WTs were highly variable in some sites, which can preclude native vegetation less adapted to deep drawdowns during extended droughts. Rates of WT recession varied between sites and should be assessed in regard to recruitment potential. Locations with relatively shallow WTs and limited variability are likely to be more viable for successful restoration. Suitable sites have diminished greatly as the once meandering Rio Grande has been constrained and depleted. Increasing demands on water and the presence of invasive vegetation better adapted to the altered hydrologic regime further impact native riparian communities. Long-term monitoring over a range of sites and hydroclimatic extremes reveals attributes that can be evaluated for restoration potential.
DOI: 10.1007/s00267-017-0945-x
PubMed: 28993863
Affiliations:
Links toward previous steps (curation, corpus...)
Le document en format XML
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Snowmelt runoff elevates groundwater levels and inundates floodplains, which promotes cottonwood germination. Once established, these phreatophytes rely on accessible water tables (WTs). In New Mexico's Middle Rio Grande corridor diminished flooding and deepening WTs threaten native riparian communities. We monitored surface flows and riparian WTs for up to 14 years, which revealed that WTs and surface flows, including peak snowmelt discharge, respond to basin climate conditions and resource management. WT hydrographs influence the composition of riparian communities and can be used to assess if potential restoration sites meet native vegetation tolerances for WT depths, rates of recession, and variability throughout their life stages. WTs were highly variable in some sites, which can preclude native vegetation less adapted to deep drawdowns during extended droughts. Rates of WT recession varied between sites and should be assessed in regard to recruitment potential. Locations with relatively shallow WTs and limited variability are likely to be more viable for successful restoration. Suitable sites have diminished greatly as the once meandering Rio Grande has been constrained and depleted. Increasing demands on water and the presence of invasive vegetation better adapted to the altered hydrologic regime further impact native riparian communities. Long-term monitoring over a range of sites and hydroclimatic extremes reveals attributes that can be evaluated for restoration potential.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" IndexingMethod="Curated" Owner="NLM"><PMID Version="1">28993863</PMID><DateCompleted><Year>2018</Year><Month>03</Month><Day>02</Day></DateCompleted><DateRevised><Year>2018</Year><Month>12</Month><Day>02</Day></DateRevised><Article PubModel="Print-Electronic"><Journal><ISSN IssnType="Electronic">1432-1009</ISSN><JournalIssue CitedMedium="Internet"><Volume>60</Volume><Issue>6</Issue><PubDate><Year>2017</Year><Month>12</Month></PubDate></JournalIssue><Title>Environmental management</Title><ISOAbbreviation>Environ Manage</ISOAbbreviation></Journal><ArticleTitle>Long-term Water Table Monitoring of Rio Grande Riparian Ecosystems for Restoration Potential Amid Hydroclimatic Challenges.</ArticleTitle><Pagination><MedlinePgn>1101-1115</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1007/s00267-017-0945-x</ELocationID><Abstract><AbstractText>Hydrological processes drive the ecological functioning and sustainability of cottonwood-dominated riparian ecosystems in the arid southwestern USA. Snowmelt runoff elevates groundwater levels and inundates floodplains, which promotes cottonwood germination. Once established, these phreatophytes rely on accessible water tables (WTs). In New Mexico's Middle Rio Grande corridor diminished flooding and deepening WTs threaten native riparian communities. We monitored surface flows and riparian WTs for up to 14 years, which revealed that WTs and surface flows, including peak snowmelt discharge, respond to basin climate conditions and resource management. WT hydrographs influence the composition of riparian communities and can be used to assess if potential restoration sites meet native vegetation tolerances for WT depths, rates of recession, and variability throughout their life stages. WTs were highly variable in some sites, which can preclude native vegetation less adapted to deep drawdowns during extended droughts. Rates of WT recession varied between sites and should be assessed in regard to recruitment potential. Locations with relatively shallow WTs and limited variability are likely to be more viable for successful restoration. Suitable sites have diminished greatly as the once meandering Rio Grande has been constrained and depleted. Increasing demands on water and the presence of invasive vegetation better adapted to the altered hydrologic regime further impact native riparian communities. Long-term monitoring over a range of sites and hydroclimatic extremes reveals attributes that can be evaluated for restoration potential.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Thibault</LastName><ForeName>James R</ForeName><Initials>JR</Initials><Identifier Source="ORCID">0000-0001-7079-1117</Identifier><AffiliationInfo><Affiliation>Department of Biology, University of New Mexico, Albuquerque, NM, 87131, USA. thibault@unm.edu.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Cleverly</LastName><ForeName>James R</ForeName><Initials>JR</Initials><AffiliationInfo><Affiliation>Department of Biology, University of New Mexico, Albuquerque, NM, 87131, USA.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>Terrestrial Ecohydrology Research Group, School of Life Sciences, University of Technology Sydney, P.O. Box 123, Broadway, NSW, 2007, Australia.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Dahm</LastName><ForeName>Clifford N</ForeName><Initials>CN</Initials><AffiliationInfo><Affiliation>Department of Biology, University of New Mexico, Albuquerque, NM, 87131, USA.</Affiliation></AffiliationInfo><AffiliationInfo><Affiliation>Delta Stewardship Council, 980 Ninth St., Ste. 1500, Sacramento, CA, 95814, USA.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2017</Year><Month>10</Month><Day>09</Day></ArticleDate></Article><MedlineJournalInfo><Country>United States</Country><MedlineTA>Environ Manage</MedlineTA><NlmUniqueID>7703893</NlmUniqueID><ISSNLinking>0364-152X</ISSNLinking></MedlineJournalInfo><CitationSubset>IM</CitationSubset><MeshHeadingList><MeshHeading><DescriptorName UI="D003889" MajorTopicYN="N">Desert Climate</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D055864" MajorTopicYN="N">Droughts</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D017753" MajorTopicYN="Y">Ecosystem</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D004784" MajorTopicYN="N">Environmental Monitoring</DescriptorName><QualifierName UI="Q000379" MajorTopicYN="Y">methods</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D052918" MajorTopicYN="N">Environmental Restoration and Remediation</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D055868" MajorTopicYN="N">Floods</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D005618" MajorTopicYN="N">Fresh Water</DescriptorName><QualifierName UI="Q000032" MajorTopicYN="Y">analysis</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D060587" MajorTopicYN="N">Groundwater</DescriptorName><QualifierName UI="Q000032" MajorTopicYN="Y">analysis</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D032107" MajorTopicYN="N">Populus</DescriptorName><QualifierName UI="Q000254" MajorTopicYN="Y">growth & development</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D015206" MajorTopicYN="N">Southwestern United States</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D014872" MajorTopicYN="Y">Water Movements</DescriptorName></MeshHeading></MeshHeadingList><KeywordList Owner="NOTNLM"><Keyword MajorTopicYN="Y">Cottonwood</Keyword><Keyword MajorTopicYN="Y">Drought</Keyword><Keyword MajorTopicYN="Y">Flood</Keyword><Keyword MajorTopicYN="Y">Groundwater</Keyword><Keyword MajorTopicYN="Y">Salt cedar</Keyword><Keyword MajorTopicYN="Y">Surface flow</Keyword></KeywordList></MedlineCitation><PubmedData><History><PubMedPubDate PubStatus="received"><Year>2017</Year><Month>01</Month><Day>10</Day></PubMedPubDate><PubMedPubDate 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Thibault</name></noRegion><name sortKey="Cleverly, James R" sort="Cleverly, James R" uniqKey="Cleverly J" first="James R" last="Cleverly">James R. Cleverly</name><name sortKey="Dahm, Clifford N" sort="Dahm, Clifford N" uniqKey="Dahm C" first="Clifford N" last="Dahm">Clifford N. Dahm</name><name sortKey="Dahm, Clifford N" sort="Dahm, Clifford N" uniqKey="Dahm C" first="Clifford N" last="Dahm">Clifford N. Dahm</name></country><country name="Australie"><noRegion><name sortKey="Cleverly, James R" sort="Cleverly, James R" uniqKey="Cleverly J" first="James R" last="Cleverly">James R. Cleverly</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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