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Evapotranspiration by remote sensing: An analysis of the Colorado River Delta before and after the Minute 319 pulse flow to Mexico
The unique hydrologic conditions characterizing riparian ecosystems in dryland (arid and semi-arid) areas help maintain high biodiversity and support high levels of primary productivity compared to associated uplands. In western North America, many riparian ecosystems have been damaged by altered fl...
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| Published in: | Ecological engineering 2017-09, Vol.106, p.725-732 |
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| cites | cdi_FETCH-LOGICAL-c421t-45398c40528959fb07a21f7079d38422fa35873d4563ecba53f63b0afc70d8b13 |
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| container_title | Ecological engineering |
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| creator | Jarchow, Christopher J. Nagler, Pamela L. Glenn, Edward P. Ramírez-Hernández, Jorge Rodríguez-Burgueño, J. Eliana |
| description | The unique hydrologic conditions characterizing riparian ecosystems in dryland (arid and semi-arid) areas help maintain high biodiversity and support high levels of primary productivity compared to associated uplands. In western North America, many riparian ecosystems have been damaged by altered flow regimes (e.g., impoundments and diversions) and over utilization of water resources (e.g., groundwater pumping for agriculture and human consumption). This has led some state and national governments to provide occasional environmental flows to address the declining condition of such riparian systems. In a historic agreement between the United States and Mexico, 130 million cubic meters (mcm) of water was released to the lower Colorado River Delta in Mexico, with the intent to evaluate the hydrological and biological response of the ecosystem. We used the Moderate Resolution Imaging Spectroradiometer (MODIS) Enhanced Vegetation Index (EVI) to estimate long term (2000–2014) and short term (pre- and post-pulse; 2013 and 2014) evapotranspiration (ET; used herein as an indicator of plant health) of the delta’s riparian corridor. We found the pulse flow helped reverse a decline in ET from 2011 to 2013, with a small, but statistically significant increase in 2014 (P |
| doi_str_mv | 10.1016/j.ecoleng.2016.10.056 |
| format | article |
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Eliana</creator><creatorcontrib>Jarchow, Christopher J. ; Nagler, Pamela L. ; Glenn, Edward P. ; Ramírez-Hernández, Jorge ; Rodríguez-Burgueño, J. Eliana</creatorcontrib><description>The unique hydrologic conditions characterizing riparian ecosystems in dryland (arid and semi-arid) areas help maintain high biodiversity and support high levels of primary productivity compared to associated uplands. In western North America, many riparian ecosystems have been damaged by altered flow regimes (e.g., impoundments and diversions) and over utilization of water resources (e.g., groundwater pumping for agriculture and human consumption). This has led some state and national governments to provide occasional environmental flows to address the declining condition of such riparian systems. In a historic agreement between the United States and Mexico, 130 million cubic meters (mcm) of water was released to the lower Colorado River Delta in Mexico, with the intent to evaluate the hydrological and biological response of the ecosystem. We used the Moderate Resolution Imaging Spectroradiometer (MODIS) Enhanced Vegetation Index (EVI) to estimate long term (2000–2014) and short term (pre- and post-pulse; 2013 and 2014) evapotranspiration (ET; used herein as an indicator of plant health) of the delta’s riparian corridor. We found the pulse flow helped reverse a decline in ET from 2011 to 2013, with a small, but statistically significant increase in 2014 (P<0.05). ET was greater than 100mcm in all years analyzed (even in years without surface flows) and exceeded surface flows in all years except 2000 (result of excess flows following an El Niño cycle in 1997) and 2014 (year of the pulse flow). Based on groundwater salinities and MODIS ET estimates, we estimated groundwater flow into the delta to be ∼103mcm. Shallow groundwater salinities in the riparian zone increased from 1.30gL−1 in the most upstream reach to 2.77gL−1 in the most downstream reach we measured, partly due to uptake of water by riparian vegetation and partly to intrusion of saline agricultural return flows. The disparity between surface flows and ET can likely be explained by the predominantly phreatophytic plants characterizing the area, which draw water from the aquifer. These results also suggest that the deteriorated condition of vegetation within the riparian zone might not be reversed by a single pulse event and could instead require subsequent pulse flows as a long term strategy to restore vegetation in this riparian ecosystem.</description><identifier>ISSN: 0925-8574</identifier><identifier>EISSN: 1872-6992</identifier><identifier>DOI: 10.1016/j.ecoleng.2016.10.056</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>Aquifers ; Arid regions ; Biodiversity ; Colorado River Delta ; Ecosystems ; El Nino ; El Nino phenomena ; Evapotranspiration ; Evapotranspiration (ET) ; Groundwater ; Groundwater flow ; Highlands ; Hydrologic cycle ; Hydrology ; Imaging techniques ; Impoundments ; Intrusion ; Measuring instruments ; Minute 319 ; MODIS ; Plants (botany) ; Primary production ; Pulse flow ; Remote sensing ; Riparian environments ; Riparian land ; Riparian vegetation ; Riparian zone ; Rivers ; Statistical analysis ; Stream flow ; Studies ; Uptake ; Vegetation ; Water balance ; Water flow ; Water resources</subject><ispartof>Ecological engineering, 2017-09, Vol.106, p.725-732</ispartof><rights>2016 Elsevier B.V.</rights><rights>Copyright Elsevier BV Sep 2017</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c421t-45398c40528959fb07a21f7079d38422fa35873d4563ecba53f63b0afc70d8b13</citedby><cites>FETCH-LOGICAL-c421t-45398c40528959fb07a21f7079d38422fa35873d4563ecba53f63b0afc70d8b13</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27922,27923</link.rule.ids></links><search><creatorcontrib>Jarchow, Christopher J.</creatorcontrib><creatorcontrib>Nagler, Pamela L.</creatorcontrib><creatorcontrib>Glenn, Edward P.</creatorcontrib><creatorcontrib>Ramírez-Hernández, Jorge</creatorcontrib><creatorcontrib>Rodríguez-Burgueño, J. Eliana</creatorcontrib><title>Evapotranspiration by remote sensing: An analysis of the Colorado River Delta before and after the Minute 319 pulse flow to Mexico</title><title>Ecological engineering</title><description>The unique hydrologic conditions characterizing riparian ecosystems in dryland (arid and semi-arid) areas help maintain high biodiversity and support high levels of primary productivity compared to associated uplands. In western North America, many riparian ecosystems have been damaged by altered flow regimes (e.g., impoundments and diversions) and over utilization of water resources (e.g., groundwater pumping for agriculture and human consumption). This has led some state and national governments to provide occasional environmental flows to address the declining condition of such riparian systems. In a historic agreement between the United States and Mexico, 130 million cubic meters (mcm) of water was released to the lower Colorado River Delta in Mexico, with the intent to evaluate the hydrological and biological response of the ecosystem. We used the Moderate Resolution Imaging Spectroradiometer (MODIS) Enhanced Vegetation Index (EVI) to estimate long term (2000–2014) and short term (pre- and post-pulse; 2013 and 2014) evapotranspiration (ET; used herein as an indicator of plant health) of the delta’s riparian corridor. We found the pulse flow helped reverse a decline in ET from 2011 to 2013, with a small, but statistically significant increase in 2014 (P<0.05). ET was greater than 100mcm in all years analyzed (even in years without surface flows) and exceeded surface flows in all years except 2000 (result of excess flows following an El Niño cycle in 1997) and 2014 (year of the pulse flow). Based on groundwater salinities and MODIS ET estimates, we estimated groundwater flow into the delta to be ∼103mcm. Shallow groundwater salinities in the riparian zone increased from 1.30gL−1 in the most upstream reach to 2.77gL−1 in the most downstream reach we measured, partly due to uptake of water by riparian vegetation and partly to intrusion of saline agricultural return flows. The disparity between surface flows and ET can likely be explained by the predominantly phreatophytic plants characterizing the area, which draw water from the aquifer. These results also suggest that the deteriorated condition of vegetation within the riparian zone might not be reversed by a single pulse event and could instead require subsequent pulse flows as a long term strategy to restore vegetation in this riparian ecosystem.</description><subject>Aquifers</subject><subject>Arid regions</subject><subject>Biodiversity</subject><subject>Colorado River Delta</subject><subject>Ecosystems</subject><subject>El Nino</subject><subject>El Nino phenomena</subject><subject>Evapotranspiration</subject><subject>Evapotranspiration (ET)</subject><subject>Groundwater</subject><subject>Groundwater flow</subject><subject>Highlands</subject><subject>Hydrologic cycle</subject><subject>Hydrology</subject><subject>Imaging techniques</subject><subject>Impoundments</subject><subject>Intrusion</subject><subject>Measuring instruments</subject><subject>Minute 319</subject><subject>MODIS</subject><subject>Plants (botany)</subject><subject>Primary production</subject><subject>Pulse flow</subject><subject>Remote sensing</subject><subject>Riparian environments</subject><subject>Riparian land</subject><subject>Riparian vegetation</subject><subject>Riparian zone</subject><subject>Rivers</subject><subject>Statistical analysis</subject><subject>Stream flow</subject><subject>Studies</subject><subject>Uptake</subject><subject>Vegetation</subject><subject>Water balance</subject><subject>Water flow</subject><subject>Water resources</subject><issn>0925-8574</issn><issn>1872-6992</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNqFkE9rGzEUxEVJoI7Tj1AQ9LyO_qxWq15KcJ22kBAI6VlotU-pzEbaSrITX_vJI-Pce3q84TcDMwh9pmRFCe2utiuwcYLwtGL1rdqKiO4DWtBesqZTip2hBVFMNL2Q7Ud0kfOWECKZUAv0b7M3cyzJhDz7ZIqPAQ8HnOA5FsAZQvbh6Su-DtgEMx2yzzg6XP4AXscpJjNG_OD3kPB3mIrBA7iYoLIjNq5U-Uje-bCrYZwqPO-mDNhN8QWXiO_g1dt4ic6dqfKn97tEv282j-ufze39j1_r69vGtoyWphVc9bYlgvVKKDcQaRh1kkg18r5lzBkuesnHVnQc7GAEdx0fiHFWkrEfKF-iL6fcOcW_O8hFb-Mu1VZZU9XRlom-lZUSJ8qmmHMCp-fkn006aEr0cW691e9z6-PcR7nOXX3fTj6oFfYeks7WQ7Aw-gS26DH6_yS8AYlci3w</recordid><startdate>20170901</startdate><enddate>20170901</enddate><creator>Jarchow, Christopher J.</creator><creator>Nagler, Pamela L.</creator><creator>Glenn, Edward P.</creator><creator>Ramírez-Hernández, Jorge</creator><creator>Rodríguez-Burgueño, J. 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Eliana</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c421t-45398c40528959fb07a21f7079d38422fa35873d4563ecba53f63b0afc70d8b13</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Aquifers</topic><topic>Arid regions</topic><topic>Biodiversity</topic><topic>Colorado River Delta</topic><topic>Ecosystems</topic><topic>El Nino</topic><topic>El Nino phenomena</topic><topic>Evapotranspiration</topic><topic>Evapotranspiration (ET)</topic><topic>Groundwater</topic><topic>Groundwater flow</topic><topic>Highlands</topic><topic>Hydrologic cycle</topic><topic>Hydrology</topic><topic>Imaging techniques</topic><topic>Impoundments</topic><topic>Intrusion</topic><topic>Measuring instruments</topic><topic>Minute 319</topic><topic>MODIS</topic><topic>Plants (botany)</topic><topic>Primary production</topic><topic>Pulse flow</topic><topic>Remote sensing</topic><topic>Riparian environments</topic><topic>Riparian land</topic><topic>Riparian vegetation</topic><topic>Riparian zone</topic><topic>Rivers</topic><topic>Statistical analysis</topic><topic>Stream flow</topic><topic>Studies</topic><topic>Uptake</topic><topic>Vegetation</topic><topic>Water balance</topic><topic>Water flow</topic><topic>Water resources</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Jarchow, Christopher J.</creatorcontrib><creatorcontrib>Nagler, Pamela L.</creatorcontrib><creatorcontrib>Glenn, Edward P.</creatorcontrib><creatorcontrib>Ramírez-Hernández, Jorge</creatorcontrib><creatorcontrib>Rodríguez-Burgueño, J. 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Eliana</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Evapotranspiration by remote sensing: An analysis of the Colorado River Delta before and after the Minute 319 pulse flow to Mexico</atitle><jtitle>Ecological engineering</jtitle><date>2017-09-01</date><risdate>2017</risdate><volume>106</volume><spage>725</spage><epage>732</epage><pages>725-732</pages><issn>0925-8574</issn><eissn>1872-6992</eissn><abstract>The unique hydrologic conditions characterizing riparian ecosystems in dryland (arid and semi-arid) areas help maintain high biodiversity and support high levels of primary productivity compared to associated uplands. In western North America, many riparian ecosystems have been damaged by altered flow regimes (e.g., impoundments and diversions) and over utilization of water resources (e.g., groundwater pumping for agriculture and human consumption). This has led some state and national governments to provide occasional environmental flows to address the declining condition of such riparian systems. In a historic agreement between the United States and Mexico, 130 million cubic meters (mcm) of water was released to the lower Colorado River Delta in Mexico, with the intent to evaluate the hydrological and biological response of the ecosystem. We used the Moderate Resolution Imaging Spectroradiometer (MODIS) Enhanced Vegetation Index (EVI) to estimate long term (2000–2014) and short term (pre- and post-pulse; 2013 and 2014) evapotranspiration (ET; used herein as an indicator of plant health) of the delta’s riparian corridor. We found the pulse flow helped reverse a decline in ET from 2011 to 2013, with a small, but statistically significant increase in 2014 (P<0.05). ET was greater than 100mcm in all years analyzed (even in years without surface flows) and exceeded surface flows in all years except 2000 (result of excess flows following an El Niño cycle in 1997) and 2014 (year of the pulse flow). Based on groundwater salinities and MODIS ET estimates, we estimated groundwater flow into the delta to be ∼103mcm. Shallow groundwater salinities in the riparian zone increased from 1.30gL−1 in the most upstream reach to 2.77gL−1 in the most downstream reach we measured, partly due to uptake of water by riparian vegetation and partly to intrusion of saline agricultural return flows. The disparity between surface flows and ET can likely be explained by the predominantly phreatophytic plants characterizing the area, which draw water from the aquifer. These results also suggest that the deteriorated condition of vegetation within the riparian zone might not be reversed by a single pulse event and could instead require subsequent pulse flows as a long term strategy to restore vegetation in this riparian ecosystem.</abstract><cop>Amsterdam</cop><pub>Elsevier B.V</pub><doi>10.1016/j.ecoleng.2016.10.056</doi><tpages>8</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Aquifers Arid regions Biodiversity Colorado River Delta Ecosystems El Nino El Nino phenomena Evapotranspiration Evapotranspiration (ET) Groundwater Groundwater flow Highlands Hydrologic cycle Hydrology Imaging techniques Impoundments Intrusion Measuring instruments Minute 319 MODIS Plants (botany) Primary production Pulse flow Remote sensing Riparian environments Riparian land Riparian vegetation Riparian zone Rivers Statistical analysis Stream flow Studies Uptake Vegetation Water balance Water flow Water resources |
| title | Evapotranspiration by remote sensing: An analysis of the Colorado River Delta before and after the Minute 319 pulse flow to Mexico |
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