Evapotranspiraton Partitioning Using Stable Water Isotopes in a Semi-Arid Evergreen Forest
| dc.contributor.advisor | Dominguez, Francina | en_US |
| dc.contributor.author | Meuth, Jacob | |
| dc.creator | Meuth, Jacob | en_US |
| dc.date.accessioned | 2012-06-08T21:02:47Z | |
| dc.date.available | 2012-06-08T21:02:47Z | |
| dc.date.issued | 2012 | |
| dc.identifier.uri | http://hdl.handle.net/10150/228162 | |
| dc.description.abstract | Total evapotranspiration (ET) is the key process that links the land and the atmosphere via water, energy and carbon exchange. ET is a combination of evaporation and transpiration, which behave dynamically in very different ways. In this work we investigate the relative contribution of transpiration and soil evaporation to total ET in a semi-wooded, semi-arid forest in the Manitou Research Park northwest of Colorado Springs, CO. We use stable water isotopes measured at different levels within and outside the canopy, over a 30-day period (June 26 - July 26, 2010), using a field-deployable cavity ring-down spectrometer. The traditional "Keeling plot" analysis is used to partition the ET flux from moisture that comes from outside of the ecosystem, and then a simple model is used to partition the transpiration flux. In addition, we introduce a new alternative "multi-level" method to calculate the fraction of transpiration to total ET. Both the "Keeling plot" method and the "multi-level" method yield very similar fractions of transpiration to total ET, ranging from about 15% to about 85%. We compare both methodologies and discuss some of the corrections that must be made when measuring with high-frequency field-deployable instruments. | |
| dc.language.iso | en | en_US |
| dc.publisher | The University of Arizona. | en_US |
| dc.rights | Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. | en_US |
| dc.subject | multi-level | en_US |
| dc.subject | partitioning | en_US |
| dc.subject | transpiration | en_US |
| dc.subject | Atmospheric Sciences | en_US |
| dc.subject | forest | en_US |
| dc.subject | isotopes | en_US |
| dc.title | Evapotranspiraton Partitioning Using Stable Water Isotopes in a Semi-Arid Evergreen Forest | en_US |
| dc.type | text | en_US |
| dc.type | Electronic Thesis | en_US |
| thesis.degree.grantor | University of Arizona | en_US |
| thesis.degree.level | masters | en_US |
| dc.contributor.committeemember | Shuttleworth, William J. | en_US |
| dc.contributor.committeemember | McIntosh, Jennifer | en_US |
| thesis.degree.discipline | Graduate College | en_US |
| thesis.degree.discipline | Atmospheric Sciences | en_US |
| thesis.degree.name | M.S. | en_US |
| refterms.dateFOA | 2018-06-27T09:39:23Z | |
| html.description.abstract | Total evapotranspiration (ET) is the key process that links the land and the atmosphere via water, energy and carbon exchange. ET is a combination of evaporation and transpiration, which behave dynamically in very different ways. In this work we investigate the relative contribution of transpiration and soil evaporation to total ET in a semi-wooded, semi-arid forest in the Manitou Research Park northwest of Colorado Springs, CO. We use stable water isotopes measured at different levels within and outside the canopy, over a 30-day period (June 26 - July 26, 2010), using a field-deployable cavity ring-down spectrometer. The traditional "Keeling plot" analysis is used to partition the ET flux from moisture that comes from outside of the ecosystem, and then a simple model is used to partition the transpiration flux. In addition, we introduce a new alternative "multi-level" method to calculate the fraction of transpiration to total ET. Both the "Keeling plot" method and the "multi-level" method yield very similar fractions of transpiration to total ET, ranging from about 15% to about 85%. We compare both methodologies and discuss some of the corrections that must be made when measuring with high-frequency field-deployable instruments. |
