Comparisons of lysimetric and Bowen ratio estimates of evapotranspiration

Two sets of Bowen ratio and lysimeter measurements of evapotranspiration (ET) were compared for a field of winter wheat in Phoenix, Arizona. Daytime data for ten days of clear skies were examined. Daily lysimeter ET (LET) generally exceeded Bowen ratio ET (BRET). Advective cases were compared with l...

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Main Author: Brownridge, Alyce Mahan.
Other Authors: Gay, Lloyd W.
Language:en
Published: The University of Arizona. 1985
Online Access:http://hdl.handle.net/10150/191841
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spelling ndltd-arizona.edu-oai-arizona.openrepository.com-10150-1918412015-10-23T04:37:46Z Comparisons of lysimetric and Bowen ratio estimates of evapotranspiration Brownridge, Alyce Mahan. Gay, Lloyd W. Fogel, Martin M. Matthias, Allan Two sets of Bowen ratio and lysimeter measurements of evapotranspiration (ET) were compared for a field of winter wheat in Phoenix, Arizona. Daytime data for ten days of clear skies were examined. Daily lysimeter ET (LET) generally exceeded Bowen ratio ET (BRET). Advective cases were compared with lapse cases. For one set of lysimeter and Bowen ratio measurements, average LET was 10% more than BRET during advective conditions, while average LET and BRET were equal during lapse conditions. Results for the other pair of measurements were less conclusive due to unresolved lysimeter problems, with average LET 13% more than BRET during advection, and average LET 13% less than BRET during lapse conditions. These results suggest that the assumption of equal eddy diffusivities for heat and vapor caused BRET to underestimate evapotranspiration during advection. The Bowen ratio, wind speed, and wind direction were identified as possible variables for correcting BRET underestimation. 1985 Thesis-Reproduction (electronic) text http://hdl.handle.net/10150/191841 212626975 en 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. The University of Arizona.
collection NDLTD
language en
sources NDLTD
description Two sets of Bowen ratio and lysimeter measurements of evapotranspiration (ET) were compared for a field of winter wheat in Phoenix, Arizona. Daytime data for ten days of clear skies were examined. Daily lysimeter ET (LET) generally exceeded Bowen ratio ET (BRET). Advective cases were compared with lapse cases. For one set of lysimeter and Bowen ratio measurements, average LET was 10% more than BRET during advective conditions, while average LET and BRET were equal during lapse conditions. Results for the other pair of measurements were less conclusive due to unresolved lysimeter problems, with average LET 13% more than BRET during advection, and average LET 13% less than BRET during lapse conditions. These results suggest that the assumption of equal eddy diffusivities for heat and vapor caused BRET to underestimate evapotranspiration during advection. The Bowen ratio, wind speed, and wind direction were identified as possible variables for correcting BRET underestimation.
author2 Gay, Lloyd W.
author_facet Gay, Lloyd W.
Brownridge, Alyce Mahan.
author Brownridge, Alyce Mahan.
spellingShingle Brownridge, Alyce Mahan.
Comparisons of lysimetric and Bowen ratio estimates of evapotranspiration
author_sort Brownridge, Alyce Mahan.
title Comparisons of lysimetric and Bowen ratio estimates of evapotranspiration
title_short Comparisons of lysimetric and Bowen ratio estimates of evapotranspiration
title_full Comparisons of lysimetric and Bowen ratio estimates of evapotranspiration
title_fullStr Comparisons of lysimetric and Bowen ratio estimates of evapotranspiration
title_full_unstemmed Comparisons of lysimetric and Bowen ratio estimates of evapotranspiration
title_sort comparisons of lysimetric and bowen ratio estimates of evapotranspiration
publisher The University of Arizona.
publishDate 1985
url http://hdl.handle.net/10150/191841
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