Vertical Mesoscale Water Vapor Flux in an Irrigated Valley
To obtain the profiles of dry bulb and wet bulb temperature, specific humidity, q, and air density, ρ, to a height of 200 meters above the ground, a precise lightweight thermocouple psychrometer was designed. To lift the thermocouple psychrometer and the attached wires in obtaining the ρq profiles,...
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ndltd-UTAHS-oai-digitalcommons.usu.edu-etd-48332019-10-13T05:44:29Z Vertical Mesoscale Water Vapor Flux in an Irrigated Valley Malek, Esmaiel To obtain the profiles of dry bulb and wet bulb temperature, specific humidity, q, and air density, ρ, to a height of 200 meters above the ground, a precise lightweight thermocouple psychrometer was designed. To lift the thermocouple psychrometer and the attached wires in obtaining the ρq profiles, a rigid polyethylene balloon augmented with 5.5-feet outdoor or 100-g meteorological balloons were used. Using the height dependent eddy exchange coefficient and a one-dimensional time-dependent profile model, the nighttime variations of ρq as a function of height were predicted and compared with observed values. It was found that the general shape of the eddy exchange coefficient, K(Z), was approximately the same as found in recent literature. 1977-05-01T07:00:00Z text application/pdf https://digitalcommons.usu.edu/etd/3821 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=4833&context=etd Copyright for this work is held by the author. Transmission or reproduction of materials protected by copyright beyond that allowed by fair use requires the written permission of the copyright owners. Works not in the public domain cannot be commercially exploited without permission of the copyright owner. Responsibility for any use rests exclusively with the user. For more information contact Andrew Wesolek (andrew.wesolek@usu.edu). All Graduate Theses and Dissertations DigitalCommons@USU vertical mesoscale water vapor flux irrigated valley Soil Science |
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vertical mesoscale water vapor flux irrigated valley Soil Science |
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vertical mesoscale water vapor flux irrigated valley Soil Science Malek, Esmaiel Vertical Mesoscale Water Vapor Flux in an Irrigated Valley |
description |
To obtain the profiles of dry bulb and wet bulb temperature, specific humidity, q, and air density, ρ, to a height of 200 meters above the ground, a precise lightweight thermocouple psychrometer was designed. To lift the thermocouple psychrometer and the attached wires in obtaining the ρq profiles, a rigid polyethylene balloon augmented with 5.5-feet outdoor or 100-g meteorological balloons were used. Using the height dependent eddy exchange coefficient and a one-dimensional time-dependent profile model, the nighttime variations of ρq as a function of height were predicted and compared with observed values. It was found that the general shape of the eddy exchange coefficient, K(Z), was approximately the same as found in recent literature. |
author |
Malek, Esmaiel |
author_facet |
Malek, Esmaiel |
author_sort |
Malek, Esmaiel |
title |
Vertical Mesoscale Water Vapor Flux in an Irrigated Valley |
title_short |
Vertical Mesoscale Water Vapor Flux in an Irrigated Valley |
title_full |
Vertical Mesoscale Water Vapor Flux in an Irrigated Valley |
title_fullStr |
Vertical Mesoscale Water Vapor Flux in an Irrigated Valley |
title_full_unstemmed |
Vertical Mesoscale Water Vapor Flux in an Irrigated Valley |
title_sort |
vertical mesoscale water vapor flux in an irrigated valley |
publisher |
DigitalCommons@USU |
publishDate |
1977 |
url |
https://digitalcommons.usu.edu/etd/3821 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=4833&context=etd |
work_keys_str_mv |
AT malekesmaiel verticalmesoscalewatervaporfluxinanirrigatedvalley |
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1719266437503123456 |