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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Main Author: Malek, Esmaiel
Format: Others
Published: DigitalCommons@USU 1977
Subjects:
Online Access:https://digitalcommons.usu.edu/etd/3821
https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=4833&context=etd
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spelling 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
collection NDLTD
format Others
sources NDLTD
topic vertical
mesoscale
water
vapor
flux
irrigated
valley
Soil Science
spellingShingle 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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