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Analysis of Turbulence in the Near-Shore Marine Atmospheric Surface Layer Using Sonic Anemometer Data.
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Analysis of Turbulence in the Near-Shore Marine Atmospheric Surface Layer Using Sonic Anemometer Data./
作者:
Bodoque Garcia, Alberto Javier.
出版者:
Ann Arbor : ProQuest Dissertations & Theses, : 2022,
面頁冊數:
103 p.
附註:
Source: Masters Abstracts International, Volume: 83-12.
Contained By:
Masters Abstracts International83-12.
標題:
Mechanical engineering. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=29208588
ISBN:
9798819384121
Analysis of Turbulence in the Near-Shore Marine Atmospheric Surface Layer Using Sonic Anemometer Data.
Bodoque Garcia, Alberto Javier.
Analysis of Turbulence in the Near-Shore Marine Atmospheric Surface Layer Using Sonic Anemometer Data.
- Ann Arbor : ProQuest Dissertations & Theses, 2022 - 103 p.
Source: Masters Abstracts International, Volume: 83-12.
Thesis (M.S.)--University of New Hampshire, 2022.
This item must not be sold to any third party vendors.
This thesis investigates turbulence in the marine atmospheric boundary layer (MABL), above, the wave boundary layer (WBL). To conduct this research, wind velocity and temperature data was collected by a sonic anemometer located on Wood, Island, NH, mounted to a tower 4 meters above the ground. To study turbulence in the MABL, variables such as Reynolds stress and friction velocity were calculated for different days in August 2019. Friction velocity was calculated following three different approaches: the first approach employs the eddy covariance method, the second employs a tilt correction to the eddy covariance method, and the third uses the Reynolds stress tensor invariants to calculate friction velocity, which eliminates the need for tilt correction. The three methods showed similar results for most of the days investigated. Lastly, the Monin-Obukhov Similarity Theory (MOST) was studied with the purpose of investigating how the Reynolds stress tensor invariants method for calculating friction velocity responds to scaling laws such as MOST. This analysis showed that friction velocity values are greater for the Reynolds stress tensor invariants method than for the eddy covariance method with tilt correction. Overall, the Reynolds stress tensor invariants method does not reproduce well the friction velocity values obtained from the eddy covariance method with tilt correction for any of the stability conditions of the MABL.
ISBN: 9798819384121Subjects--Topical Terms:
649730
Mechanical engineering.
Subjects--Index Terms:
Near-shore
Analysis of Turbulence in the Near-Shore Marine Atmospheric Surface Layer Using Sonic Anemometer Data.
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This item must not be sold to any third party vendors.
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This thesis investigates turbulence in the marine atmospheric boundary layer (MABL), above, the wave boundary layer (WBL). To conduct this research, wind velocity and temperature data was collected by a sonic anemometer located on Wood, Island, NH, mounted to a tower 4 meters above the ground. To study turbulence in the MABL, variables such as Reynolds stress and friction velocity were calculated for different days in August 2019. Friction velocity was calculated following three different approaches: the first approach employs the eddy covariance method, the second employs a tilt correction to the eddy covariance method, and the third uses the Reynolds stress tensor invariants to calculate friction velocity, which eliminates the need for tilt correction. The three methods showed similar results for most of the days investigated. Lastly, the Monin-Obukhov Similarity Theory (MOST) was studied with the purpose of investigating how the Reynolds stress tensor invariants method for calculating friction velocity responds to scaling laws such as MOST. This analysis showed that friction velocity values are greater for the Reynolds stress tensor invariants method than for the eddy covariance method with tilt correction. Overall, the Reynolds stress tensor invariants method does not reproduce well the friction velocity values obtained from the eddy covariance method with tilt correction for any of the stability conditions of the MABL.
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http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=29208588
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