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Interaction between surface and atmo...
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Garai, Anirban.
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Interaction between surface and atmosphere in a convective boundary layer.
紀錄類型:
書目-語言資料,印刷品 : Monograph/item
正題名/作者:
Interaction between surface and atmosphere in a convective boundary layer./
作者:
Garai, Anirban.
面頁冊數:
175 p.
附註:
Source: Dissertation Abstracts International, Volume: 75-02(E), Section: B.
Contained By:
Dissertation Abstracts International75-02B(E).
標題:
Engineering, Mechanical. -
電子資源:
http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3597827
ISBN:
9781303461750
Interaction between surface and atmosphere in a convective boundary layer.
Garai, Anirban.
Interaction between surface and atmosphere in a convective boundary layer.
- 175 p.
Source: Dissertation Abstracts International, Volume: 75-02(E), Section: B.
Thesis (Ph.D.)--University of California, San Diego, 2013.
Solar heating of the surface causes the near surface air to warm up and with sufficient buoyancy it ascends through the atmosphere as surface-layer plumes and thermals. The cold fluid from the upper part of the boundary layer descends as downdrafts. The downdrafts and thermals form streamwise roll vortices. All these turbulent coherent structures are important because they contribute most of the momentum and heat transport. While these structures have been studied in depth, their imprint on the surface through energy budget in a convective atmospheric boundary layer has received little attention. The main objective of the present study is to examine the turbulence-induced surface temperature fluctuations for different surface properties and stratification.
ISBN: 9781303461750Subjects--Topical Terms:
783786
Engineering, Mechanical.
Interaction between surface and atmosphere in a convective boundary layer.
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Source: Dissertation Abstracts International, Volume: 75-02(E), Section: B.
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Thesis (Ph.D.)--University of California, San Diego, 2013.
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Solar heating of the surface causes the near surface air to warm up and with sufficient buoyancy it ascends through the atmosphere as surface-layer plumes and thermals. The cold fluid from the upper part of the boundary layer descends as downdrafts. The downdrafts and thermals form streamwise roll vortices. All these turbulent coherent structures are important because they contribute most of the momentum and heat transport. While these structures have been studied in depth, their imprint on the surface through energy budget in a convective atmospheric boundary layer has received little attention. The main objective of the present study is to examine the turbulence-induced surface temperature fluctuations for different surface properties and stratification.
520
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Experiments were performed to measure atmospheric turbulence using sonic anemometers, fine wire thermocouples and LIDAR; and surface temperature using an infra-red camera over grass and artificial turf fields. The surface temperature fluctuations were found to be highly correlated to the turbulent coherent structures and follow the processes postulated in the surface renewal theory. The spatio-temporal scales and advection speed of the surface temperature fluctuation were found to match with those of turbulent coherent structures.
520
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A parametric direct numerical simulation (DNS) study was then performed by solving the solid-fluid heat transport mechanism numerically for varying solid thermal properties, solid thickness and strength of stratification. Even though there were large differences in the friction Reynolds and Richardson numbers between the experiments and numerical simulations, similar turbulent characteristics were observed. The ejection (sweep) events tend to be aligned with the streamwise direction to form roll vortices with unstable stratification. The solid-fluid interfacial temperature fluctuations increase with the decreases in solid thermal inertia; and with the increase in solid thickness to attain a constant value for a sufficiently thick solid. The temperature fluctuation changes from a Gaussian distribution near the wall to a positively skewed distribution away from the wall. The turbulent temperature fluctuations influence the solid interfacial temperature by thermal conduction only.
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These studies provided unique insights into the solid-fluid coupled heat transport in low and high Reynolds number flows. This turbulence induced surface temperature fluctuation can influence the performances of several satellite remote sensing models.
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