Temperature profiles, plumes, and spectra in the surface layer of convective boundary layers

K. Mcnaughton, S. Chowdhuri
{"title":"Temperature profiles, plumes, and spectra in the surface layer of convective boundary layers","authors":"K. Mcnaughton, S. Chowdhuri","doi":"10.1063/5.0023429","DOIUrl":null,"url":null,"abstract":"We survey temperature patterns and heat transport in convective boundary layers (CBLs) from the perspective that these are emergent properties of far-from-equilibrium, complex dynamical systems. We introduce a two-temperature (2T) toy model to define the cross-sectional areas of plumes, and connect the scaling properties of temperature gradients, temperature variance and heat transport to this area. We examine temperature ($T$) probability density functions and $w$-$T$ joint probability density functions, $T$ spectra and $wT$ cospectra observed both within and above the surface friction layer. Here $w$ is vertical velocity. In our discussion of $T$ spectra and $wT$ cospectra we focus on the self-similarity property of the plumes and flux events above the SFL. We interpret the $z^{1/2}$ dependence of the mixed length scale for wavenumbers in the $T$ spectra as reflecting the cross-sectional areas of the plumes, and so with the $z^{-1/2}$ form of the temperature profile, where $z$ is observation height. We introduce new scaling results for $T$ spectra and $wT$ cospectra from within the surface friction layer (SFL), based on a data from the SLTEST experiment. We confirm earlier results showing that the scaling behaviours of $T$ spectra and $wT$ cospectra change for heights below $z/z_s<0.1$, where $z_s$ the height of the SFL, and come to display properties associated with random diffusion. We conclude by contrasting our interpretation of the role of buoyancy as a system-wide action in CBL flows with that of Richardson, whose ideas inform the current interpretation of the statistical fluid mechanics model of boundary-layer flows.","PeriodicalId":328276,"journal":{"name":"arXiv: Fluid Dynamics","volume":"78 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2020-07-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv: Fluid Dynamics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1063/5.0023429","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

We survey temperature patterns and heat transport in convective boundary layers (CBLs) from the perspective that these are emergent properties of far-from-equilibrium, complex dynamical systems. We introduce a two-temperature (2T) toy model to define the cross-sectional areas of plumes, and connect the scaling properties of temperature gradients, temperature variance and heat transport to this area. We examine temperature ($T$) probability density functions and $w$-$T$ joint probability density functions, $T$ spectra and $wT$ cospectra observed both within and above the surface friction layer. Here $w$ is vertical velocity. In our discussion of $T$ spectra and $wT$ cospectra we focus on the self-similarity property of the plumes and flux events above the SFL. We interpret the $z^{1/2}$ dependence of the mixed length scale for wavenumbers in the $T$ spectra as reflecting the cross-sectional areas of the plumes, and so with the $z^{-1/2}$ form of the temperature profile, where $z$ is observation height. We introduce new scaling results for $T$ spectra and $wT$ cospectra from within the surface friction layer (SFL), based on a data from the SLTEST experiment. We confirm earlier results showing that the scaling behaviours of $T$ spectra and $wT$ cospectra change for heights below $z/z_s<0.1$, where $z_s$ the height of the SFL, and come to display properties associated with random diffusion. We conclude by contrasting our interpretation of the role of buoyancy as a system-wide action in CBL flows with that of Richardson, whose ideas inform the current interpretation of the statistical fluid mechanics model of boundary-layer flows.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
对流边界层表层的温度分布、羽流和光谱
我们调查了温度模式和热输运在对流边界层(CBLs)的角度来看,这些是紧急性质的远非平衡,复杂的动力系统。我们引入了一个双温度(2T)玩具模型来定义羽流的横截面积,并将温度梯度、温度方差和热输运的标度特性与该区域联系起来。我们研究了温度($T$)概率密度函数和$w$-$T$联合概率密度函数,$T$光谱和$wT$共光谱在表面摩擦层内部和上面观察到。这里w是垂直速度。在讨论$T$谱和$wT$共谱时,我们着重讨论了SFL以上羽流和通量事件的自相似性。我们将$T$光谱中波数的混合长度尺度的$z^{1/2}$依赖性解释为反映羽流的横截面积,因此与$z^{-1/2}$形式的温度剖面有关,其中$z$为观测高度。基于SLTEST实验的数据,我们介绍了表面摩擦层(SFL)内的$T$谱和$wT$共谱的新的标度结果。我们证实了先前的结果,表明$T$光谱和$wT$共光谱的缩放行为在$z/z_s<0.1$(其中$z_s$为SFL的高度)以下发生变化,并开始显示与随机扩散相关的性质。最后,我们将我们对浮力在CBL流动中作为全系统作用的解释与理查森的解释进行了对比,理查森的观点为目前对边界层流动的统计流体力学模型的解释提供了信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
Reproduction of vortex lattices in the simulations of rotating liquid helium-4 by numerically solving the two-fluid model using smoothed-particle hydrodynamics incorporating vortex dynamics Surface wave scattering by multiple flexible fishing cage system Capillary fluctuations and energy dynamics for flow in porous media Paths to caustic formation in turbulent aerosols An implicit kinetic inviscid flux for predicting continuum flows in all speed regimes
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1