Turbulence behaviors underlying the sensible heat and water vapor flux dissimilarity in a stably stratified flow

Based on eddy-covariance measurements over a glacier, we investigate the scalar flux dissimilarity between sensible heat and water vapor transport in a stably stratified flow. The scalar flux correlation coefficient R F is used as a measure of variable levels of the flux similarity, which are often...

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Published inEnvironmental fluid mechanics (Dordrecht, Netherlands : 2001) Vol. 23; no. 5; pp. 1193 - 1232
Main Authors Guo, Xiaofeng, Yang, Wei, Hong, Jinkyu, Wang, Linlin, Gao, Zhiqiu, Zhou, Degang
Format Journal Article
LanguageEnglish
Published Dordrecht Springer Netherlands 01.10.2023
Springer Nature B.V
Subjects
Air parcels
Air temperature
Amplitude
Amplitudes
Analysis
Anisotropy
Aspect ratio
Classical Mechanics
Connecting
Correlation coefficient
Correlation coefficients
Earth and Environmental Science
Earth Sciences
Eddy covariance
Enthalpy
Environmental Physics
Fast Fourier transformations
Fluctuations
Fluxes
Fourier transforms
Glacier measurements
Glaciers
Heat
Hole size
Hydrogeology
Hydrology/Water Resources
Oceanography
Original Article
Quadrants
Resonant frequencies
Resonant frequency
Scalars
Sensible heat
Stratified flow
Temperature fluctuations
Turbulence
Vortices
Water vapor
Water vapor flux
Water vapor transport
Water vapour
Scalar turbulence
Octant analysis technique
Stably stratified boundary layer
Turbulent flux dissimilarity
Sensible heat and water vapor transport
Online AccessGet full text
ISSN1567-7419
1573-1510
DOI10.1007/s10652-023-09940-2

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Abstract Based on eddy-covariance measurements over a glacier, we investigate the scalar flux dissimilarity between sensible heat and water vapor transport in a stably stratified flow. The scalar flux correlation coefficient R F is used as a measure of variable levels of the flux similarity, which are often elevated due to a rising degree of the kinetic anisotropy of turbulence. Moreover, sensible heat is transported more efficiently than water vapor; and transport efficiencies of these two scalars are separated in terms of their variability with the velocity aspect ratio. Compared with air temperature fluctuations, turbulence characteristics of the water vapor concentration are subject to a more pronounced modification because of distinct magnitudes of R F . An innovative method is employed for connecting quadrant analysis and cospectral analysis, so that the hyperbolic quadrant-hole size can be coupled to the natural frequency underlying the fast Fourier transform. Then, we introduce a hypothetical octant hole whose size is invoked as a metric for the amplitude scale of fluctuating scalar fluxes. The contributions to R F are quantified for a variety of eddy structures that are associated with different ranges of the amplitude scale. Regarding larger-amplitude fluxes due to heated drier air parcels in descending motions, reductions in R F correspond to increasing flux fractions for water vapor, whereas the flux fractions for sensible heat are largely unchanged. Overall, a more substantial portion of the changes in R F can be ascribed to smaller-amplitude fluxes due to cooled moister air parcels and heated drier air parcels being involved, respectively, in ascending and descending motions. Reductions in R F relate to the flux fractions of a decreasing magnitude for sensible heat but of an increasing magnitude for water vapor. Highlights In a stably stratified flow, dissimilar transport of sensible heat and water vapor is associated with anisotropy properties of turbulence. A new approach is developed for a scrutiny of scalar transport, whereby quadrant analysis and cospectral analysis can be interconnected. Extending octant analysis to scalar turbulence identifies eddy structures that exhibit distinct behaviors indicative of the flux dissimilarity. Comparatively small-amplitude fluxes are accountable for a substantial portion of the changes in the overall level of scalar flux correlation.
AbstractList Based on eddy-covariance measurements over a glacier, we investigate the scalar flux dissimilarity between sensible heat and water vapor transport in a stably stratified flow. The scalar flux correlation coefficient R F is used as a measure of variable levels of the flux similarity, which are often elevated due to a rising degree of the kinetic anisotropy of turbulence. Moreover, sensible heat is transported more efficiently than water vapor; and transport efficiencies of these two scalars are separated in terms of their variability with the velocity aspect ratio. Compared with air temperature fluctuations, turbulence characteristics of the water vapor concentration are subject to a more pronounced modification because of distinct magnitudes of R F . An innovative method is employed for connecting quadrant analysis and cospectral analysis, so that the hyperbolic quadrant-hole size can be coupled to the natural frequency underlying the fast Fourier transform. Then, we introduce a hypothetical octant hole whose size is invoked as a metric for the amplitude scale of fluctuating scalar fluxes. The contributions to R F are quantified for a variety of eddy structures that are associated with different ranges of the amplitude scale. Regarding larger-amplitude fluxes due to heated drier air parcels in descending motions, reductions in R F correspond to increasing flux fractions for water vapor, whereas the flux fractions for sensible heat are largely unchanged. Overall, a more substantial portion of the changes in R F can be ascribed to smaller-amplitude fluxes due to cooled moister air parcels and heated drier air parcels being involved, respectively, in ascending and descending motions. Reductions in R F relate to the flux fractions of a decreasing magnitude for sensible heat but of an increasing magnitude for water vapor. Highlights In a stably stratified flow, dissimilar transport of sensible heat and water vapor is associated with anisotropy properties of turbulence. A new approach is developed for a scrutiny of scalar transport, whereby quadrant analysis and cospectral analysis can be interconnected. Extending octant analysis to scalar turbulence identifies eddy structures that exhibit distinct behaviors indicative of the flux dissimilarity. Comparatively small-amplitude fluxes are accountable for a substantial portion of the changes in the overall level of scalar flux correlation.
Based on eddy-covariance measurements over a glacier, we investigate the scalar flux dissimilarity between sensible heat and water vapor transport in a stably stratified flow. The scalar flux correlation coefficient RF is used as a measure of variable levels of the flux similarity, which are often elevated due to a rising degree of the kinetic anisotropy of turbulence. Moreover, sensible heat is transported more efficiently than water vapor; and transport efficiencies of these two scalars are separated in terms of their variability with the velocity aspect ratio. Compared with air temperature fluctuations, turbulence characteristics of the water vapor concentration are subject to a more pronounced modification because of distinct magnitudes of RF. An innovative method is employed for connecting quadrant analysis and cospectral analysis, so that the hyperbolic quadrant-hole size can be coupled to the natural frequency underlying the fast Fourier transform. Then, we introduce a hypothetical octant hole whose size is invoked as a metric for the amplitude scale of fluctuating scalar fluxes. The contributions to RF are quantified for a variety of eddy structures that are associated with different ranges of the amplitude scale. Regarding larger-amplitude fluxes due to heated drier air parcels in descending motions, reductions in RF correspond to increasing flux fractions for water vapor, whereas the flux fractions for sensible heat are largely unchanged. Overall, a more substantial portion of the changes in RF can be ascribed to smaller-amplitude fluxes due to cooled moister air parcels and heated drier air parcels being involved, respectively, in ascending and descending motions. Reductions in RF relate to the flux fractions of a decreasing magnitude for sensible heat but of an increasing magnitude for water vapor.HighlightsIn a stably stratified flow, dissimilar transport of sensible heat and water vapor is associated with anisotropy properties of turbulence.A new approach is developed for a scrutiny of scalar transport, whereby quadrant analysis and cospectral analysis can be interconnected.Extending octant analysis to scalar turbulence identifies eddy structures that exhibit distinct behaviors indicative of the flux dissimilarity.Comparatively small-amplitude fluxes are accountable for a substantial portion of the changes in the overall level of scalar flux correlation.
Author Hong, Jinkyu
Guo, Xiaofeng
Wang, Linlin
Zhou, Degang
Gao, Zhiqiu
Yang, Wei
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  orcidid: 0000-0002-2490-806X
  surname: Zhou
  fullname: Zhou, Degang
  organization: Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences
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CitedBy_id crossref_primary_10_1007_s10652_023_09950_0
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Octant analysis technique
Stably stratified boundary layer
Turbulent flux dissimilarity
Sensible heat and water vapor transport
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Snippet Based on eddy-covariance measurements over a glacier, we investigate the scalar flux dissimilarity between sensible heat and water vapor transport in a stably...
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SubjectTerms Air parcels
Air temperature
Amplitude
Amplitudes
Analysis
Anisotropy
Aspect ratio
Classical Mechanics
Connecting
Correlation coefficient
Correlation coefficients
Earth and Environmental Science
Earth Sciences
Eddy covariance
Enthalpy
Environmental Physics
Fast Fourier transformations
Fluctuations
Fluxes
Fourier transforms
Glacier measurements
Glaciers
Heat
Hole size
Hydrogeology
Hydrology/Water Resources
Oceanography
Original Article
Quadrants
Resonant frequencies
Resonant frequency
Scalars
Sensible heat
Stratified flow
Temperature fluctuations
Turbulence
Vortices
Water vapor
Water vapor flux
Water vapor transport
Water vapour
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Title Turbulence behaviors underlying the sensible heat and water vapor flux dissimilarity in a stably stratified flow
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