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The Heat-Flux Imbalance: The Role of Advection and Dispersive Fluxes on Heat Transport Over Thermally Heterogeneous Terrain
by
Pardyjak, Eric R
, Morrison, Travis
, Calaf Marc
, Mauder Matthias
in
Advection
/ Air temperature
/ Dispersion
/ Energy balance
/ Fluctuations
/ Heat
/ Heat flux
/ Heat transfer
/ Heat transport
/ Heterogeneity
/ Numerical prediction
/ Patchiness
/ Prediction models
/ Spatial heterogeneity
/ Surface energy
/ Surface energy balance
/ Surface properties
/ Temperature
/ Turbulence
/ Wind speed
2022
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The Heat-Flux Imbalance: The Role of Advection and Dispersive Fluxes on Heat Transport Over Thermally Heterogeneous Terrain
by
Pardyjak, Eric R
, Morrison, Travis
, Calaf Marc
, Mauder Matthias
in
Advection
/ Air temperature
/ Dispersion
/ Energy balance
/ Fluctuations
/ Heat
/ Heat flux
/ Heat transfer
/ Heat transport
/ Heterogeneity
/ Numerical prediction
/ Patchiness
/ Prediction models
/ Spatial heterogeneity
/ Surface energy
/ Surface energy balance
/ Surface properties
/ Temperature
/ Turbulence
/ Wind speed
2022
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The Heat-Flux Imbalance: The Role of Advection and Dispersive Fluxes on Heat Transport Over Thermally Heterogeneous Terrain
by
Pardyjak, Eric R
, Morrison, Travis
, Calaf Marc
, Mauder Matthias
in
Advection
/ Air temperature
/ Dispersion
/ Energy balance
/ Fluctuations
/ Heat
/ Heat flux
/ Heat transfer
/ Heat transport
/ Heterogeneity
/ Numerical prediction
/ Patchiness
/ Prediction models
/ Spatial heterogeneity
/ Surface energy
/ Surface energy balance
/ Surface properties
/ Temperature
/ Turbulence
/ Wind speed
2022
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The Heat-Flux Imbalance: The Role of Advection and Dispersive Fluxes on Heat Transport Over Thermally Heterogeneous Terrain
Journal Article
The Heat-Flux Imbalance: The Role of Advection and Dispersive Fluxes on Heat Transport Over Thermally Heterogeneous Terrain
2022
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Overview
Data from the Idealized Planar-Array experiment for Quantifying Spatial heterogeneity are used to perform a control volume analysis (400 × 400 × 2 m3) on the total derivative of the temperature tendency equation. Analysis of the heat-flux imbalance, which is defined as the ratio of the sum of advective, dispersive, and turbulence-flux terms to the turbulence-flux term, are presented. Results are divided amongst free-convective and forced-convective days, as well as high-wind-speed and quiescent nocturnal periods. Findings show that the median flux imbalance is greater on forced-convective days (a 168% turbulence-flux overestimation, or relative importance of the advection to dispersive flux to the turbulence flux) when compared to free-convective periods (79% turbulence-flux overestimation). During nocturnal periods, a median turbulence-flux underestimation of 146% exists for quiescent nights and a 43% underestimation of the flux for high-wind-speed nights. These results support the existing literature, suggesting that mean air-temperature heterogeneities lead to strong bulk advection and dispersive fluxes. A discussion of the impact of the flux imbalance on the surface energy balance and numerical-weather-prediction modelling is presented.
Publisher
Springer Nature B.V
Subject
/ Heat
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