Is There a Scalar Atmospheric Surface Layer Within a Convective Boundary Layer? Implications for Flux Measurements

Abstract Top‐down entrainment shapes the vertical gradients of sensible heat, latent heat, and CO2 fluxes, influencing the interpretation of eddy covariance (EC) measurements in the unstable atmospheric surface layer (ASL). Using large eddy simulations for convective boundary layer flows, we demonst...

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Hlavní autoři:	Heping Liu, Cheng Liu, Yanzhao Zhou, Qianyu Zhang, Ankur R. Desai, Khaled Ghannam, Jianping Huang, Gabriel G. Katul
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Wiley 2025-03-01
Edice:	Geophysical Research Letters
Témata:	eddy covariance fluxes of scalars entrainment processes flux vertical gradients large eddy simulations non‐closure of surface energy balance
On-line přístup:	https://doi.org/10.1029/2024GL112619
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