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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Главные авторы:	Heping Liu, Cheng Liu, Yanzhao Zhou, Qianyu Zhang, Ankur R. Desai, Khaled Ghannam, Jianping Huang, Gabriel G. Katul
Формат:	Artigo
Язык:	Inglês
Опубликовано:	Wiley 2025-03-01
Серии:	Geophysical Research Letters
Предметы:	eddy covariance fluxes of scalars entrainment processes flux vertical gradients large eddy simulations non‐closure of surface energy balance
Online-ссылка:	https://doi.org/10.1029/2024GL112619
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