Coupling between radiative flux divergence and turbulence near the surface

Gentine, Pierre; Steeneveld, Gert‐Jan; Heusinkveld, Bert G.; Holtslag, Albert A. M.

doi:10.1002/qj.3333

Title: Coupling between radiative flux divergence and turbulence near the surface

Journal Article · 14 December 2018 · Quarterly Journal of the Royal Meteorological Society

DOI: https://doi.org/10.1002/qj.3333 · OSTI ID:1487156

^[1];

^[2]; Heusinkveld, Bert G. ^[2]; Holtslag, Albert A. M. ^[2]

Earth and Environmental Engineering, Earth Institute Columbia University New York New York
Meteorology and Air Quality Section Wageningen University Wageningen The Netherlands

Near‐surface turbulent flux and radiation divergence field observations are analysed over a grass‐covered surface located at the Wageningen observatory, the Netherlands. Net radiative flux divergence appears to be a large component of the energy budget near the surface, accounting for a cooling rate of several tens of degrees per day. Long‐wave radiation divergence dominates this radiation divergence flux. We show here that long‐wave flux divergence near the surface is strongly coupled to sensible heat flux, except in high relative humidity (>90%) and foggy conditions. The net long‐wave radiative flux divergence exhibits a sharp gradient within the first 20 m above the surface. This flux divergence is itself strongly coupled to sensible heat flux through adjustments in surface‐layer profiles. Nonetheless, no systematic effect of radiation is witnessed on the turbulent temperature spectrum so that the main effect of near‐surface radiation is on the mean heat budget. As typical flux‐gradient relationships are derived based on observations taken in the near‐surface boundary‐layer region where sharp long‐wave divergence is present, we suspect that those relationships implicitly represent some of the long‐wave divergence term. A modification of Monin–Obukhov Similarity Theory to include the effect of radiative divergence is proposed and discussed. This calls for independent measurements of turbulent fluxes and radiative flux divergence near the surface to re‐derive turbulent flux‐gradient relationships independently of radiative effects.

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Sponsoring Organization:: USDOE

OSTI ID:: 1487156

Journal Information:: Quarterly Journal of the Royal Meteorological Society, Journal Name: Quarterly Journal of the Royal Meteorological Society Vol. 144 Journal Issue: 717; ISSN 0035-9009

Publisher:: Wiley Blackwell (John Wiley & Sons)Copyright Statement

Country of Publication:: United Kingdom

Language:: English

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Cited by: 7 works

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