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Organised motion and radiative perturbations in the nocturnal canopy sublayer above an even-aged pine forest

Publication ,  Journal Article
Cava, D; Giostra, U; Siqueira, M; Katul, G
Published in: Boundary-Layer Meteorology
July 1, 2004

Using time series measurements of velocity, carbon dioxide and water vapour concentration, and temperature collected just above a 15 m tall even-aged pine forest, we quantify the role of organized motion on scalar and momentum transport within the nocturnal canopy sublayer (CSL). We propose a framework in which the nocturnal CSL has two end-members, both dominated by organised motion. These end-members represent fully developed turbulent flows at near-neutral or slightly stable stratification and no turbulence for very stable stratification. Our analysis suggests that ramps dominate scalar transport for near-neutral and slightly stable conditions, while linear canopy waves dominate the flow dynamics for very stable conditions. For intermediate stability, the turbulence is highly damped and often dominated by fine scale motions. Co-spectral analysis suggests that ramps are the most efficient net scalar mass-transporting agent while linear canopy waves contribute little to net scalar transport between the canopy and atmosphere for averaging intervals that include complete wave cycles. However, canopy waves significantly contribute to the spectral properties of the scalar time series. Ramps are the most frequently occurring organised motion in the nocturnal CSL for this site. Numerous night-time runs, however, resided between these two end-members. Our analysis suggests that when radiative perturbations are sufficient large (>20 W m-2 in net radiation), the flow can switch from being highly damped fine-scale turbulence to being organized with ramp-like properties. We also found that when ramps are already the dominant eddy motion in the nocturnal CSL, radiative perturbations have a minor impact on scalar transport. Finally, in agreement with previous studies, we found that ramps and canopy waves have comparable length scales of about 30-60 metres. Consequences to night-time flux averaging are also discussed. © 2004 Kluwer Academic Publishers.

Duke Scholars

Published In

Boundary-Layer Meteorology

DOI

ISSN

0006-8314

Publication Date

July 1, 2004

Volume

112

Issue

1

Start / End Page

129 / 157

Related Subject Headings

  • Meteorology & Atmospheric Sciences
  • 3701 Atmospheric sciences
  • 0401 Atmospheric Sciences
 

Citation

APA
Chicago
ICMJE
MLA
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Cava, D., Giostra, U., Siqueira, M., & Katul, G. (2004). Organised motion and radiative perturbations in the nocturnal canopy sublayer above an even-aged pine forest. Boundary-Layer Meteorology, 112(1), 129–157. https://doi.org/10.1023/B:BOUN.0000020160.28184.a0
Cava, D., U. Giostra, M. Siqueira, and G. Katul. “Organised motion and radiative perturbations in the nocturnal canopy sublayer above an even-aged pine forest.” Boundary-Layer Meteorology 112, no. 1 (July 1, 2004): 129–57. https://doi.org/10.1023/B:BOUN.0000020160.28184.a0.
Cava D, Giostra U, Siqueira M, Katul G. Organised motion and radiative perturbations in the nocturnal canopy sublayer above an even-aged pine forest. Boundary-Layer Meteorology. 2004 Jul 1;112(1):129–57.
Cava, D., et al. “Organised motion and radiative perturbations in the nocturnal canopy sublayer above an even-aged pine forest.” Boundary-Layer Meteorology, vol. 112, no. 1, July 2004, pp. 129–57. Scopus, doi:10.1023/B:BOUN.0000020160.28184.a0.
Cava D, Giostra U, Siqueira M, Katul G. Organised motion and radiative perturbations in the nocturnal canopy sublayer above an even-aged pine forest. Boundary-Layer Meteorology. 2004 Jul 1;112(1):129–157.
Journal cover image

Published In

Boundary-Layer Meteorology

DOI

ISSN

0006-8314

Publication Date

July 1, 2004

Volume

112

Issue

1

Start / End Page

129 / 157

Related Subject Headings

  • Meteorology & Atmospheric Sciences
  • 3701 Atmospheric sciences
  • 0401 Atmospheric Sciences