1. Katabatic Winds over Steep Slopes: Overview of a Field Experiment Designed to Investigate Slope-Normal Velocity and Near-Surface Turbulence
- Author
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Catherine Coulaud, Claudine Charrondière, Hélène Guyard, Jean-Martial Cohard, Martin Obligado, Romain Biron, Jean-Emmanuel Sicart, Christophe Brun, Laboratoire des Écoulements Géophysiques et Industriels [Grenoble] (LEGI), Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), Institut des Géosciences de l’Environnement (IGE), and Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )
- Subjects
Atmospheric Science ,Katabatic wind ,010504 meteorology & atmospheric sciences ,Near-surface turbulence ,Reynolds stress ,[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology ,01 natural sciences ,010305 fluids & plasmas ,Physics::Fluid Dynamics ,Katabatic jet ,0103 physical sciences ,ComputingMilieux_MISCELLANEOUS ,0105 earth and related environmental sciences ,[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere ,Jet (fluid) ,Turbulence ,[SPI.FLUID]Engineering Sciences [physics]/Reactive fluid environment ,Mechanics ,Dissipation ,Entrainment (meteorology) ,Field experiment ,Boundary layer ,Dissipative system ,Steep alpine slope ,Geology ,Slope-normal velocity - Abstract
We describe a new field campaign over a steep, snowy $$30^{\circ }$$ alpine slope, designed to investigate three recurrent issues in experimental studies of steep-slope katabatic winds. (1) Entrainment is known to be present in katabatic jets and has been estimated at the interface between the jet and the boundary layer above it. However, to our knowledge, the slope-normal velocity component has never been measured in the katabatic jet. (2) It is hard to accurately measure turbulence in the first tens of centimetres above the surface using standard sonic anemometry due to the filtering effect of the long instrument path. The present field experiment used a three-dimensional multi-hole pitot-type probe with a high sampling frequency (1250 Hz) that was positioned as close to the surface as 3 cm. It provides three-dimensional mean velocity and Reynolds stress tensor from which dissipation can be estimated, as well as spectra for the turbulent quantities. Energy spectra reveal a well-developed inertial range and capture the inertial scales and some of the dissipative scales. (3) Measuring turbulence on a mast usually provides information about mean and turbulent quantities at certain discrete heights because the sensors are sparsely located inside the jet. We present the first measurements of well-developed katabatic flows where the full wind-speed and temperature profiles acquired, from tethered balloon are available at the location of the measurement mast, which comprises three-dimensional anemometry and thermometry.
- Published
- 2022
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