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Journal ArticleDOI

The CRPE minisodar: Applications in micrometeorology and in physics of precipitations

A. Weill, +2 more
- 01 Dec 1986 - 
- Vol. 20, Iss: 2, pp 317-333
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TLDR
In this paper, the technical characteristics of the CRPE minisodar are described and compared with the classical Doppler sodar, and simple methods are demonstrated for estimating the sensible heat flux and friction velocity in the surface layer.
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This article is published in Atmospheric Research.The article was published on 1986-12-01. It has received 29 citations till now. The article focuses on the topics: SODAR & Wind shear.

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Citations
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A case study of turbulence in the stable nocturnal boundary layer

TL;DR: In this paper, the authors measured and analyzed vertical profiles of vertical velocity standard deviation, dissipation rate, and temperature variance destruction rate in the nocturnal boundary layer (NBL) according to levels of turbulence activity.
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Acoustic sounder measurements of the vertical velocity of volcanic jets at Stromboli Volcano

TL;DR: In this paper, the authors used a Sodar (acoustic doppler sounder) to characterize the behavior of volcanoes, and in particular, to measure the vertical velocities of volcanic jets.
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The role of acoustic sounding in a high-technology era.

TL;DR: In this paper, a brief synopsis of past, current and anticipated progress and problems in the use of acoustic remote sensing for basic and applied research of the lower atmosphere is presented, where the potential and reality of the sodar for determination of meteorological parameters and turbulence characteristics is discussed.
Book

Acoustic Remote Sensing Applications

S. P. Singal
TL;DR: In this article, the authors present the physical grounds for acoustic remote sensing of the Atmospheric Boundary Layer and the development of Atmospheric Echosounders Sodar Detection and its Application Ocean Acoustics and Instrumentation.
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Similarity methods to derive turbulence quantities and mixed-layer depth from SODAR measurements in the convective boundary layer: A review

TL;DR: In this article, a brief review of similarity methods which have been developed to calculate turbulence parameters and mixed-layer depth from SODAR measurements is made, where a variety of parametric relations valid in the convective boundary layer are surveyed.
References
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Journal ArticleDOI

Flux-Profile Relationships in the Atmospheric Surface Layer

TL;DR: In this article, the free constants in several interpolation formulas can be adjusted to give excellent fits to the wind and temperature gradient data, and the behavior of the gradients under neutral conditions is unusual, however, and indicates that von Karman's constant is ∼0.35, rather than 0.40 as usually assumed, and that the ratio of eddy diffusivities for heat and momentum at neutrality is ∼1.0.
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The Mathematical Representation of Wind Speed and Temperature Profiles in the Unstable Atmospheric Surface Layer

TL;DR: In this article, analytical expressions which specify non-dimensionalized wind speed and potential temperature gradients as functions of stability are integrated with Swinhank's wind and temperature profiles measured at Kerang, Australia.
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Advances in atmospheric acoustics

TL;DR: A detailed review of developments in atmospheric acoustics of the last decade is given in this paper, which includes new ways to use refractive effects, studies of phase and amplitude fluctuations during propagation of sound along a path, nonlinear effects near high-powered acoustic antennas, problems related to noise, insights into large-scale atmospheric processes gained from infrasound, applications dependent on the Doppler frequency shift, and hybrid devices using both acoustic and electromagnetic waves.
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The Birth of “CAT” and Microscale Turbulence

TL;DR: In this paper, a 2m radar image was used to study the life cycle of clear air turbulence and showed the amplification of unstable Kelvin-Helmholtz (KH) waves, the development of roll vortices, their breaking and resulting turbulence.
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Acoustic sounding of the lower troposphere

TL;DR: In this article, an acoustic sounding experiment is described in which pulses of acoustic energy were directed upwards and reflected from inhomogeneities in the temperature structure of the lower troposphere to obtain a continuous record of their height, movement, and vertical distribution.
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