Trajectory derived from the 3D linear wind field retrieved by a wind-profiler mesoscale network

B. Campistron; V. Puygrenier; B. Bénech; F. Lohou; F. Saïd; C. Moppert; F. Cousin; E. Dupont

Trajectory derived from the 3D linear wind field retrieved by a wind-profiler mesoscale network

B. Campistron
, V. Puygrenier
, B. Bénech
, F. Lohou
, F. Saïd
, C. Moppert
, F. Cousin
, E. Dupont

Research output: Contribution to conference › Paper › peer-review

Abstract

A methodology, based on the measurements made by a UHF wind-profiler mesoscale network, which retrieves the three-dimensional (3D) wind field used to derive any type of air parcel trajectories, is presented. The technique is applied t o observations collected during the ESCOMPTE campagin, related to pollution studies. Turbulence that prevails in the ABL tends to quickly remove the identity of air parcels, which is the basic assumption for the trajectory construction. A strong rotation on the balloon trajectory was observed which was induced there is an important temporal and spatial change of the wind.

Original language	English
Pages	745-749
Number of pages	5
Publication status	Published - 1 Dec 2004
Externally published	Yes
Event	16th Symposium on Boundary Layers and Turbulence - Portland, ME, United States Duration: 9 Aug 2004 → 13 Aug 2004

Conference

Conference	16th Symposium on Boundary Layers and Turbulence
Country/Territory	United States
City	Portland, ME
Period	9/08/04 → 13/08/04

Cite this

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title = "Trajectory derived from the 3D linear wind field retrieved by a wind-profiler mesoscale network",

abstract = "A methodology, based on the measurements made by a UHF wind-profiler mesoscale network, which retrieves the three-dimensional (3D) wind field used to derive any type of air parcel trajectories, is presented. The technique is applied t o observations collected during the ESCOMPTE campagin, related to pollution studies. Turbulence that prevails in the ABL tends to quickly remove the identity of air parcels, which is the basic assumption for the trajectory construction. A strong rotation on the balloon trajectory was observed which was induced there is an important temporal and spatial change of the wind.",

author = "B. Campistron and V. Puygrenier and B. B{\'e}nech and F. Lohou and F. Sa{\"i}d and C. Moppert and F. Cousin and E. Dupont",

year = "2004",

month = dec,

day = "1",

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pages = "745--749",

note = "16th Symposium on Boundary Layers and Turbulence ; Conference date: 09-08-2004 Through 13-08-2004",

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TY - CONF

T1 - Trajectory derived from the 3D linear wind field retrieved by a wind-profiler mesoscale network

AU - Campistron, B.

AU - Puygrenier, V.

AU - Bénech, B.

AU - Lohou, F.

AU - Saïd, F.

AU - Moppert, C.

AU - Cousin, F.

AU - Dupont, E.

PY - 2004/12/1

Y1 - 2004/12/1

N2 - A methodology, based on the measurements made by a UHF wind-profiler mesoscale network, which retrieves the three-dimensional (3D) wind field used to derive any type of air parcel trajectories, is presented. The technique is applied t o observations collected during the ESCOMPTE campagin, related to pollution studies. Turbulence that prevails in the ABL tends to quickly remove the identity of air parcels, which is the basic assumption for the trajectory construction. A strong rotation on the balloon trajectory was observed which was induced there is an important temporal and spatial change of the wind.

AB - A methodology, based on the measurements made by a UHF wind-profiler mesoscale network, which retrieves the three-dimensional (3D) wind field used to derive any type of air parcel trajectories, is presented. The technique is applied t o observations collected during the ESCOMPTE campagin, related to pollution studies. Turbulence that prevails in the ABL tends to quickly remove the identity of air parcels, which is the basic assumption for the trajectory construction. A strong rotation on the balloon trajectory was observed which was induced there is an important temporal and spatial change of the wind.

UR - https://www.scopus.com/pages/publications/23744487359

M3 - Paper

AN - SCOPUS:23744487359

SP - 745

EP - 749

T2 - 16th Symposium on Boundary Layers and Turbulence

Y2 - 9 August 2004 through 13 August 2004

ER -

Trajectory derived from the 3D linear wind field retrieved by a wind-profiler mesoscale network

Abstract

Conference

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