The alpine mountain-plain circulation "Alpine Pumping": Airborne Doppler lidar observations at 2μm and 10.6 μm and MM5 simulations

Oliver Reitebuch; Alain Dabas; Patricia Delville; Philippe Drobinski; Leonhard Gantner; Stephan Rahm; Martin Weissmann

The alpine mountain-plain circulation "Alpine Pumping": Airborne Doppler lidar observations at 2μm and 10.6 μm and MM5 simulations

Oliver Reitebuch
, Alain Dabas
, Patricia Delville
, Philippe Drobinski
, Leonhard Gantner
, Stephan Rahm
, Martin Weissmann

DLR
Météo-France/CNRS
Division Technique
Sorbonne Université
Universität München

Résultats de recherche: Contribution à un journal › Article › Revue par des pairs

Résumé

A mesoscale advection towards the Alps and vertical transport above the Alps usually develops during fair weather conditions ("Alpine Pumping"). The field experiment VERTIKATOR (Vertical Exchange and Orography) was conducted in June/July 2002 in the Alps to study the development of this mountain-plain circulation and the initiation of convection and thunderstorms. Observations from the airborne 10.6 μm Doppler lidar WIND and the airborne 2μm Doppler lidar are presented together with numerical simulations. Observations and simulations could quantify the mass flux from the forelands to the Alps.

langue originale	Anglais
Pages (de - à)	747-750
Nombre de pages	4
journal	European Space Agency, (Special Publication) ESA SP
Volume	2
Numéro de publication	561
état	Publié - 1 juin 2004
Modification externe	Oui

Contient cette citation

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title = "The alpine mountain-plain circulation {"}Alpine Pumping{"}: Airborne Doppler lidar observations at 2μm and 10.6 μm and MM5 simulations",

abstract = "A mesoscale advection towards the Alps and vertical transport above the Alps usually develops during fair weather conditions ({"}Alpine Pumping{"}). The field experiment VERTIKATOR (Vertical Exchange and Orography) was conducted in June/July 2002 in the Alps to study the development of this mountain-plain circulation and the initiation of convection and thunderstorms. Observations from the airborne 10.6 μm Doppler lidar WIND and the airborne 2μm Doppler lidar are presented together with numerical simulations. Observations and simulations could quantify the mass flux from the forelands to the Alps.",

author = "Oliver Reitebuch and Alain Dabas and Patricia Delville and Philippe Drobinski and Leonhard Gantner and Stephan Rahm and Martin Weissmann",

year = "2004",

month = jun,

day = "1",

language = "English",

volume = "2",

pages = "747--750",

journal = "European Space Agency, (Special Publication) ESA SP",

issn = "0379-6566",

number = "561",

}

The alpine mountain-plain circulation "Alpine Pumping": Airborne Doppler lidar observations at 2μm and 10.6 μm and MM5 simulations. / Reitebuch, Oliver; Dabas, Alain; Delville, Patricia et al.
Dans: European Space Agency, (Special Publication) ESA SP, Vol 2, Numéro 561, 01.06.2004, p. 747-750.

Résultats de recherche: Contribution à un journal › Article › Revue par des pairs

TY - JOUR

T1 - The alpine mountain-plain circulation "Alpine Pumping"

T2 - Airborne Doppler lidar observations at 2μm and 10.6 μm and MM5 simulations

AU - Reitebuch, Oliver

AU - Dabas, Alain

AU - Delville, Patricia

AU - Drobinski, Philippe

AU - Gantner, Leonhard

AU - Rahm, Stephan

AU - Weissmann, Martin

PY - 2004/6/1

Y1 - 2004/6/1

N2 - A mesoscale advection towards the Alps and vertical transport above the Alps usually develops during fair weather conditions ("Alpine Pumping"). The field experiment VERTIKATOR (Vertical Exchange and Orography) was conducted in June/July 2002 in the Alps to study the development of this mountain-plain circulation and the initiation of convection and thunderstorms. Observations from the airborne 10.6 μm Doppler lidar WIND and the airborne 2μm Doppler lidar are presented together with numerical simulations. Observations and simulations could quantify the mass flux from the forelands to the Alps.

AB - A mesoscale advection towards the Alps and vertical transport above the Alps usually develops during fair weather conditions ("Alpine Pumping"). The field experiment VERTIKATOR (Vertical Exchange and Orography) was conducted in June/July 2002 in the Alps to study the development of this mountain-plain circulation and the initiation of convection and thunderstorms. Observations from the airborne 10.6 μm Doppler lidar WIND and the airborne 2μm Doppler lidar are presented together with numerical simulations. Observations and simulations could quantify the mass flux from the forelands to the Alps.

M3 - Article

AN - SCOPUS:3142577034

SN - 0379-6566

VL - 2

SP - 747

EP - 750

JO - European Space Agency, (Special Publication) ESA SP

JF - European Space Agency, (Special Publication) ESA SP

IS - 561

ER -

The alpine mountain-plain circulation "Alpine Pumping": Airborne Doppler lidar observations at 2μm and 10.6 μm and MM5 simulations

Résumé

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