Zobrazeno 1 - 10
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pro vyhledávání: '"G. Dubosclard"'
Autor:
Eugenio Privitera, R. Cordesses, G. Dubosclard, Franck Donnadieu, Mauro Coltelli, Patrick Allard, J. Kornprobst, C. Hervier
Publikováno v:
Bulletin of Volcanology. 66:443-456
Besides their common use in atmospheric studies, Doppler radars are promising tools for the active remote sensing of volcanic eruptions but were little applied to this field. We present the observations made with a mid-power UHF Doppler radar (Voldor
Autor:
J. G. Van Der Vliet, Aimé Druilhet, M. Masmoudi, J. Y. Caneil, M. Crochet, O. Taconet, R. Bernard, W. A. A. Monna, A. C. M. Beljaars, Christine Mazaudier, D. Vidal Madjar, B. S. Gera, A. Weill, P. Durand, Dennis W. Thomson, A. Sauvaget, T. Carlson, C. Klapisz, G. Dubosclard, F. Leca, P. Mery, F. Baudin
Publikováno v:
Boundary-Layer Meteorology. 42:251-264
During the MESOGERS 84 experiment in SW France from September 10 to October 5, 1984, different aspects of the Atmospheric Boundary Layer over complex terrain were investigated using a regional meteorological network, two instrumented aircraft and a D
étude expérimentale de la couche limite au-dessus d'un relief modéré proche d'une chaîne de montagne
Publikováno v:
Boundary-Layer Meteorology. 25:3-16
Publikováno v:
Boundary-Layer Meteorology. 24:395-414
The characteristics of the boundary layer over complex terrain (Lannemezan - lat.: 43.7° N and, long.: 0.7 ° E) are analyzed for various scales, using measurements obtained during the COCAGNE Experiment. In this first part, the dynamic characterist
Autor:
G. Dubosclard
Publikováno v:
Boundary-Layer Meteorology. 22:325-334
From sodar measurements gathered during the Voves experiment (France, summer 1977), the variations of the temperature structure parameter CT2 were studied in the morning planetary boundary layer. Dimensionless profiles of CT2 are consistent with the
�tude exp�rimentale de la couche limite au-dessus d'un relief mod�r� proche d'une cha�ne de montagne
Publikováno v:
Boundary-Layer Meteorology. 25:107-119
For the heterogeneous site described in the first part, some aspects of the turbulent structure of the planetary boundary layer are studied. Using mixed-layer scaling, the normalized profiles are compared with those obtained over flat terrain during
Publikováno v:
Journal de Physique. 29:839-851
L'etude theorique des structures hyperfines en champ faible (transitions « π », Δm = ± 1, induites lorsque le champ radiofrequence est perpendiculaire au champ continu, et transitions « σ », Δm = 0, induites lorsque ces deux champs sont para
Autor:
Timothy H. Druitt, C. Hervier, Jean-François Lénat, G. Dubosclard, Patrick Allard, J. Kornprobst, Mauro Coltelli, Franck Donnadieu, R. Cordesses
Publikováno v:
Scopus-Elsevier
Eos, Transactions American Geophysical Union
Eos, Transactions American Geophysical Union, 2005, 86 (21), pp.201. ⟨10.1029/2005EO210001⟩
Eos, Transactions American Geophysical Union
Eos, Transactions American Geophysical Union, 2005, 86 (21), pp.201. ⟨10.1029/2005EO210001⟩
Concern about hazards that volcanic plumes pose, especially to aviation safety, has led scientists for about two decades to use satellite sensors in different wavelengths for the detection and study of volcanic activity. Together with ground-based me
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