Study of water vapor vertical variability ...
Document type :
Article dans une revue scientifique: Article original
DOI :
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Title :
Study of water vapor vertical variability and possible cloud formation with a small network of GPS stations
Author(s) :
Van Baelen, Joël [Auteur]
Laboratoire de météorologie physique [LaMP]
Penide, Guillaume [Auteur]
Laboratoire de météorologie physique [LaMP]
Laboratoire de météorologie physique [LaMP]
Penide, Guillaume [Auteur]
Laboratoire de météorologie physique [LaMP]
Journal title :
Geophysical Research Letters
Abbreviated title :
Geophysical Research Letters
Volume number :
36
Publisher :
American Geophysical Union (AGU)
Publication date :
2009-01
HAL domain(s) :
Planète et Univers [physics]/Océan, Atmosphère
English abstract : [en]
During a short experiment we have investigated the vertical variability of water vapor in the lower part of the atmosphere with the help of small network of GPS stations positioned on the eastern slopes of the Puy de Dôme ...
Show more >During a short experiment we have investigated the vertical variability of water vapor in the lower part of the atmosphere with the help of small network of GPS stations positioned on the eastern slopes of the Puy de Dôme in central France. We have found out that the urban layer exhibits somewhat constant water vapor content. In contrast, the major IWV variations arise in the upper troposphere level, in particular in the presence of westerly flows that bring elevated water vapor content over the mountain ridge. Finally, the transition layer situated between these lower and upper levels presents quite variable water vapor content, acting as a buffer zone for the boundary layer. Comparing two episodes of higher water vapor contents, one being associated with a sharp frontal passage, we have shown that the contrasted behavior of the different layers revealed the possible formation of clouds before the advent of rain.Show less >
Show more >During a short experiment we have investigated the vertical variability of water vapor in the lower part of the atmosphere with the help of small network of GPS stations positioned on the eastern slopes of the Puy de Dôme in central France. We have found out that the urban layer exhibits somewhat constant water vapor content. In contrast, the major IWV variations arise in the upper troposphere level, in particular in the presence of westerly flows that bring elevated water vapor content over the mountain ridge. Finally, the transition layer situated between these lower and upper levels presents quite variable water vapor content, acting as a buffer zone for the boundary layer. Comparing two episodes of higher water vapor contents, one being associated with a sharp frontal passage, we have shown that the contrasted behavior of the different layers revealed the possible formation of clouds before the advent of rain.Show less >
Language :
Anglais
Peer reviewed article :
Oui
Audience :
Internationale
Popular science :
Non
Administrative institution(s) :
Université de Lille
CNRS
CNRS
Collections :
Research team(s) :
Interactions Rayonnement Nuages (IRN)
Submission date :
2024-01-10T15:48:23Z
2024-02-23T11:31:13Z
2024-02-23T11:31:13Z
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