Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Thibault Vaillant de Guélis"'
Autor:
Thibault Vaillant de Guélis, Gérard Ancellet, Anne Garnier, Laurent C.-Labonnote, Jacques Pelon, Mark A. Vaughan, Zhaoyan Liu, David M. Winker
Publikováno v:
Atmospheric Measurement Techniques
Atmospheric Measurement Techniques, 2022, 15 (6), pp.1931-1956. ⟨10.5194/amt-15-1931-2022⟩
Atmospheric Measurement Techniques, 2022, 15 (6), pp.1931-1956. ⟨10.5194/amt-15-1931-2022⟩
The features detected in monolayer atmospheric columns sounded by the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) and classified as cloud or aerosol layers by the CALIOP version 4 (V4) cloud and aerosol discrimination (CAD) algorithm ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eab78dc885c4e781fb542bf434e9c43d
https://hal-insu.archives-ouvertes.fr/insu-03483413
https://hal-insu.archives-ouvertes.fr/insu-03483413
Autor:
Assia Arouf, Hélène Chepfer, Thibault Vaillant de Guélis, Marjolaine Chiriaco, Matthew D. Shupe, Rodrigo Guzman, Artem Feofilov, Patrick Raberanto, Tristan S. L'Ecuyer, Seiji Kato, Michael R. Gallagher
Publikováno v:
Atmospheric Measurement Techniques Discussions
Atmospheric Measurement Techniques Discussions, Copernicus Publications / European Geosciences Union 2022, ⟨10.5194/amt-2021-392⟩
Atmospheric Measurement Techniques Discussions, Copernicus Publications / European Geosciences Union 2022, ⟨10.5194/amt-2021-392⟩
Clouds warm the surface in the longwave (LW), and this warming effect can be quantified through the surface LW cloud radiative effect (CRE). The global surface LW CRE has been estimated over more than 2 decades using space-based radiometers (2000–2
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a4f1aee14b94db632b85da8d02bf6693
https://amt.copernicus.org/preprints/amt-2021-392/
https://amt.copernicus.org/preprints/amt-2021-392/
Autor:
Thibault Vaillant de Guélis, Gérard Ancellet, Anne Garnier, Laurent C.-Labonnote, Jacques Pelon, Mark A. Vaughan, Zhaoyan Liu, David M. Winker
Publikováno v:
Atmospheric Measurement Techniques Discussions
Atmospheric Measurement Techniques Discussions, Copernicus Publications / European Geosciences Union 2022, pp.(Discussions). ⟨10.5194/amt-2021-419⟩
Atmospheric Measurement Techniques Discussions, Copernicus Publications / European Geosciences Union 2022, pp.(Discussions). ⟨10.5194/amt-2021-419⟩
The features detected in monolayer atmospheric columns sounded by the Cloud and Aerosol Lidar with Orthogonal Polarization (CALIOP) and classified as cloud or aerosol layers by the CALIOP version 4 (V4) cloud and aerosol discrimination (CAD) algorith
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7a9785df56962c01542b23a529c1299c
https://amt.copernicus.org/preprints/amt-2021-419/
https://amt.copernicus.org/preprints/amt-2021-419/
Autor:
Thibault Vaillant de Guélis, David M. Winker, Vincent Noel, Marine Bonazzola, Rodrigo Guzman, Hélène Chepfer
Publikováno v:
Scientific Reports
Scientific Reports, Vol 10, Iss 1, Pp 1-2 (2020)
Scientific Reports, Vol 10, Iss 1, Pp 1-2 (2020)
Some of the most challenging questions in atmospheric science relate to how clouds will respond as the climate warms. On centennial scales, the response of clouds could either weaken or enhance the warming due to greenhouse gas emissions. Here we use
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a77a46236eadcd5825bbca62005bb0aa
https://doi.org/10.1038/s41598-020-74323-2
https://doi.org/10.1038/s41598-020-74323-2
Publikováno v:
Optics Express
Optics Express, Optical Society of America-OSA Publishing, 2019, 27 (7), pp.9372-9381. ⟨10.1364/OE.27.009372⟩
Optics Express, 2019, 27 (7), pp.9372-9381. ⟨10.1364/OE.27.009372⟩
Optics Express, Optical Society of America-OSA Publishing, 2019, 27 (7), pp.9372-9381. ⟨10.1364/OE.27.009372⟩
Optics Express, 2019, 27 (7), pp.9372-9381. ⟨10.1364/OE.27.009372⟩
International audience; The Maggi-Rubinowicz method (MRM) is a useful tool to compute diffraction patterns from opaque planar objects. We adapted the MRM to planar rectangles. In the first part of this study, differences between diffraction patterns,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fa637b8e5a746229136a260388668bc1
https://pubmed.ncbi.nlm.nih.gov/31045089
https://pubmed.ncbi.nlm.nih.gov/31045089
Autor:
Thibault Vaillant de Guélis, Alfons Schwarzenböck, Valery Shcherbakov, Christophe Gourbeyre, Bastien Laurent, Régis Dupuy, Pierre Coutris, Christophe Duroure
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8518310ccd73fca41db59cd584b7870e
https://doi.org/10.5194/amt-2018-437-supplement
https://doi.org/10.5194/amt-2018-437-supplement
Autor:
Thibault Vaillant de Guélis, Alfons Schwarzenböck, Valery Shcherbakov, Christophe Gourbeyre, Bastien Laurent, Régis Dupuy, Pierre Coutris, Christophe Duroure
Optical array probes (OAPs) are classical instrumental means to derive shape, size, and number concentration of cloud and precipitation particles from 2D images. However, recorded 2D images are subject to distortion based on the diffraction of light
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a426fd4131eebc637a7e692e0af4731c
https://doi.org/10.5194/amt-2018-437
https://doi.org/10.5194/amt-2018-437