Zobrazeno 1 - 10
of 91
pro vyhledávání: '"Scoccione A."'
Autor:
Dionisi D., Iannarelli A.M., Scoccione A., Liberti G.L., Cacciani M., Argentini S., Baldini L., Barnaba F., Campanelli M., Casasanta G., Diémoz H., Di Liberto L., Gobbi G.P., Petenko I., Siani A.M., Von Bismarck J., Casadio S.
Publikováno v:
EPJ Web of Conferences, Vol 176, p 05050 (2018)
A joint instrumental Super Site, combining observation in urban (“Sapienza” University) and semi-rural (ESA-ESRIN and CNR-ISAC) environment, for atmospheric studies and satellites Cal/Val activities, has been set-up in the Rome area (Italy). Grou
Externí odkaz:
https://doaj.org/article/fb427fe452ef44d390ea9d7f3ec3ef55
Publikováno v:
Atmospheric Measurement Techniques, Vol 12, Pp 2183-2199 (2019)
Vertical profiles of the particle backscattering coefficient at 355, 532 and 1064 nm measured by the University of Basilicata Raman lidar system (BASIL) have been compared with simulated particle backscatter profiles obtained through a Mie scatteri
Externí odkaz:
https://doaj.org/article/e395c4e2a6234498bbd98a33e7df5ca2
Autor:
M. Snels, A. Scoccione, L. Di Liberto, F. Colao, M. Pitts, L. Poole, T. Deshler, F. Cairo, C. Cagnazzo, F. Fierli
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 955-972 (2019)
A comparison of polar stratospheric cloud (PSC) occurrence from 2006 to 2010 is presented, as observed from the ground-based lidar station at McMurdo (Antarctica) and by the satellite-borne CALIOP lidar (Cloud-Aerosol Lidar with Orthogonal Polarizati
Externí odkaz:
https://doaj.org/article/241f3ffd8dce439ab4cfea96a3be55f8
Publikováno v:
Atmospheric Chemistry and Physics, Vol 18, Pp 4885-4896 (2018)
This paper illustrates measurements carried out by the Raman lidar BASIL in the frame of the HD(CP)2 Observational Prototype Experiment (HOPE), revealing the presence of a clear-air dark band phenomenon (i.e. a minimum in lidar backscatter echoes)
Externí odkaz:
https://doaj.org/article/9a517e25df0a467ab8922412c47ba3ce
Scattering codes are used to study the optical properties of Polar Stratospheric Clouds (PSC). Particle backscattering and depolarization coefficients can be computed with available scattering codes once the particle size distribution (PSD) is known
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2844d4bf8e56daaaf70a3ba5a7b81b7
https://doi.org/10.5194/egusphere-egu23-17448
https://doi.org/10.5194/egusphere-egu23-17448
Publikováno v:
Atmospheric Chemistry and Physics, Vol 17, Iss 1, Pp 745-767 (2017)
Measurements carried out by the University of Basilicata Raman lidar system (BASIL) are reported to demonstrate the capability of this instrument to characterise turbulent processes within the convective boundary layer (CBL). In order to resolve the
Externí odkaz:
https://doaj.org/article/634afb235dca4edba266b74623a094f4
Akademický článek
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Scattering codes are used to study the optical properties of polar stratospheric clouds (PSCs). Particle backscattering and depolarization coefficients can be computed with available scattering codes once the particle size distribution (PSD) is known
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4ed2d7835a90a5149b12572c27c42576
https://amt.copernicus.org/articles/16/419/2023/
https://amt.copernicus.org/articles/16/419/2023/
Publikováno v:
eISSN
Scattering codes are used to study the optical properties of polar stratospheric clouds (PSCs). Particle backscattering and depolarization coefficients can be computed with available scattering codes once the particle size distribution (PSD) is known
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3a39d6034e58555254490ef018ce0ab5
https://doi.org/10.5194/egusphere-2022-972
https://doi.org/10.5194/egusphere-2022-972
Autor:
F. Cairo, M. De Muro, M. Snels, L. Di Liberto, S. Bucci, B. Legras, A. Kottayil, A. Scoccione, S. Ghisu
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 7947-7961 (2021)
A polarization diversity elastic backscatter lidar was deployed on the equatorial island of Palau in February and March 2016 in the framework of the EU StratoClim project. The system operated unattended in the Palau Atmosferic Observatory from 15 Feb