Zobrazeno 1 - 5
of 5
pro vyhledávání: '"William C. Skillman"'
Autor:
William C. Skillman, R. A. Ferrare, S. H. Melfi, David N. Whiteman, Steven E. Koch, Paul B. Dorian
Publikováno v:
Monthly Weather Review. 119:857-887
Detailed moisture observations from a ground-based Raman lidar and special radiosonde data of two disturbances associated with a dissipating gust front are presented. A synthesis of the lidar data with conventional meteorological data, in conjunction
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be4200ba0c0563aa15b7fec44dc78648
https://doi.org/10.1175/1520-0493(1991)119<0857:soaiba>2.0.co
https://doi.org/10.1175/1520-0493(1991)119<0857:soaiba>2.0.co
Autor:
Raymond Wexler, William C. Skillman
Publikováno v:
Monthly Weather Review. 107:343-346
On August 23, 1978, a long cirrus plume, as detected by the GOES E satellite, made a sharp anticyclonic turn and traveled a total distance of 2800 km from the generating thunderstorm, as determined from satellite imagery. During a five-hour period th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a5a5c07a4bdb16c8fc5e56fe12c0e4c7
https://doi.org/10.1175/1520-0493(1979)107<0343:sdoalc>2.0.co
https://doi.org/10.1175/1520-0493(1979)107<0343:sdoalc>2.0.co
Autor:
Dennis A. Keyser, William C. Skillman, Steven E. Koch, Michael Mccumber, Paul J. Kocin, Peter J. Wetzel, Keith F. Brill
Publikováno v:
Monthly Weather Review. 113:1714-1737
The synoptic scale performance characteristics of MASS 2.0 are determined by comparing filtered 12-24 hr model forecasts to same-case forecasts made by the National Meteorological Center's synoptic-scale Limited-area Fine Mesh model. Characteristics
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::65194efbf741ab74f8077c35dbc53556
https://doi.org/10.1175/1520-0493(1985)113<1714:ssfsas>2.0.co
https://doi.org/10.1175/1520-0493(1985)113<1714:ssfsas>2.0.co
Conference
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Autor:
Roger Grimshaw
The dynamics of flows in density-stratified fluids has been and remains now an important topic for scientific enquiry. Such flows arise in many contexts, ranging from industrial settings to the oceanic and atmospheric environments. It is the latter t
