Chloride and Sulfate Particles in the Atmosphere

Autor: Horace R. Byers

Publikováno v: Atmospheric Chemistry of Chlorine and Sulfur Compounds: Proceedings of a Symposium Held at the Robert A. Taft Sanitary Engineering Center, Cincinnati, Ohio, November 4–6, 1957

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c92a43a7d1075c875aee8343a0d05f9a
https://doi.org/10.1029/gm003p0104

Spearhead Echo and Downburst in the Crash of an Airliner

Autor: Horace R. Byers, Tetsuya Theodore. Fujita

Publikováno v: Monthly Weather Review. 105:129-146

Meteorological conditions leading to the crash of an airliner short of the runway of a New York airport were studied. Thunderstorm downdrafts much stronger than those measured on the 1946-47 Thunderstorm Project were found. These exceptional downdraf

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::968ce8b3e82ac3cf0fe62139e4c6d213
https://doi.org/10.1175/1520-0493(1977)105<0129:seadit>2.0.co

Probing the Thunderstorm

Autor: Horace R. Byers

Publikováno v: Weatherwise. 1:47-50

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::cc3ea8128c55a0dd6471e06aabe125cf
https://doi.org/10.1080/00431672.1948.9925140

Some Effects of Vertical Wind Shear on Thunderstorm Structure *

Autor: Louis J. Battan, Horace R. Byers

Publikováno v: Bulletin of the American Meteorological Society. 30:168-175

Observations of thunderclouds obtained with a 3-cm height-finding radar set are used to obtain a description of the vertical shear of thunderclouds. Several photographs are given which show the shearing of the radar clouds. A scattergram of wind shea

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::2bd80de72ebb336860bd33837a6b849a
https://doi.org/10.1175/1520-0477-30.5.168

Geographical differences in cloud populations

Autor: Horace R. Byers

Publikováno v: Archiv für Meteorologie, Geophysik und Bioklimatologie Serie A. 8:180-184

Cumulus clouds have been studied by radar and special flight observations with particular reference to the temperatures at which rain is initiated. In the Caribbean area rain starts while the clouds have temperatures greater than +5°C at their tops,

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5fab25ffb6c77fc611a8d492168983b9
https://doi.org/10.1007/bf02247278