Applied physical sciences. Hypothetical explanations of the negative apparent effects of cloud seeding in the whitetop experiment / Lovasich, J. L.

Public ISBD Titre de série : Applied physical sciences Titre : Hypothetical explanations of the negative apparent effects of cloud seeding in the whitetop experiment Type de document : texte imprimé Auteurs : Lovasich, J. L. ; Neyman, J. ; Scott, E. L. Année de publication : nov. 1971 ISBN/ISSN/EAN : CI-05434 Note générale : In order to explain the apparent losses of rain ascribable to seeding at the whitetop trial, particularly large and highly significant in the stralum E (but not in the opposite stratum W) of experimental days, it has been hypothesized that seeding causes widespread cloudiness and subsequent lowering of ground temperatures. This hypothesis is flatly contradicted by the observations : the seeded E-days (but not W-days) were uniformly less cloudy and hotter than those without seeding. Curiously, theses differences prevailed not only from the scheduled time seeding but also for several hours beforehand. Langues : Anglais (eng) Mots-clés : PRECIPITATIONS  Météorologie  Climatologie  Randomization  Stratification Index. décimale : 551.6 Climatologie et temps Résumé : In order to explain the apparent losses of rain ascribable to seeding at the whitetop trial, particularly large and highly significant in the stralum E (but not in the opposite stratum W) of experimental days, it has been hypothesized that seeding causes widespread cloudiness and subsequent lowering of ground temperatures. This hypothesis is flatly contradicted by the observations : the seeded E-days (but not W-days) were uniformly less cloudy and hotter than those without seeding. Curiously, theses differences prevailed not only from the scheduled time seeding but also for several hours beforehand. Note de contenu : In order to explain the apparent losses of rain ascribable to seeding at the whitetop trial, particularly large and highly significant in the stralum E (but not in the opposite stratum W) of experimental days, it has been hypothesized that seeding causes widespread cloudiness and subsequent lowering of ground temperatures. This hypothesis is flatly contradicted by the observations : the seeded E-days (but not W-days) were uniformly less cloudy and hotter than those without seeding. Curiously, theses differences prevailed not only from the scheduled time seeding but also for several hours beforehand. Applied physical sciences. Hypothetical explanations of the negative apparent effects of cloud seeding in the whitetop experiment [texte imprimé] / Lovasich, J. L. ; Neyman, J. ; Scott, E. L. . - nov. 1971. ISSN : CI-05434 In order to explain the apparent losses of rain ascribable to seeding at the whitetop trial, particularly large and highly significant in the stralum E (but not in the opposite stratum W) of experimental days, it has been hypothesized that seeding causes widespread cloudiness and subsequent lowering of ground temperatures. This hypothesis is flatly contradicted by the observations : the seeded E-days (but not W-days) were uniformly less cloudy and hotter than those without seeding. Curiously, theses differences prevailed not only from the scheduled time seeding but also for several hours beforehand. Langues : Anglais (eng) Mots-clés : PRECIPITATIONS  Météorologie  Climatologie  Randomization  Stratification Index. décimale : 551.6 Climatologie et temps Résumé : In order to explain the apparent losses of rain ascribable to seeding at the whitetop trial, particularly large and highly significant in the stralum E (but not in the opposite stratum W) of experimental days, it has been hypothesized that seeding causes widespread cloudiness and subsequent lowering of ground temperatures. This hypothesis is flatly contradicted by the observations : the seeded E-days (but not W-days) were uniformly less cloudy and hotter than those without seeding. Curiously, theses differences prevailed not only from the scheduled time seeding but also for several hours beforehand. Note de contenu : In order to explain the apparent losses of rain ascribable to seeding at the whitetop trial, particularly large and highly significant in the stralum E (but not in the opposite stratum W) of experimental days, it has been hypothesized that seeding causes widespread cloudiness and subsequent lowering of ground temperatures. This hypothesis is flatly contradicted by the observations : the seeded E-days (but not W-days) were uniformly less cloudy and hotter than those without seeding. Curiously, theses differences prevailed not only from the scheduled time seeding but also for several hours beforehand.

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CI03B434.199387	CI-05434	Périodique	Bibliothèque CDI-Ouaga	Fond documentaire	Disponible
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